Paleobiota of the Niobrara Formation: Difference between revisions
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[[File:Pachyrhizodus caninus skeletons.JPG|thumb|''[[Pachyrhizodus caninus]]'' skeletons (casts)]] |
[[File:Pachyrhizodus caninus skeletons.JPG|thumb|''[[Pachyrhizodus caninus]]'' skeletons (casts)]] |
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[[File:Pseudoperna congesta fossil osyters encrusting a Platyceramus platinus shell.jpg|thumb|[[Pseudoperna congesta]] fossil |
[[File:Pseudoperna congesta fossil osyters encrusting a Platyceramus platinus shell.jpg|thumb|[[Pseudoperna congesta]] fossil oysters encrusting a large [[Platyceramus platinus]] bivalve shell, Smoky Hill Chalk member of [[Niobrara Formation]] . Photo in place at Castle Rock chalk badlands, Kansas.]] |
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During the time of the deposition of the [[Niobrara Formation|Niobrara Chalk]], much life inhabited the seas of the [[Western Interior Seaway]]. By this time in the [[Late Cretaceous]] many new lifeforms appeared such as [[mosasaur]]s, which were to be some of the last of the aquatic lifeforms to evolve before the end of the [[Mesozoic]]. Life of the Niobrara Chalk is comparable to that of the [[Dakota Formation]], although the Dakota Formation, which was deposited during the [[Cenomanian]], predates the chalk by about 10 million years. |
During the time of the deposition of the [[Niobrara Formation|Niobrara Chalk]], much life inhabited the seas of the [[Western Interior Seaway]]. By this time in the [[Late Cretaceous]] many new lifeforms appeared such as [[mosasaur]]s, which were to be some of the last of the aquatic lifeforms to evolve before the end of the [[Mesozoic]]. Life of the Niobrara Chalk is comparable to that of the [[Dakota Formation]], although the Dakota Formation, which was deposited during the [[Cenomanian]], predates the chalk by about 10 million years. |
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==Bony fish== |
==Bony fish== |
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=== |
===Pycnodontiformes=== |
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{| class="wikitable" style="margin:auto;" |
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|- |
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! Genus |
! Genus |
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! Notes |
! Notes |
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|- |
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| ''[[Micropycnodon]]''<ref name="everhart-table-fish" /> |
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| |
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'' |
| ''M. kansasensis''<ref name="everhart-table-fish" /> |
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| |
| Smoky Hill Chalk<ref name="everhart-table-fish" /> |
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| {{nowrap|Smoky Hill Chalk}}<ref name="everhart-table-fish" /> |
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| |
| |
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| A [[Pycnodontiformes|pycnodontiform]] fish similar but unrelated to modern [[parrotfish]] |
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| A [[Lepisosteidae|lepisosteid]] gar |
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|- |
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| ''[[Paraliodesmus]]''<ref name="everhart-table-fish-245">"Table 13.1: Bony Fish", Everhart (2005), page 245.</ref> |
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| ''P. guadagnii''<ref name="everhart-table-fish-245" /> |
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| Smoky Hill Chalk<ref name="everhart-table-fish-245" /> |
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| |
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| Amiiformes |
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|- |
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| ''[[Urenchelys]]''<ref name="everhart-table-fish-245" /> |
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| ''U. abditus''<ref name="everhart-table-fish-245" /> |
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| Smoky Hill Chalk<ref name="everhart-table-fish-245" /> |
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| |
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| Anguilliformes |
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|- |
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|''[[Ferrifrons]]'' |
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| ''F. rugosus'' |
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| |
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| A [[Ferrifronsidae|ferrifronsid]] [[Acanthomorpha|acanthomorph]] |
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|- |
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|''[[Aethocephalichthys]]''<ref name="everhart-table-fish-245" /> |
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| ''A. hyainarhinos''<ref name="everhart-table-fish-245" /> |
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| Smoky Hill Chalk<ref name="everhart-table-fish-245" /> |
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| |
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| An [[Actinopterygii|actinopterygian]] of indeterminate classification<ref>Fielitz, C.; Stewart, J. D.; & Wiffen, J. 1999. Aethocephalichthys hyainarhinos gen. et sp. nov., a new and enigmatic Late Cretaceous actinopterygian from North America and New Zealand. ''Mesozoic Fishes'' 2 – Systematics and Fossil Record, G. Arratia & H.-P. Schultze (eds.): pp. 95-106, 7 figs.</ref> |
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|- |
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|''[[Omosoma]]'' |
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| ''O. garretti'' |
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| |
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| A [[Beardfish|polymixiid]] [[actinopterygii]]an closely related to the modern [[Beardfish]] |
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|- |
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|''[[Belonostomus]]''<ref name="everhart-table-fish">"Table 13.1: Bony Fish", Everhart (2005), page 244.</ref> |
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| Indeterminate<ref name="everhart-table-fish" /> |
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| Aspidorhynchiformes |
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|} |
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=== |
===Semionotiformes=== |
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{| class="wikitable" style="margin:auto;" |
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|- |
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! Genus |
! Genus |
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=== |
===Pachycormiformes=== |
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{| class="wikitable" style="margin:auto;" |
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|- |
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! Genus |
! Genus |
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! Abundance |
! Abundance |
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! Notes |
! Notes |
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! Images |
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|- |
|- |
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| ''[[ |
| rowspan=5 | ''[[Protosphyraena]]''<ref name="everhart-table-fish" /> |
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| {{nowrap|''P. bentonianum''}} |
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| ''M. kansasensis''<ref name="everhart-table-fish" /> |
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| |
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| |
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| rowspan=4 | A [[swordfish]]-like [[pachycormid]] |
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| rowspan=34 | [[File:Protosphyraena_perniciosa.png|thumb|center|150px|''[[Protosphyraena|Protosphyraena perniciosa]]'']] |
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[[File:Bonnerichthys_gladius.png|thumb|center|150px|''[[Bonnerichthys|Bonnerichthys gladius]]'']] |
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|- |
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| ''P. nitida''<ref name="everhart-table-fish" /> |
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| {{nowrap|Smoky Hill Chalk}}<ref name="everhart-table-fish" /> |
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| |
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|- |
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| ''P. perniciosa''<ref name="everhart-table-fish" /> |
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| Smoky Hill Chalk<ref name="everhart-table-fish" /> |
| Smoky Hill Chalk<ref name="everhart-table-fish" /> |
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| |
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|- |
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| ''P. tenuis''<ref name="everhart-table-fish" /> |
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| Smoky Hill Chalk<ref name="everhart-table-fish" /> |
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| |
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|- style="background:#E6E6E6;" |
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|| ''P. gladius''<ref name="everhart-table-fish" /> |
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|| Smoky Hill Chalk<ref name="everhart-table-fish" /> |
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| style="background:#E6E6E6;"| |
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|| Named as a new genus, [[Bonnerichthys]] |
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|- |
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| ''[[Bonnerichthys]]''<ref>Viegas, Jennifer (18 February 2010), SUV-Sized Fish Were Earliest Filter-Feeders, Discovery News, retrieved 1 April 2010</ref> |
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| ''B. gladius'' |
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| Smoky Hill Chalk<ref name="everhart-table-fish-245" /> |
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| |
| |
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| A filter feeding pachycormid |
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| A [[Pycnodontiformes|pycnodontiform]] fish similar but unrelated to modern [[parrotfish]] |
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|} |
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=== |
===Crossognathiformes=== |
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! Genus |
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! Abundance |
! Abundance |
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! Notes |
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! Images |
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|- |
|- |
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| ''[[Apsopelix]]''<ref name="everhart-table-fish-245" /> |
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| ''[[Bananogmius]]'' |
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| ''A. anglicus''<ref name="everhart-table-fish-245" /> |
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| ''B. evolutus'' |
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| Smoky Hill Chalk<ref name="everhart-table-fish-245" /> |
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| |
| |
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| A [[Crossognathidae|crossognathid]]. |
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| rowspan=4 |[[File:Pachyrhizodus.png|thumb|center|150px|''[[Pachyrhizodus|Pachyrhizodus sp.]]'']] |
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|- |
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| rowspan=3 | ''[[Pachyrhizodus]]''<ref name="everhart-table-fish-245" /> |
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| ''P. caninus''<ref name="everhart-table-fish-245" /> |
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| Smoky Hill Chalk<ref name="everhart-table-fish-245" /> |
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| |
| |
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| rowspan=3 | A [[Pachyrhizodontidae|pachyrhizodontid]] |
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| A [[Bananogmiidae|bananogmiid]] [[Albuliformes|albuliform]] [[Elopiformes|elopiform]] |
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|- |
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| ''P. leptopsis''<ref name="everhart-table-fish-245" /> |
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| Smoky Hill Chalk<ref name="everhart-table-fish-245" /> |
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| |
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|- |
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| ''P. minimus''<ref name="everhart-table-fish-245" /> |
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| Smoky Hill Chalk<ref name="everhart-table-fish-245" /> |
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| |
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|- |
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|} |
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===Ichthyodectiformes=== |
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{| class="wikitable" style="margin:auto; width:100%;" |
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|- |
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! Genus |
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! Species |
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! Member |
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! Abundance |
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! Notes |
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! Images |
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|- |
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| ''[[Xiphactinus]]''<ref name="everhart-table-fish-245" /> |
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| ''X. audax''<ref name="everhart-table-fish-245" /> |
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| Smoky Hill Chalk<ref name="everhart-table-fish-245" /> |
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| |
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| A large [[Ichthyodectidae|ichthyodectid]] |
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| rowspan=34 | [[File:Xiphactinus_audax.png|thumb|center|150px|''[[Xiphactinus audax]]'']] |
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[[Image:Ichthyodectes ctenodon.jpg|thumb|center|150px|''[[Ichthyodectes ctenodon]]'']] |
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[[Image:Gillicus arcuatus.JPG|thumb|center|150px|''[[Gillicus arcuatus]]'']] |
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[[File:Saurodon_leanus.png|thumb|center|150px|''[[Saurodon leanus]]'']] |
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|- |
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| ''[[Ichthyodectes]]''<ref name="everhart-table-fish-245" /> |
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| ''I. ctenodon''<ref name="everhart-table-fish-245" /> |
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| Smoky Hill Chalk<ref name="everhart-table-fish-245" /> |
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| |
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| An ichthyodectid |
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|- |
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| ''[[Gillicus]]''<ref name="everhart-table-fish-245" /> |
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| ''G. arcuantus''<ref name="everhart-table-fish-245" /> |
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| Smoky Hill Chalk<ref name="everhart-table-fish-245" /> |
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| |
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| A [[saurodontid]] |
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|- |
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| ''[[Saurodon]]''<ref name="everhart-table-fish-245" /> |
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| ''S. leanus''<ref name="everhart-table-fish-245" /> |
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| Smoky Hill Chalk<ref name="everhart-table-fish-245" /> |
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| |
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| A saurodontid |
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|- |
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| ''[[Saurocephalus]]''<ref name="everhart-table-fish-245" /> |
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| ''S. lanciformis''<ref name="everhart-table-fish-245" /> |
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| Smoky Hill Chalk<ref name="everhart-table-fish-245" /> |
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| |
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| A saurodontid |
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|} |
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===Tselfatiiformes=== |
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{| class="wikitable" style="margin:auto; width:100%;" |
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|- |
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! Genus |
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! Species |
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! Member |
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! Abundance |
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! Notes |
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! Images |
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|- |
|- |
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| ''[[Thryptodus]]''<ref name="everhart-table-fish-245" /> |
| ''[[Thryptodus]]''<ref name="everhart-table-fish-245" /> |
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| Smoky Hill Chalk<ref name="everhart-table-fish-245" /> |
| Smoky Hill Chalk<ref name="everhart-table-fish-245" /> |
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| |
| |
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| A [[ |
| A [[Plethodidae|plethodid]] |
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| rowspan=6 | [[File:Pentanogmius_evolutus.png|thumb|center|150px|''[[Pentanogmius|Pentanogmius evolutus]]'']] |
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|- |
|- |
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| ''[[Pentanogmius]]''<ref name="everhart-table-fish-245" /> |
| ''[[Pentanogmius]]''<ref name="everhart-table-fish-245" /> |
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| Smoky Hill Chalk<ref name="everhart-table-fish-245" /> |
| Smoky Hill Chalk<ref name="everhart-table-fish-245" /> |
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| |
| |
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| A plethodid |
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| A [[Tselfatiiformes|tselfatiiform]] |
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|- |
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|- |
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| rowspan=2 | ''[[Martinichthys]]''<ref name="everhart-table-fish-245" /> |
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| ''M. brevis''<ref name="everhart-table-fish-245" /> |
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| Smoky Hill Chalk<ref name="everhart-table-fish-245" /> |
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| |
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| rowspan=2 | A plethodid |
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|- |
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| ''M. xiphoides''<ref name="everhart-table-fish-245" /> |
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| Smoky Hill Chalk<ref name="everhart-table-fish-245" /> |
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| |
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|- |
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| ''[[Niobrara (fish)|Niobrara]]''<ref name="everhart-table-fish-245" /> |
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| ''N. encarsia''<ref name="everhart-table-fish-245" /> |
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| Smoky Hill Chalk<ref name="everhart-table-fish-245" /> |
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| |
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| A plethodid |
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|- |
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| ''[[Zanclites]]''<ref name="everhart-table-fish-245" /> |
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| ''Z. xenurus''<ref name="everhart-table-fish-245" /> |
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| Smoky Hill Chalk<ref name="everhart-table-fish-245" /> |
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| |
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| A plethodid |
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|- |
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|} |
|} |
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=== |
===Aulopiformes=== |
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{| class="wikitable" style="margin:auto;" |
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|- |
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! Genus |
! Genus |
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! Abundance |
! Abundance |
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! Notes |
! Notes |
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! Images |
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|- |
|- |
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| ''[[Cimolichthys]]''<ref name="everhart-table-fish-245" /> |
| ''[[Cimolichthys]]''<ref name="everhart-table-fish-245" /> |
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| Smoky Hill Chalk<ref name="everhart-table-fish-245" /> |
| Smoky Hill Chalk<ref name="everhart-table-fish-245" /> |
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| |
| |
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| A [[Cimolichthyidae|cimolichthyid]] |
| A [[Cimolichthyidae|cimolichthyid]] |
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| rowspan=8 | [[File:Cimolichthys_nepaholica.png|thumb|center|150px|''[[Cimolichthys|Cimolichthys nepaholica]]'']] |
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[[File:Enchodus_petrosus.png|thumb|center|150px|''[[Enchodus|Enchodus petrosus]]'']] |
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|- |
|- |
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| rowspan=4 | |
| rowspan=4 | |
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| Smoky Hill Chalk<ref name="everhart-table-fish-245" /> |
| Smoky Hill Chalk<ref name="everhart-table-fish-245" /> |
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| |
| |
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| rowspan=4 | An [[Enchodontidae|enchodontid]] |
| rowspan=4 | An [[Enchodontidae|enchodontid]] |
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|- |
|- |
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| ''E. gladiolus''<ref name="everhart-table-fish-245" /> |
| ''E. gladiolus''<ref name="everhart-table-fish-245" /> |
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| Smoky Hill Chalk<ref name="everhart-table-fish-245" /> |
| Smoky Hill Chalk<ref name="everhart-table-fish-245" /> |
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|} |
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===Alepisauriforms=== |
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{| class="wikitable" style="margin:auto;" |
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|- |
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! Genus |
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! Species |
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! Member |
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! Abundance |
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! Notes |
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|- |
|- |
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| ''[[Apateodus]]''<ref name="everhart-table-fish-245" /> |
| ''[[Apateodus]]''<ref name="everhart-table-fish-245" /> |
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=== |
===Beryciformes=== |
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{| class="wikitable" style="margin:auto;" |
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|- |
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! Genus |
! Genus |
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=== |
===Other bony fish=== |
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{| class="wikitable" style="margin:auto;" |
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|- |
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! Genus |
! Genus |
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! Abundance |
! Abundance |
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! Notes |
! Notes |
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! Images |
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|- |
|- |
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| |
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| rowspan=5 | ''[[Protosphyraena]]''<ref name="everhart-table-fish" /> |
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''[[Lepisosteus]]''<ref name="everhart-table-fish" /> |
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| {{nowrap|''P. bentonianum''}} |
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| Indeterminate<ref name="everhart-table-fish" /> |
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| |
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| |
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| rowspan=4 | A primitive [[swordfish]] about 3m in length. |
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| rowspan=34 | [[Image:Protosphyraena2DB.jpg|thumb|center|150px|''[[Protosphyraena| Protosphyraena perniciosa]]'']] |
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[[Image:XiphactinusDB.jpg|thumb|center|150px|''[[Xiphactinus|Xiphactinus audax]]'']] |
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[[Image:Ichthyodectes ctenodon.jpg|thumb|center|150px|''[[Ichthyodectes|Ichthyodectes ctenodon]]'']] |
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[[Image:Gillicus arcuatus.JPG|thumb|center|150px|''[[Gillicus|Gillicus arcuatus]]'']] |
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[[Image:Saurodon BW.jpg|thumb|center|150px|''[[Saurodon|Saurodon leanus]]'']] |
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|- |
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| ''P. nitida''<ref name="everhart-table-fish" /> |
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| {{nowrap|Smoky Hill Chalk}}<ref name="everhart-table-fish" /> |
| {{nowrap|Smoky Hill Chalk}}<ref name="everhart-table-fish" /> |
||
| |
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|- |
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| ''P. perniciosa''<ref name="everhart-table-fish" /> |
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| Smoky Hill Chalk<ref name="everhart-table-fish" /> |
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| |
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|- |
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| ''P. tenuis''<ref name="everhart-table-fish" /> |
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| Smoky Hill Chalk<ref name="everhart-table-fish" /> |
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| |
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|- style="background:#E6E6E6;" |
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|| ''P. gladius''<ref name="everhart-table-fish" /> |
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|| Smoky Hill Chalk<ref name="everhart-table-fish" /> |
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| style="background:#E6E6E6;"| |
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|| A misidentified pachycormid |
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|- |
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| ''[[Xiphactinus]]''<ref name="everhart-table-fish-245" /> |
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| ''X. audax''<ref name="everhart-table-fish-245" /> |
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| Smoky Hill Chalk<ref name="everhart-table-fish-245" /> |
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| |
| |
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| A [[Lepisosteidae|lepisosteid]] gar |
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| A large [[Ichthyodectidae|ichthyodectid]] [[Pachycormiformes|pachycormiform]] about 5m in length |
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|- |
|- |
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| ''[[ |
| ''[[Paraliodesmus]]''<ref name="everhart-table-fish-245">"Table 13.1: Bony Fish", Everhart (2005), page 245.</ref> |
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| '' |
| ''P. guadagnii''<ref name="everhart-table-fish-245" /> |
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| Smoky Hill Chalk<ref name="everhart-table-fish-245" /> |
| Smoky Hill Chalk<ref name="everhart-table-fish-245" /> |
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| |
| |
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| An [[amiiform]] |
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| An [[Ichthyodectidae|ichthyodectid]] [[Pachycormiformes|pachycormiform]] about 2m in length |
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|- |
|- |
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| ''[[ |
| ''[[Urenchelys]]''<ref name="everhart-table-fish-245" /> |
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| '' |
| ''U. abditus''<ref name="everhart-table-fish-245" /> |
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| Smoky Hill Chalk<ref name="everhart-table-fish-245" /> |
| Smoky Hill Chalk<ref name="everhart-table-fish-245" /> |
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| |
| |
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| An [[anguilliform]] |
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| An [[Ichthyodectidae|ichthyodectid]] [[Pachycormiformes|pachycormiform]] about 2m in length |
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|- |
|- |
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|''[[Ferrifrons]]'' |
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| ''[[Saurodon]]''<ref name="everhart-table-fish-245" /> |
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| ''F. rugosus'' |
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| ''S. leanus''<ref name="everhart-table-fish-245" /> |
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| Smoky Hill Chalk<ref name="everhart-table-fish-245" /> |
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| |
| |
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| A [[Saurodontinae|saurodontine]] [[Ichthyodectidae|ichthyodectid]] [[Pachycormiformes|pachycormiform]] |
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|- |
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| ''[[Saurocephalus]]''<ref name="everhart-table-fish-245" /> |
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| ''S. lanciformis''<ref name="everhart-table-fish-245" /> |
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| Smoky Hill Chalk<ref name="everhart-table-fish-245" /> |
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| |
| |
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| A [[Ferrifronsidae|ferrifronsid]] [[Acanthomorpha|acanthomorph]] |
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| A [[Saurodontinae|saurodontine]] [[Ichthyodectidae|ichthyodectid]] [[Pachycormiformes|pachycormiform]] |
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|- |
|- |
||
|''[[Aethocephalichthys]]''<ref name="everhart-table-fish-245" /> |
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| ''[[Bonnerichthys]]''<ref> Viegas, Jennifer (18 February 2010), SUV-Sized Fish Were Earliest Filter-Feeders, Discovery News, retrieved 1 April 2010</ref> |
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| ''A. hyainarhinos''<ref name="everhart-table-fish-245" /> |
|||
| ''B. gladius'' |
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| Smoky Hill Chalk<ref name="everhart-table-fish-245" /> |
| Smoky Hill Chalk<ref name="everhart-table-fish-245" /> |
||
| |
| |
||
| An [[Actinopterygii|actinopterygian]] of indeterminate classification<ref>Fielitz, C.; Stewart, J. D.; & Wiffen, J. 1999. Aethocephalichthys hyainarhinos gen. et sp. nov., a new and enigmatic Late Cretaceous actinopterygian from North America and New Zealand. ''Mesozoic Fishes'' 2 – Systematics and Fossil Record, G. Arratia & H.-P. Schultze (eds.): pp. 95-106, 7 figs.</ref> |
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| A 9 meter long filter feeding [[Pachycormiformes|pachycormiform]] |
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|} |
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===Crossognathiforms=== |
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|- |
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! Genus |
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! Species |
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! Member |
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! Abundance |
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! Notes |
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! Images |
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|- |
|- |
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|''[[Omosoma]]'' |
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| ''[[Apsopelix]]''<ref name="everhart-table-fish-245" /> |
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| ''O. garretti'' |
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| ''A. anglicus''<ref name="everhart-table-fish-245" /> |
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| Smoky Hill Chalk<ref name="everhart-table-fish-245" /> |
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| |
| |
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| A [[Crossognathiformes|crossognathiform]] about 12 cm in length |
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|- |
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| ''[[Martinichthys]]''<ref name="everhart-table-fish-245" /> |
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| ''M. brevis''<ref name="everhart-table-fish-245" /> |
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| Smoky Hill Chalk<ref name="everhart-table-fish-245" /> |
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| |
| |
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| A [[Beardfish|polymixiid]] [[actinopterygii]]an closely related to the modern [[Beardfish]] |
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| A [[Crossognathiformes|crossognathiform]] |
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|- |
|- |
||
| |
|''[[Belonostomus]]''<ref name="everhart-table-fish">"Table 13.1: Bony Fish", Everhart (2005), page 244.</ref> |
||
| |
| Indeterminate<ref name="everhart-table-fish" /> |
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| Smoky Hill Chalk<ref name="everhart-table-fish-245" /> |
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| |
| |
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| A [[Crossognathiformes|crossognathiform]] |
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|- |
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| ''[[Zanclites]]''<ref name="everhart-table-fish-245" /> |
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| ''Z. xenurus''<ref name="everhart-table-fish-245" /> |
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| Smoky Hill Chalk<ref name="everhart-table-fish-245" /> |
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| |
| |
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| An [[aspidorhynchid]] |
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| A [[Crossognathiformes|crossognathiform]] |
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|- |
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| rowspan=3 | ''[[Pachyrhizodus]]''<ref name="everhart-table-fish-245" /> |
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| ''P. caninus''<ref name="everhart-table-fish-245" /> |
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| Smoky Hill Chalk<ref name="everhart-table-fish-245" /> |
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| |
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| rowspan=3 | A [[Crossognathiformes|crossognathiform]] |
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|- |
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| ''P. leptopsis''<ref name="everhart-table-fish-245" /> |
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| Smoky Hill Chalk<ref name="everhart-table-fish-245" /> |
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| |
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|- |
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| ''P. minimus''<ref name="everhart-table-fish-245" /> |
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| Smoky Hill Chalk<ref name="everhart-table-fish-245" /> |
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===Sharks=== |
===Sharks=== |
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! Genus |
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| Smoky Hill Chalk<ref name="everhart-table-sharks" /> |
| Smoky Hill Chalk<ref name="everhart-table-sharks" /> |
||
| |
| |
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| A large [[Lamniformes|lamniform]] shark |
| A large [[Lamniformes|lamniform]] shark |
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| |
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|- |
|- |
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| Smoky Hill Chalk<ref name="everhart-table-cretalamna" /> |
| Smoky Hill Chalk<ref name="everhart-table-cretalamna" /> |
||
| |
| |
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| A [[lamniform]] shark |
| A [[lamniform]] shark |
||
| |
| |
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[[Image:MenuhaCretalamnaAppendiculata.jpg|thumb|center|150px|''Cretalamna appendiculata'' tooth from Israel]] |
[[Image:MenuhaCretalamnaAppendiculata.jpg|thumb|center|150px|''Cretalamna appendiculata'' tooth from Israel]] |
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| Smoky Hill Chalk<ref name="everhart-table-sharks" /> |
| Smoky Hill Chalk<ref name="everhart-table-sharks" /> |
||
| |
| |
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| rowspan=3 | A [[Lamniformes|lamniform]] |
| rowspan=3 | A [[Lamniformes|lamniform]] |
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|[[Image:MenuhaSqualicoraxPristodontus.jpg|thumb|center|150px|''Squalicorax falcatus'' tooth from Israel]] |
|[[Image:MenuhaSqualicoraxPristodontus.jpg|thumb|center|150px|''Squalicorax falcatus'' tooth from Israel]] |
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|- |
|- |
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| Smoky Hill Chalk<ref name="everhart-table-sharks" /> |
| Smoky Hill Chalk<ref name="everhart-table-sharks" /> |
||
| |
| |
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| rowspan=5 | A [[Ptychodontidae|ptychodontid]] [[ |
| rowspan=5 | A [[Ptychodontidae|ptychodontid]] [[Lamniformes|lamniform]] shark |
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| |
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===Other cartilaginous fish=== |
===Other cartilaginous fish=== |
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|- |
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! Genus |
! Genus |
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[[Image:Kansas sea2DB.jpg|right|thumb|An artist's restoration of a dinosaur carcass that has been carried out to sea and some scavenging ''Squalicorax'' sharks.]] Nonavian dinosaurs have been found in the Niobrara Chalk despite it being located hundreds of miles out to sea at the time. The most reasonable theory is that the carcasses drifted out to sea. It is unlikely that the bodies were carried out by outgoing tides along the shorelines where they died, but rather it is more probable that the dinosaurs were carried offshore by floodwaters during a storm. In the shallow waters the bodies would have begun to [[Decomposition|decompose]] and bacteria within the carcass would have produced gasses that would have accumulated in the gut, thereby making the body [[Buoyancy|buoyant]]. Next, the prevailing winds and currents would have carried it out to sea, where it would eventually settle to the bottom and be buried in sediment.<ref>{{cite web|url=http://www.oceansofkansas.com/Dinosaur.html |title=Niobrarasaurus |publisher=Oceansofkansas.com |date= |accessdate=2016-04-13}}</ref> |
[[Image:Kansas sea2DB.jpg|right|thumb|An artist's restoration of a dinosaur carcass that has been carried out to sea and some scavenging ''Squalicorax'' sharks.]] Nonavian dinosaurs have been found in the Niobrara Chalk despite it being located hundreds of miles out to sea at the time. The most reasonable theory is that the carcasses drifted out to sea. It is unlikely that the bodies were carried out by outgoing tides along the shorelines where they died, but rather it is more probable that the dinosaurs were carried offshore by floodwaters during a storm. In the shallow waters the bodies would have begun to [[Decomposition|decompose]] and bacteria within the carcass would have produced gasses that would have accumulated in the gut, thereby making the body [[Buoyancy|buoyant]]. Next, the prevailing winds and currents would have carried it out to sea, where it would eventually settle to the bottom and be buried in sediment.<ref>{{cite web|url=http://www.oceansofkansas.com/Dinosaur.html |title=Niobrarasaurus |publisher=Oceansofkansas.com |date= |accessdate=2016-04-13}}</ref> |
||
A few [[caudal vertebrae]] from a [[Hadrosaurid|hadrosaur]] have been found with bite marks and have been eroded, suggesting at one point they were digested. A single tooth belonging to ''[[Squalicorax]]'' was found [[in situ]] under the vertebrae. This suggested the shark consumed the [[Posterior (anatomy)|posterior]] end of the tail of a floating hadrosaur carcass and had partially digested it before fossilization.<ref>{{cite web|url=http://www.oceansofkansas.com/New-dino.html |title=Shark bit dino |publisher=Oceansofkansas.com |date= |accessdate=2016-04-13}}</ref><ref>Everhart, M. J. and K. Ewell. 2006. Shark-bitten dinosaur (Hadrosauridae) vertebrae from the Niobrara Chalk (Upper Coniacian) of western Kansas. Kansas Academy of Science, Transactions, 109 (1-2):27-35.</ref> Most dinosaurs in the chalk were [[Nodosauridae|nodosaurs]]. |
A few [[caudal vertebrae]] from a [[Hadrosaurid|hadrosaur]] have been found with bite marks and have been eroded, suggesting at one point they were digested. A single tooth belonging to ''[[Squalicorax]]'' was found [[in situ]] under the vertebrae. This suggested the shark consumed the [[Posterior (anatomy)|posterior]] end of the tail of a floating hadrosaur carcass and had partially digested it before fossilization.<ref>{{cite web|url=http://www.oceansofkansas.com/New-dino.html |title=Shark bit dino |publisher=Oceansofkansas.com |date= |accessdate=2016-04-13}}</ref><ref>Everhart, M. J. and K. Ewell. 2006. Shark-bitten dinosaur (Hadrosauridae) vertebrae from the Niobrara Chalk (Upper Coniacian) of western Kansas. Kansas Academy of Science, Transactions, 109 (1-2):27-35.</ref> Most dinosaurs in the chalk were [[Nodosauridae|nodosaurs]]. The dinosaurs found here were endemic to [[Appalachia (landmass)|Appalachia]].<ref>{{cite journal |last1=Brownstein |first1=Chase D. |title=The biogeography and ecology of the Cretaceous non-avian dinosaurs of Appalachia |journal=Palaeontologia Electronica |date=February 2018 |volume=21 |issue=1.5A |pages=1–56 |doi=10.26879/801 |url=https://palaeo-electronica.org/content/2018/2123-appalachia-biogeography |access-date=21 March 2021|doi-access=free }}</ref> |
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===Non-avian=== |
===Non-avian=== |
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"Single articulated postcranial skeleton with associated skull fragments."<ref name="table-20-1-439">"Table 20.1," in Weishampel, et al. (2004). Page 439.</ref> |
"Single articulated postcranial skeleton with associated skull fragments."<ref name="table-20-1-439">"Table 20.1," in Weishampel, et al. (2004). Page 439.</ref> |
||
| A small [[hadrosaurid]] |
| A small [[hadrosaurid]] |
||
| rowspan="99" | [[Image:Claosaurus yale.JPG|thumb|center|200px|''[[Claosaurus|Claosaurus agilis]]'']] |
| rowspan="99" | [[Image:Claosaurus yale.JPG|thumb|center|200px|''[[Claosaurus|Claosaurus agilis]]'']] |
||
|- |
|- |
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| Indeterminate [[hadrosaurid]]<ref name="Everhart 27–35">{{Cite journal|last1=Everhart|first1=Michael J.|last2=Ewell|first2=Keith|date=April 2006|title=Shark-bitten dinosaur (Hadrosauridae) caudal vertebrae from the Niobrara Chalk (Upper Coniacian) of western Kansas|url=http://dx.doi.org/10.1660/0022-8443(2006)109[27:sdhcvf]2.0.co;2|journal=Transactions of the Kansas Academy of Science|volume=109|issue=1 & 2|pages=27–35|doi=10.1660/0022-8443(2006)109[27:sdhcvf]2.0.co;2|s2cid=86366930 |issn=0022-8443}}</ref> |
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| Indeterminate [[hadrosaurid]] |
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| |
| |
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| |
| |
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| |
| |
||
| |
| |
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| A [[hadrosaurid]] of indeterminate classification |
| A [[hadrosaurid]] of indeterminate classification. Possibly ''[[Corythosaurus]].''<ref name="Everhart 27–35"/> |
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|- |
|- |
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| |
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Three genre of birds are present in the formation, although rare. They were unrelated to modern birds, as they still retained teeth. ''[[Baptornis]]'' and ''[[Hesperornis]]'' were large flightless aquatic birds suited for diving. ''[[Ichthyornis]]'' was a seabird that resembled the [[gull]]s and [[petrel]]s of today. Both probably preyed on small fish and were preyed upon by sharks, large bony fish such as ''[[Xiphactinus]]'', and mosasaurs. |
Three genre of birds are present in the formation, although rare. They were unrelated to modern birds, as they still retained teeth. ''[[Baptornis]]'' and ''[[Hesperornis]]'' were large flightless aquatic birds suited for diving. ''[[Ichthyornis]]'' was a seabird that resembled the [[gull]]s and [[petrel]]s of today. Both probably preyed on small fish and were preyed upon by sharks, large bony fish such as ''[[Xiphactinus]]'', and mosasaurs. |
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{| class="wikitable" style="margin:auto;" |
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| rowspan="99" | [[Image:Hesperornis BW.jpg|thumb|center|150px|''[[Hesperornis|Hesperornis regalis]]'']] |
| rowspan="99" | [[Image:Hesperornis BW.jpg|thumb|center|150px|''[[Hesperornis|Hesperornis regalis]]'']] |
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[[Image:Ichthyornis |
[[Image:Ichthyornis restoration.jpeg|thumb|center|150px|''[[Ichthyornis|Ichthyornis dispar]]'']] |
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|- |
|- |
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| ''[[Baptornis]]''<ref name="everhart-table-birds" /> |
| ''[[Baptornis]]''<ref name="everhart-table-birds" /> |
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Line 569: | Line 576: | ||
| [[Smoky Hill Chalk]]<ref name="everhart-table-birds" /> |
| [[Smoky Hill Chalk]]<ref name="everhart-table-birds" /> |
||
|"Fragmentary skull [and] nearly complete postcranium."<ref name="table-11-1-215">"Table 11.1," in Weishampel, et al. (2004). Page 215.</ref> |
|"Fragmentary skull [and] nearly complete postcranium."<ref name="table-11-1-215">"Table 11.1," in Weishampel, et al. (2004). Page 215.</ref> |
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| A [[Baptornithidae|baptornithid]] [[Hesperornithiformes|hesperornithiform]] |
| A [[Baptornithidae|baptornithid]] [[Hesperornithiformes|hesperornithiform]] |
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|- |
|- |
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| ''[[Guildavis]]''<ref name="everhart-table-birds" /> |
| ''[[Guildavis]]''<ref name="everhart-table-birds" /> |
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Line 597: | Line 604: | ||
| [[Smoky Hill Chalk]]<ref name="everhart-table-birds" /> |
| [[Smoky Hill Chalk]]<ref name="everhart-table-birds" /> |
||
| |
| |
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| A large [[Hesperornithidae|hesperornithid]] [[Hesperornithiformes|hesperornithiform]] |
| A large [[Hesperornithidae|hesperornithid]] [[Hesperornithiformes|hesperornithiform]] |
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|- |
|- |
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| ''[[Iaceornis]]''<ref name="everhart-table-birds" /> |
| ''[[Iaceornis]]''<ref name="everhart-table-birds" /> |
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| [[Smoky Hill Chalk]]<ref name="everhart-table-birds" /> |
| [[Smoky Hill Chalk]]<ref name="everhart-table-birds" /> |
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| |
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| An [[Ichthyornithidae|ichthyornithid]] |
| An [[Ichthyornithidae|ichthyornithid]] |
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|- |
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| ''I. lentus''<ref name="distribution-niobrara" /> |
| ''I. lentus''<ref name="distribution-niobrara" /> |
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===Bivalves=== |
===Bivalves=== |
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''[[Haploscapha]]''<ref name="everhart-ypm1640" /> |
''[[Haploscapha]]''<ref name="everhart-ypm1640">"Material: YPM 1640," in "The Occurrence of Elasmosaurids..." Everhart (2006), page 172.</ref> |
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| |
| |
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| [[Fort Hays Limestone]]<ref name="everhart-ypm1640" /> |
| [[Fort Hays Limestone]]<ref name="everhart-ypm1640" /> |
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===Cephalopods=== |
===Cephalopods=== |
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| rowspan="34" | [[File:SouthDakotaBaculites.jpg|thumb|150px|center|''[[Baculites]]'']] |
| rowspan="34" | [[File:SouthDakotaBaculites.jpg|thumb|150px|center|''[[Baculites]]'']] |
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[[File: |
[[File:Enchoteuthis_reconstruction.png|thumb|150px|center| ''[[Enchoteuthis]]'']] |
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|- |
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| ''[[Clioscaphites]]''<ref name="everhart-table-inverts" /> |
| ''[[Clioscaphites]]''<ref name="everhart-table-inverts" /> |
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| style="background:#E6E6E6;" | [[Smoky Hill Chalk]]<ref name="everhart-table-inverts" /> |
| style="background:#E6E6E6;" | [[Smoky Hill Chalk]]<ref name="everhart-table-inverts" /> |
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| style="background:#E6E6E6;" | |
| style="background:#E6E6E6;" | |
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| style="background:#E6E6E6;" | A ''nomen dubium''.<ref name="muensterelloidea">{{cite journal |last1=Fuchs |first1=D. |last2=Iba |first2=Y. |last3=Heyng |first3=A. |last4=Iijima |first4=M. |last5=Klug |first5=C. |last6=Larson |first6=N. |last7=Schweigert |first7=G. |title=The Muensterelloidea: phylogeny and character evolution of Mesozoic stem octopods |journal=Papers in Palaeontology |date=28 June 2019 |volume=6 |issue=1 |doi=10.1002/spp2.1254 |url=https://onlinelibrary.wiley.com/doi/abs/10.1002/spp2.1254}}</ref> |
| style="background:#E6E6E6;" | A ''nomen dubium''.<ref name="muensterelloidea">{{cite journal |last1=Fuchs |first1=D. |last2=Iba |first2=Y. |last3=Heyng |first3=A. |last4=Iijima |first4=M. |last5=Klug |first5=C. |last6=Larson |first6=N. |last7=Schweigert |first7=G. |title=The Muensterelloidea: phylogeny and character evolution of Mesozoic stem octopods |journal=Papers in Palaeontology |date=28 June 2019 |volume=6 |issue=1 |pages=31–92 |doi=10.1002/spp2.1254 |s2cid=198256507 |url=https://onlinelibrary.wiley.com/doi/abs/10.1002/spp2.1254}}</ref> |
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|- |
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| rowspan=2 | ''[[Enchoteuthis]] |
| rowspan=2 | ''[[Enchoteuthis]]'' |
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| ''E. melanae'' |
| ''E. melanae'' |
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| [[Smoky Hill Chalk]] |
| [[Smoky Hill Chalk]] |
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| |
| |
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| Most material formerly referred to ''Tusoteuthis'' now belongs to this taxon. |
| Most material formerly referred to ''Tusoteuthis'' now belongs to this taxon.<ref name="muensterelloidea"/> |
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|- |
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| ''E. cobbani |
| ''E. cobbani'' |
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| [[Smoky Hill Chalk]] |
| [[Smoky Hill Chalk]] |
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===Echinoderms=== |
===Echinoderms=== |
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==Mosasaurs== |
==Mosasaurs== |
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[[Image:Ichthyosaurus Smithsonian.jpg|right|thumb|''[[Tylosaurus|Tylosaurus proriger]]'' specimen which was found with a plesiosaur in its stomach<ref>{{cite web|url=http://www.oceansofkansas.com/Tylo-prey.html |title=Tylosaur food |publisher=Oceansofkansas.com |date=2004-09-26 |accessdate=2016-04-13}}</ref>]] |
[[Image:Ichthyosaurus Smithsonian.jpg|right|thumb|''[[Tylosaurus|Tylosaurus proriger]]'' specimen which was found with a plesiosaur in its stomach<ref>{{cite web|url=http://www.oceansofkansas.com/Tylo-prey.html |title=Tylosaur food |publisher=Oceansofkansas.com |date=2004-09-26 |accessdate=2016-04-13}}</ref>]] |
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Mosasaurs are the most common marine reptiles in the Niobrara Chalk and the most successful ones in the sea at the time. |
Mosasaurs are the most common marine reptiles in the Niobrara Chalk and the most successful ones in the sea at the time. Several different genera representing the four different subfamilies of [[Mosasaur]]idae: the [[Tylosaurinae]], [[Plioplatecarpinae]], [[Mosasaurinae]], and [[Halisaurinae]], were present in Niobrara. They were the dominant carnivorous marine reptiles and ate cephalopods, fish, turtles, pterosaurs, birds, and even plesiosaurs.<ref>Everhart, M. J. 2002. New data on plesiosaur remains found as stomach contents of a Tylosaurus proriger (Squamata; Mosasauridae) from the Niobrara Formation of western Kansas. (Abstract) Transactions of the Kansas Academy of Science</ref> There is evidence of them consuming other smaller mosasaurs. Despite this, mosasaurs often fell prey to some of the large sharks at the time, such as ''[[Cretoxyrhina]]''.<ref>Everhart, M. J. 2004. Late Cretaceous interaction between predators and prey. Evidence of feeding by two species of shark on a mosasaur. PalArch, vertebrate palaeontology series 1(1):1-7.</ref> |
||
The presence of young mosasaurs in the formation suggests that mosasaurs were [[Viviparity|viviparous]] and gave birth hundreds of miles out to sea, as Niobrara was in the middle of the Western Interior Seaway at the time.<ref>Everhart, M. J. 2002. Remains of immature mosasaurs (Squamata; Mosasauridae) from the Niobrara Chalk (Late Cretaceous) argue against nearshore nurseries. (Abstract) Journal of Vertebrate Paleontology 22(suppl. to 3):52A.</ref> Juveniles would likely have been vulnerable to predation by the many large mid-ocean predators present in the ecosystem. |
The presence of young mosasaurs in the formation suggests that mosasaurs were [[Viviparity|viviparous]] and gave birth hundreds of miles out to sea, as Niobrara was in the middle of the Western Interior Seaway at the time.<ref>Everhart, M. J. 2002. Remains of immature mosasaurs (Squamata; Mosasauridae) from the Niobrara Chalk (Late Cretaceous) argue against nearshore nurseries. (Abstract) Journal of Vertebrate Paleontology 22(suppl. to 3):52A.</ref> Juveniles would likely have been vulnerable to predation by the many large mid-ocean predators present in the ecosystem. |
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{{clear}} |
{{clear}} |
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''[[ |
''[[Clidastes]]''<ref name="everhart-table-mosasaurs">"Table 13.1: Mosasaurs", Everhart (2005), page 245.</ref> |
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| style="background:#E6E6E6;" | ''C. liodontus''<ref name="everhart-table-mosasaurs" /> |
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| |
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| style="background:#E6E6E6;" | Smoky Hill Chalk<ref name="everhart-table-mosasaurs" /> |
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| style="background:#E6E6E6;" | |
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| Smoky Hill Chalk<ref name="everhart-table-mosasaurs-246" /> |
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| rowspan=2 | A large [[Tylosaurinae|tylosaurine]], with the largest ''T. proriger'' reaching about 13 metres in length. |
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| rowspan="99" | [[File:Tylosaurus_nepaeolicus_NT.png|thumb|center|150px|''[[Tylosaurus|Tylosaurus nepaeolicus]]'']] |
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[[Image:Platecarpus yale1.JPG|thumb|center|150px|Anterolateral view of ''Platecarpus tympaniticus'' skull at the [[Peabody Museum of Natural History]].]] |
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[[Image:Clidastes proph1DB.jpg|thumb|center|150px|''[[Clidastes|Clidastes propython]]'']] |
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| '' |
| ''C. prophython''<ref name="everhart-table-mosasaurs" /> |
||
| Smoky Hill Chalk<ref name="everhart-table-mosasaurs" /> |
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| |
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| |
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| |
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|- |
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| rowspan="3" | |
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''[[Ectenosaurus]]''<ref name="everhart-table-mosasaurs-246" /> |
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| ''E. clidastoides''<ref name="everhart-table-mosasaurs-246" /> |
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| Smoky Hill Chalk<ref name="everhart-table-mosasaurs-246" /> |
| Smoky Hill Chalk<ref name="everhart-table-mosasaurs-246" /> |
||
| |
| |
||
| |
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| |
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|- |
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| ''E. everhartorum''<ref>{{cite journal |last1=Willman |first1=A.J. |last2=Konishi |first2=T. |last3=Caldwell |first3=M.W. |year=2021 |title=A new species of ''Ectenosaurus'' (Mosasauridae: Plioplatecarpinae) from western Kansas, USA, reveals a novel suite of osteological characters for the genus |journal=Canadian Journal of Earth Sciences |volume=58 |issue=9 |pages=741–755 |doi=10.1139/cjes-2020-0175}}</ref> |
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| Smoky Hill Chalk |
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| |
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| |
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| |
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|- |
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|''E. tlemonectes''<ref>{{Cite journal |last=Kiernan |first=Caitlin R. |last2=Ebersole |first2=Jun A. |date=2023 |title=Two new plioplatecarpine mosasaurs (Mosasauridae; Plioplatecarpinae) of the genus Ectenosaurus from the Upper Cretaceous of North America |url=https://escholarship.org/uc/item/6jk04749 |journal=PaleoBios |language=en |volume=40 |issue=13 |doi=10.5070/P9401362375 |issn=0031-0298|doi-access=free }}</ref> |
|||
|Smoky Hill Chalk |
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| |
|||
| |
|||
| |
|||
|- |
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| ''[[Eonatator]]'' |
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| ''E. sternbergii'' |
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| Smoky Hill Chalk<ref name="BARDET">{{cite journal |year=2005 |title=A new species of ''Halisaurus'' from the Late Cretaceous phosphates of Morocco, and the phylogenetical relationships of the Halisaurinae (Squamata: Mosasauridae) |journal=Zoological Journal of the Linnean Society|volume=143 |pages=447–472 |vauthors=Bardet N, Suberbiola P, Iarochene M, Bouya B, Amaghzaz M |doi=10.1111/j.1096-3642.2005.00152.x |issue=3 |doi-access=free }}</ref><ref name="everhart-table-mosasaurs" /> |
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| |
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| A small [[Halisaurinae|halisaurine]] |
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| |
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|- |
|- |
||
| ''[[Platecarpus]]''<ref name="everhart-table-mosasaurs-246">"Table 13.1: Mosasaurs", Everhart (2005), page 246.</ref> |
| ''[[Platecarpus]]''<ref name="everhart-table-mosasaurs-246">"Table 13.1: Mosasaurs", Everhart (2005), page 246.</ref> |
||
| ''P. tympaniticus''<ref name="everhart-table-mosasaurs-246" /> |
| ''P. tympaniticus''<ref name="everhart-table-mosasaurs-246" /> |
||
| Smoky Hill Chalk<ref name="everhart-table-mosasaurs-246" /> |
| Smoky Hill Chalk<ref name="everhart-table-mosasaurs-246" /> |
||
| |
| |
||
| A [[Plioplatecarpinae|plioplatecarpine]] |
| A [[Plioplatecarpinae|plioplatecarpine]] |
||
| rowspan="94" |[[File:Tylosaurus_nepaeolicus_NT.png|thumb|center|150px|''[[Tylosaurus|Tylosaurus nepaeolicus]]'']] |
|||
[[Image:Platecarpus yale1.JPG|thumb|center|150px|Anterolateral view of ''Platecarpus tympaniticus'' skull at the [[Peabody Museum of Natural History]].]] |
|||
[[Image:Clidastes proph1DB.jpg|thumb|center|150px|''[[Clidastes|Clidastes propython]]'']] |
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|- |
|- |
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| ''[[Plesioplatecarpus]]'' |
| ''[[Plesioplatecarpus]]'' |
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Line 867: | Line 903: | ||
| |
| |
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|- |
|- |
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| rowspan=2 | |
| rowspan="2" | |
||
''[[ |
''[[Tylosaurus]]''<ref name="everhart-table-mosasaurs-246" /> |
||
| ''C. liodontus''<ref name="everhart-table-mosasaurs" /> |
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| Smoky Hill Chalk<ref name="everhart-table-mosasaurs" /> |
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| |
| |
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''T. nepaeolicus''<ref name="everhart-table-mosasaurs-246" /> |
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| rowspan=2 | A small [[Mosasaurinae|mosasaurine]] about 4m long |
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| Smoky Hill Chalk<ref name="everhart-table-mosasaurs-246" /> |
|||
|- |
|||
| ''C. prophython''<ref name="everhart-table-mosasaurs" /> |
|||
| Smoky Hill Chalk<ref name="everhart-table-mosasaurs" /> |
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| |
|||
|- |
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| ''[[Eonatator]]'' |
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| ''E. sternbergii'' |
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| |
| |
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| rowspan="2" | A large [[Tylosaurinae|tylosaurine]], with the largest ''T. proriger'' reaching about 13 metres in length. |
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| |
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| A small [[Halisaurinae|halisaurine]] only 2.5m long |
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|- |
|- |
||
| '' |
| ''T. proriger''<ref name="everhart-table-mosasaurs-246" /> |
||
| ''H. sternbergi''<ref name="everhart-table-mosasaurs-246" /> |
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| Smoky Hill Chalk<ref name="everhart-table-mosasaurs-246" /> |
| Smoky Hill Chalk<ref name="everhart-table-mosasaurs-246" /> |
||
| |
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| |
| |
||
|- |
|- |
||
| ''[[Selmasaurus]]''<ref name="Polcyn, 20082">Polcyn, M. J., and Everhart, M. J., 2008, Description and phylogenetic analysis of a new species of ''Selmasaurus'' (Mosasauridae: Plioplatecarpinae) from the Niobrara Chalk of western Kansas: In: Proceedings of the Second Mosasaur Meeting, edited by Everhart, M. J, Fort Hays Studies, Special Issue number 3, p. 13-28.</ref> |
|||
| ''[[Ectenosaurus]]''<ref name="everhart-table-mosasaurs-246" /> |
|||
| ''S. johnsoni'' |
|||
| ''E. clidastoides''<ref name="everhart-table-mosasaurs-246" /> |
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| Smoky Hill Chalk |
| Smoky Hill Chalk |
||
| |
| |
||
| |
| |
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Line 900: | Line 925: | ||
Plesiosaurs are present from two different families within [[Plesiosaur]]oidea in the Niobrara Chalk: the [[Polycotylidae]], or short-necked plesiosaurs, and the [[Elasmosauridae]], or long-necked plesiosaurs. Polycotylids superficially resemble [[pliosaur]]s, which are not present within the formation, but are unrelated. They were fast swimmers, unlike the Elasmosaurs that used their long necks to catch fish.<ref>{{cite web|url=http://www.oceansofkansas.com/FieldGuide3.html |title=Field Guide, Part 3; Marine reptiles |publisher=Oceansofkansas.com |date=2011-01-25 |accessdate=2016-04-13}}</ref> Plesiosaurs are rare in the formation and were therefore likely uncommon in the Western Interior Seaway at the time. Specimens become much more numerous in the [[Pierre Shale]] situated above the chalk. |
Plesiosaurs are present from two different families within [[Plesiosaur]]oidea in the Niobrara Chalk: the [[Polycotylidae]], or short-necked plesiosaurs, and the [[Elasmosauridae]], or long-necked plesiosaurs. Polycotylids superficially resemble [[pliosaur]]s, which are not present within the formation, but are unrelated. They were fast swimmers, unlike the Elasmosaurs that used their long necks to catch fish.<ref>{{cite web|url=http://www.oceansofkansas.com/FieldGuide3.html |title=Field Guide, Part 3; Marine reptiles |publisher=Oceansofkansas.com |date=2011-01-25 |accessdate=2016-04-13}}</ref> Plesiosaurs are rare in the formation and were therefore likely uncommon in the Western Interior Seaway at the time. Specimens become much more numerous in the [[Pierre Shale]] situated above the chalk. |
||
{| class="wikitable" style="margin:auto; width:100%;" |
{| class="wikitable" style="margin:auto; width:100%; width:100%;" |
||
|- |
|- |
||
! Genus |
! Genus |
||
Line 917: | Line 942: | ||
| 84.5-81.5 Ma ago<ref name=carpenter2003/> |
| 84.5-81.5 Ma ago<ref name=carpenter2003/> |
||
| A [[Polycotylidae|polycotylid]]. |
| A [[Polycotylidae|polycotylid]]. |
||
| rowspan="99" | |
|||
| rowspan="99" | [[Image:Dolichorhynchops BW.jpg|thumb|center|200px|''[[Dolichorhynchops|Dolichorhynchops osborni]]'']] |
|||
[[Image:Styxosaurus BW.jpg|thumb|center|200px|''[[Styxosaurus|Styxosaurus snowii]]'']] |
[[Image:Styxosaurus BW.jpg|thumb|center|200px|''[[Styxosaurus|Styxosaurus snowii]]'']] |
||
[[Image:Elasmosaurus2.jpg|thumb|center|200px|''[[Elasmosaurus|Elasmosaurus platyurus]]'']] |
[[Image:Elasmosaurus2.jpg|thumb|center|200px|''[[Elasmosaurus|Elasmosaurus platyurus]]'']] |
||
Line 926: | Line 951: | ||
| Smoky Hill Chalk<ref name="everhart-table-plesiosaurs" /> |
| Smoky Hill Chalk<ref name="everhart-table-plesiosaurs" /> |
||
| 84.5-81.5 Ma ago<ref name=carpenter2003/> |
| 84.5-81.5 Ma ago<ref name=carpenter2003/> |
||
| A [[Polycotylidae|polycotylid]] |
| A [[Polycotylidae|polycotylid]]. also present in the [[Pierre Shale Formation]] |
||
|- |
|- |
||
| style="background:#E6E6E6;" | ''[[Brimosaurus]]''<ref name="everhart-ypm1640-173">"Material: YPM 1640," in "The Occurrence of Elasmosaurids..." Everhart (2006), page 173.</ref> |
| style="background:#E6E6E6;" | ''[[Brimosaurus]]''<ref name="everhart-ypm1640-173">"Material: YPM 1640," in "The Occurrence of Elasmosaurids..." Everhart (2006), page 173.</ref> |
||
Line 940: | Line 965: | ||
| Smoky Hill Chalk<ref name="everhart-table-plesiosaurs" /> |
| Smoky Hill Chalk<ref name="everhart-table-plesiosaurs" /> |
||
| 85-81.5 Ma ago<ref name=carpenter2003/> |
| 85-81.5 Ma ago<ref name=carpenter2003/> |
||
| A large [[Elasmosauridae|elasmosaurid]] |
| A large [[Elasmosauridae|elasmosaurid]], also present in the Pierre Shale Formation |
||
|- |
|- |
||
|''[[Elasmosaurus]]''<ref name="everhart-table-plesiosaurs">"Table 13.1: Plesiosaurs," Everhart (2005), page 245.</ref> |
|''[[Elasmosaurus]]''<ref name="everhart-table-plesiosaurs">"Table 13.1: Plesiosaurs," Everhart (2005), page 245.</ref> |
||
Line 953: | Line 978: | ||
Two genre of pterosaurs are present in the formation, both within [[Pterodactyloidea]]: the [[pteranodontid]] ''[[Pteranodon]]'' (sometimes broken into several genera like ''[[Geosternbergia]]'' and ''[[Dawndraco]]'', though this is dubious) and the [[nyctosaurid]] ''[[Nyctosaurus]]''. They are large pterosaurs with elongated cranial crests. The pterosaurs of Niobrara probably spent most of their time at sea and rarely went on land, with ''[[Nyctosaurus]]'' being a probably fully pelagic animal. ''[[Pteranodon]]'' probably foraged on the ocean surface, while ''[[Nyctosaurus]]'' was a [[frigatebird]]-like aerial predator.<ref>Wilton, Mark P. (2013). Pterosaurs: Natural History, Evolution, Anatomy. Princeton University Press. {{ISBN|0691150613}}.</ref> |
Two genre of pterosaurs are present in the formation, both within [[Pterodactyloidea]]: the [[pteranodontid]] ''[[Pteranodon]]'' (sometimes broken into several genera like ''[[Geosternbergia]]'' and ''[[Dawndraco]]'', though this is dubious) and the [[nyctosaurid]] ''[[Nyctosaurus]]''. They are large pterosaurs with elongated cranial crests. The pterosaurs of Niobrara probably spent most of their time at sea and rarely went on land, with ''[[Nyctosaurus]]'' being a probably fully pelagic animal. ''[[Pteranodon]]'' probably foraged on the ocean surface, while ''[[Nyctosaurus]]'' was a [[frigatebird]]-like aerial predator.<ref>Wilton, Mark P. (2013). Pterosaurs: Natural History, Evolution, Anatomy. Princeton University Press. {{ISBN|0691150613}}.</ref> |
||
{| class="wikitable" style="margin:auto; width:100%;" |
{| class="wikitable" style="margin:auto; width:100%; width:100%;" |
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|- |
|- |
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! Genus |
! Genus |
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Line 968: | Line 993: | ||
| Smoky Hill Chalk<ref name="everhart-table-pteros" /> |
| Smoky Hill Chalk<ref name="everhart-table-pteros" /> |
||
|{{nowrap|85–84.5 Ma ago}}<ref name=carpenter2003>Carpenter, K. (2003). "Vertebrate Biostratigraphy of the Smoky Hill Chalk (Niobrara Formation) and the Sharon Springs Member (Pierre Shale)." ''High-Resolution Approaches in Stratigraphic Paleontology'', '''21''': 421-437. {{doi|10.1007/978-1-4020-9053-0}}</ref> |
|{{nowrap|85–84.5 Ma ago}}<ref name=carpenter2003>Carpenter, K. (2003). "Vertebrate Biostratigraphy of the Smoky Hill Chalk (Niobrara Formation) and the Sharon Springs Member (Pierre Shale)." ''High-Resolution Approaches in Stratigraphic Paleontology'', '''21''': 421-437. {{doi|10.1007/978-1-4020-9053-0}}</ref> |
||
| A [[ |
| A [[nyctosaurid]] [[ornithocheiroid]]. |
||
| rowspan="99" | [[Image:Nyctosaurus DB.jpg|thumb|center|150px|''[[Nyctosaurus|Nyctosaurus sp.]]'']] |
| rowspan="99" | [[Image:Nyctosaurus DB.jpg|thumb|center|150px|''[[Nyctosaurus|Nyctosaurus sp.]]'']] |
||
|- |
|- |
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Line 976: | Line 1,001: | ||
| Smoky Hill Chalk<ref name="everhart-table-pteros" /> |
| Smoky Hill Chalk<ref name="everhart-table-pteros" /> |
||
|86–84.5 Ma ago<ref name=carpenter2003/> |
|86–84.5 Ma ago<ref name=carpenter2003/> |
||
| rowspan=2 | A large [[Pteranodontidae|pteranodontid]] [[ |
| rowspan=2 | A large and very abundant [[Pteranodontidae|pteranodontid]] [[ornithocheiroid]]. |
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|- |
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| |
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| |
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| |
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|- |
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| rowspan=2 | |
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''[[Geosternbergia]]''<ref>{{cite web |title=Geosternbergia |url=https://www.pteros.com/pterosaurs/geosternbergia.html |website=Pteros|publisher=Pteros |access-date=28 August 2022}}</ref> |
|||
| {{nowrap|''G. sternbergi''}} |
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| Smoky Hill Chalk |
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|86–84.5 Ma ago |
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| rowspan=2 | A species of Pterosaur that is regarded by a few Paleontologists to be a species of Pteranodon, though most regard it as a distinct species. |
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|- |
|- |
||
| |
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| {{nowrap|''P. sternbergi''}}<ref name="everhart-table-pteros" /> |
|||
| {{nowrap|Smoky Hill Chalk}}<ref name="everhart-table-pteros" /> |
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|88–85 Ma ago<ref name=carpenter2003/> |
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|} |
|} |
||
==Turtles== |
==Turtles== |
||
[[Sea turtle]]s have been found from the Niobrara Chalk that reached large sizes. The biggest, ''[[Archelon]]'', |
[[Sea turtle]]s have been found from the Niobrara Chalk that reached large sizes. The biggest, ''[[Archelon]]'', was considerably larger than its distant relative, the [[leatherback sea turtle]], which is the largest of the sea turtles alive today. The sea turtles most likely fed on ammonites, squid, and other [[cephalopod]]s. |
||
{| class="wikitable" style="margin:auto;" |
{| class="wikitable" style="margin:auto; width:100%;" |
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|- |
|- |
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! Genus |
! Genus |
||
Line 1,029: | Line 1,063: | ||
| Smoky Hill Chalk<ref name="everhart-table-turtles" /> |
| Smoky Hill Chalk<ref name="everhart-table-turtles" /> |
||
| |
| |
||
| A [[Protostegidae|protostegid]] [[Cryptodira|cryptodire]] |
| A [[Protostegidae|protostegid]] [[Cryptodira|cryptodire]] |
||
|- |
|- |
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| ''[[Toxochelys]]''<ref name="everhart-table-turtles" /> |
| ''[[Toxochelys]]''<ref name="everhart-table-turtles" /> |
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Line 1,035: | Line 1,069: | ||
| Smoky Hill Chalk<ref name="everhart-table-turtles" /> |
| Smoky Hill Chalk<ref name="everhart-table-turtles" /> |
||
| |
| |
||
| A [[Chelonioidea|chelonioid]] [[Cryptodira|cryptodire]] |
| A [[Chelonioidea|chelonioid]] [[Cryptodira|cryptodire]] |
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|} |
|} |
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Line 1,046: | Line 1,080: | ||
* Shimada, K. 2007. "Skeletal and dental anatomy of lamniform shark, Cretalamna appendiculata from Upper Cretaceous Niobrara Chalk of Kansas". ''Journal of Vertebrate Paleontology'', 27(3):584–602. |
* Shimada, K. 2007. "Skeletal and dental anatomy of lamniform shark, Cretalamna appendiculata from Upper Cretaceous Niobrara Chalk of Kansas". ''Journal of Vertebrate Paleontology'', 27(3):584–602. |
||
* Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): ''The Dinosauria'', 2nd, Berkeley: University of California Press. 861 pp. {{ISBN|0-520-24209-2}}. |
* Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): ''The Dinosauria'', 2nd, Berkeley: University of California Press. 861 pp. {{ISBN|0-520-24209-2}}. |
||
{{Commons category|Niobrara Formation}} |
{{Commons category|Paleobiota of the Niobrara Formation}} |
||
[[Category:Geology of Kansas]] |
[[Category:Geology of Kansas]] |
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[[Category:Upper Cretaceous Series of North America]] |
[[Category:Upper Cretaceous Series of North America]] |
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[[Category:Prehistoric fauna by locality|Niobrara]] |
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[[Category:Mesozoic paleobiotas]] |
Revision as of 05:11, 15 December 2024
During the time of the deposition of the Niobrara Chalk, much life inhabited the seas of the Western Interior Seaway. By this time in the Late Cretaceous many new lifeforms appeared such as mosasaurs, which were to be some of the last of the aquatic lifeforms to evolve before the end of the Mesozoic. Life of the Niobrara Chalk is comparable to that of the Dakota Formation, although the Dakota Formation, which was deposited during the Cenomanian, predates the chalk by about 10 million years.
Table key
Color | Explanation |
---|---|
Light grey | A "regular" taxon which the scientific consensus does not regard as a dubious, synonymous, undescribed, or otherwise taxonomically questionable name. |
Dark grey | A taxon or parataxon that is misidentified, dubious, synonymous, undescribed, or otherwise taxonomically questionable name. |
Peach | An ichnotaxon, a parataxon representing a specific kind of trace fossil. |
Light blue | An ootaxon, a parataxon representing a specific kind of fossil egg. |
Light green | A morphotaxon, a parataxon representing a single stage or anatomical part of a plant or plant-like organism. Examples include fossil pine cones, fungal spores, and leaves. |
Bony fish
Pycnodontiformes
Genus | Species | Member | Abundance | Notes |
---|---|---|---|---|
Micropycnodon[1] | M. kansasensis[1] | Smoky Hill Chalk[1] | A pycnodontiform fish similar but unrelated to modern parrotfish |
Semionotiformes
Genus | Species | Member | Abundance | Notes |
---|---|---|---|---|
H. marshi[1] | Smoky Hill Chalk[1] | Family Hadrodontidae Thurmond and Jones 1981 |
Pachycormiformes
Genus | Species | Member | Abundance | Notes | Images |
---|---|---|---|---|---|
Protosphyraena[1] | P. bentonianum | A swordfish-like pachycormid | |||
P. nitida[1] | Smoky Hill Chalk[1] | ||||
P. perniciosa[1] | Smoky Hill Chalk[1] | ||||
P. tenuis[1] | Smoky Hill Chalk[1] | ||||
P. gladius[1] | Smoky Hill Chalk[1] | Named as a new genus, Bonnerichthys | |||
Bonnerichthys[2] | B. gladius | Smoky Hill Chalk[3] | A filter feeding pachycormid |
Crossognathiformes
Genus | Species | Member | Abundance | Notes | Images |
---|---|---|---|---|---|
Apsopelix[3] | A. anglicus[3] | Smoky Hill Chalk[3] | A crossognathid. | ||
Pachyrhizodus[3] | P. caninus[3] | Smoky Hill Chalk[3] | A pachyrhizodontid | ||
P. leptopsis[3] | Smoky Hill Chalk[3] | ||||
P. minimus[3] | Smoky Hill Chalk[3] |
Ichthyodectiformes
Genus | Species | Member | Abundance | Notes | Images |
---|---|---|---|---|---|
Xiphactinus[3] | X. audax[3] | Smoky Hill Chalk[3] | A large ichthyodectid | ||
Ichthyodectes[3] | I. ctenodon[3] | Smoky Hill Chalk[3] | An ichthyodectid | ||
Gillicus[3] | G. arcuantus[3] | Smoky Hill Chalk[3] | A saurodontid | ||
Saurodon[3] | S. leanus[3] | Smoky Hill Chalk[3] | A saurodontid | ||
Saurocephalus[3] | S. lanciformis[3] | Smoky Hill Chalk[3] | A saurodontid |
Tselfatiiformes
Genus | Species | Member | Abundance | Notes | Images |
---|---|---|---|---|---|
Thryptodus[3] | T. zitteli[3] | Smoky Hill Chalk[3] | A plethodid | ||
Pentanogmius[3] | P. evolutus[3] | Smoky Hill Chalk[3] | A plethodid | ||
Martinichthys[3] | M. brevis[3] | Smoky Hill Chalk[3] | A plethodid | ||
M. xiphoides[3] | Smoky Hill Chalk[3] | ||||
Niobrara[3] | N. encarsia[3] | Smoky Hill Chalk[3] | A plethodid | ||
Zanclites[3] | Z. xenurus[3] | Smoky Hill Chalk[3] | A plethodid |
Aulopiformes
Genus | Species | Member | Abundance | Notes | Images |
---|---|---|---|---|---|
Cimolichthys[3] | C. nepaholica[3] | Smoky Hill Chalk[3] | A cimolichthyid | ||
E. dirus[3] | Smoky Hill Chalk[3] | An enchodontid | |||
E. gladiolus[3] | Smoky Hill Chalk[3] | ||||
E. petrosus[3] | Smoky Hill Chalk[3] | ||||
E. shumardi[3] | Smoky Hill Chalk[3] | ||||
Apateodus[3] | Indeterminate[3] | Smoky Hill Chalk[3] | An alepisauriform actinopterygiian related to the modern lancetfish and lizardfish | ||
Stratodus[3] | S. apicalis[3] | Smoky Hill Chalk[3] | An alepisauriform actinopterygiian | ||
Leptecodon[3] | L. rectus[citation needed] | An alepisauriform actinopterygiian |
Beryciformes
Genus | Species | Member | Abundance | Notes |
---|---|---|---|---|
Kansius[3] | K. sternbergi[3] | Smoky Hill Chalk[3] | A beryciform actinopterygiian | |
Trachichthyoides[3] | Indeterminate[3] | Smoky Hill Chalk[3] | A beryciform actinopterygiian | |
Caproberyx[3] | Indeterminate[3] | Smoky Hill Chalk[3] | A beryciform actinopterygiian |
Other bony fish
Genus | Species | Member | Abundance | Notes |
---|---|---|---|---|
Indeterminate[1] | Smoky Hill Chalk[1] | A lepisosteid gar | ||
Paraliodesmus[3] | P. guadagnii[3] | Smoky Hill Chalk[3] | An amiiform | |
Urenchelys[3] | U. abditus[3] | Smoky Hill Chalk[3] | An anguilliform | |
Ferrifrons | F. rugosus | A ferrifronsid acanthomorph | ||
Aethocephalichthys[3] | A. hyainarhinos[3] | Smoky Hill Chalk[3] | An actinopterygian of indeterminate classification[4] | |
Omosoma | O. garretti | A polymixiid actinopterygiian closely related to the modern Beardfish | ||
Belonostomus[1] | Indeterminate[1] | An aspidorhynchid |
Cartilaginous fish
Fish are by far the most common fossils found from the formation, with remains of prehistoric sharks, ray-finned fishes, and lobe-finned fishes in abundance. As well as smaller fish, many large predatory fish were present in the seas at that time, most notably Xiphactinus. Several fish were of close relation to modern day fish including primitive coelacanths, slime heads, lancetfish, gars, swordfish, and salmonids.
Sharks
Genus | Species | State | Member | Abundance | Notes | Images |
---|---|---|---|---|---|---|
C. mantelli[5] | Smoky Hill Chalk[5] | A large lamniform shark | ||||
C. appendiculata[6] | Smoky Hill Chalk[6] | A lamniform shark | ||||
C. appendiculata[5] |
N/A | N/A | N/A | An extremely widely used lapsus calami for Cretalamna.[7] | ||
Johnlongia[5] | Indeterminate[5] | Smoky Hill Chalk[5] | An odontaspidid lamniform shark | |||
Pseudocorax[5] | P. laevis[5] | Smoky Hill Chalk[5] | A lamniform shark smaller than Cretoxyrhina | |||
Squalicorax[5] | S. falcatus[5] | Smoky Hill Chalk[5] | A lamniform | |||
S. kaupi[5] | Smoky Hill Chalk[5] | |||||
S. pristodontus[5] | Smoky Hill Chalk[5] | |||||
Scapanorhynchus[5] | S. raphiodon[5] | Smoky Hill Chalk[5] | A mitsukurinid shark similar in appearance to the modern day goblin shark | |||
Ptychodus[5] | P. anonymus[5] | Smoky Hill Chalk[5] | A ptychodontid lamniform shark | |||
P. martini[5] | Smoky Hill Chalk[5] | |||||
P. mortoni[5] |
Smoky Hill Chalk[5] | |||||
P. occidentalis[5] | Smoky Hill Chalk[5] | |||||
P. polygyrus[5] | Smoky Hill Chalk[5] |
Other cartilaginous fish
Genus | Species | State | Member | Abundance | Notes | Images |
---|---|---|---|---|---|---|
E. laqueatus[citation needed] |
A callorhinchid chimaeriform related to the modern ratfish | |||||
Rhinobatos[5] | R. incertus[5] | Smoky Hill Chalk[5] |
Dinosaurs
Nonavian dinosaurs have been found in the Niobrara Chalk despite it being located hundreds of miles out to sea at the time. The most reasonable theory is that the carcasses drifted out to sea. It is unlikely that the bodies were carried out by outgoing tides along the shorelines where they died, but rather it is more probable that the dinosaurs were carried offshore by floodwaters during a storm. In the shallow waters the bodies would have begun to decompose and bacteria within the carcass would have produced gasses that would have accumulated in the gut, thereby making the body buoyant. Next, the prevailing winds and currents would have carried it out to sea, where it would eventually settle to the bottom and be buried in sediment.[8]
A few caudal vertebrae from a hadrosaur have been found with bite marks and have been eroded, suggesting at one point they were digested. A single tooth belonging to Squalicorax was found in situ under the vertebrae. This suggested the shark consumed the posterior end of the tail of a floating hadrosaur carcass and had partially digested it before fossilization.[9][10] Most dinosaurs in the chalk were nodosaurs. The dinosaurs found here were endemic to Appalachia.[11]
Non-avian
Genus | Species | State | Member | Material | Notes | Images |
---|---|---|---|---|---|---|
C. agilis[12] |
Kansas[13] | Smoky Hill Chalk[12] |
"Single articulated postcranial skeleton with associated skull fragments."[14] |
A small hadrosaurid | ||
Indeterminate hadrosaurid[15] | A hadrosaurid of indeterminate classification. Possibly Corythosaurus.[15] | |||||
N. coleii[12] |
Kansas[13] | Smoky Hill Chalk[12] | "Partial skeleton."[16] | A nodosaurid ankylosaur. | ||
Hierosaurus[12] | H. sternbergi[12] | Kansas[13] | Smoky Hill Chalk[12] | "Osteoderms."[17] | A nodosaurid ankylosaur. |
Birds
Three genre of birds are present in the formation, although rare. They were unrelated to modern birds, as they still retained teeth. Baptornis and Hesperornis were large flightless aquatic birds suited for diving. Ichthyornis was a seabird that resembled the gulls and petrels of today. Both probably preyed on small fish and were preyed upon by sharks, large bony fish such as Xiphactinus, and mosasaurs.
Genus | Species | State | Member | Material | Notes | Images |
---|---|---|---|---|---|---|
Apatornis[18] | A. celer[18] | Smoky Hill Chalk[18] | "Postcranial elements."[20] | |||
Baptornis[18] | B. advenus[18] | Smoky Hill Chalk[18] | "Fragmentary skull [and] nearly complete postcranium."[21] | A baptornithid hesperornithiform | ||
Guildavis[18] | G. tener[18] | Smoky Hill Chalk[18] | ||||
H. crassipes[13] | Kansas[13] | "Partial postcranial skeleton."[21] | ||||
H. gracilis[13] | Kansas[13] | "Tarsometatarsus."[21] | ||||
H. regalis[18] |
Kansas[13] | Smoky Hill Chalk[18] | A large hesperornithid hesperornithiform | |||
Iaceornis[18] | I. marshi[18] | Smoky Hill Chalk[18] | ||||
I. agilis[13] |
Kansas[13] | Junior synonym of I. dispar.[13] | ||||
I. anceps[13] | Kansas[13] | Junior synonym of I. dispar.[13] | ||||
I. dispar[18] |
Kansas[13] | Smoky Hill Chalk[18] | An ichthyornithid | |||
I. lentus[13] | Kansas[13] | |||||
I. tener[13] | Kansas[13] | |||||
I. validus[13] |
Kansas[13] | Junior synonym of I. dispar.[13] | ||||
I. victor[13] | Kansas[13] | Junior synonym of I. dispar.[13] | ||||
Parahesperornis[18] | P. alexi[18] | Kansas[13] | Smoky Hill Chalk[18] | "Partial skull [and] complete postcranium."[21] |
Invertebrates
Clams, oysters, crinoids, ammonites, and squid are all common in the Niobrara Chalk and must have constituted the majority of life at the time. Evidence of sponges, annelid worms, and crustaceans are less common and are usually found as trace fossils.
Bivalves
Genus | Species | Member | Abundance | Notes | Images |
---|---|---|---|---|---|
C. undulatoplicatus[22] |
Smoky Hill Chalk[22] | ||||
D. maxima[22] |
Smoky Hill Chalk[22] | ||||
Fort Hays Limestone[23] | |||||
Fort Hays Limestone[23] | |||||
Ostrea[23] | Fort Hays Limestone[23] | ||||
P. platinus[22] |
Smoky Hill Chalk[22] | ||||
P. congesta[22] |
Smoky Hill Chalk[22] | ||||
V. grandis[22] | Smoky Hill Chalk[22] |
Cephalopods
Genus | Species | Member | Abundance | Notes | Images |
---|---|---|---|---|---|
Smoky Hill Chalk[22] | |||||
Clioscaphites[22] | Smoky Hill Chalk[22] | ||||
Rugaptychus[22] | Smoky Hill Chalk[22] | ||||
Spinaptychus[22] | Smoky Hill Chalk[22] | ||||
Tusoteuthis[22] | T. longa | Smoky Hill Chalk[22] | A nomen dubium.[24] | ||
Enchoteuthis | E. melanae | Smoky Hill Chalk | Most material formerly referred to Tusoteuthis now belongs to this taxon.[24] | ||
E. cobbani | Smoky Hill Chalk | ||||
Niobrarateuthis | N. bonneri | Smoky Hill Chalk |
Echinoderms
Genus | Species | State | Member | Abundance | Notes |
---|---|---|---|---|---|
"Unitacrinus"[22] | "U. socialis"[22] | N/A | N/A | N/A | Common lapsus calami of Uintacrinus |
Uintacrinus |
Mosasaurs
Mosasaurs are the most common marine reptiles in the Niobrara Chalk and the most successful ones in the sea at the time. Several different genera representing the four different subfamilies of Mosasauridae: the Tylosaurinae, Plioplatecarpinae, Mosasaurinae, and Halisaurinae, were present in Niobrara. They were the dominant carnivorous marine reptiles and ate cephalopods, fish, turtles, pterosaurs, birds, and even plesiosaurs.[26] There is evidence of them consuming other smaller mosasaurs. Despite this, mosasaurs often fell prey to some of the large sharks at the time, such as Cretoxyrhina.[27]
The presence of young mosasaurs in the formation suggests that mosasaurs were viviparous and gave birth hundreds of miles out to sea, as Niobrara was in the middle of the Western Interior Seaway at the time.[28] Juveniles would likely have been vulnerable to predation by the many large mid-ocean predators present in the ecosystem.
Genus | Species | Member | Abundance | Notes | Images |
---|---|---|---|---|---|
C. liodontus[29] | Smoky Hill Chalk[29] | ||||
C. prophython[29] | Smoky Hill Chalk[29] | ||||
E. clidastoides[30] | Smoky Hill Chalk[30] | ||||
E. everhartorum[31] | Smoky Hill Chalk | ||||
E. tlemonectes[32] | Smoky Hill Chalk | ||||
Eonatator | E. sternbergii | Smoky Hill Chalk[33][29] | A small halisaurine | ||
Platecarpus[30] | P. tympaniticus[30] | Smoky Hill Chalk[30] | A plioplatecarpine | ||
Plesioplatecarpus | P. planifrons[30] | Smoky Hill Chalk[30] | |||
T. nepaeolicus[30] |
Smoky Hill Chalk[30] | A large tylosaurine, with the largest T. proriger reaching about 13 metres in length. | |||
T. proriger[30] | Smoky Hill Chalk[30] | ||||
Selmasaurus[34] | S. johnsoni | Smoky Hill Chalk |
Plesiosaurs
Plesiosaurs are present from two different families within Plesiosauroidea in the Niobrara Chalk: the Polycotylidae, or short-necked plesiosaurs, and the Elasmosauridae, or long-necked plesiosaurs. Polycotylids superficially resemble pliosaurs, which are not present within the formation, but are unrelated. They were fast swimmers, unlike the Elasmosaurs that used their long necks to catch fish.[35] Plesiosaurs are rare in the formation and were therefore likely uncommon in the Western Interior Seaway at the time. Specimens become much more numerous in the Pierre Shale situated above the chalk.
Genus | Species | State | Member | Time span | Notes | Images |
---|---|---|---|---|---|---|
P. latipinnis[36] | Smoky Hill Chalk[36] | 84.5-81.5 Ma ago[37] | A polycotylid. | |||
Dolichorhynchops[36] | D. osborni[36] | Smoky Hill Chalk[36] | 84.5-81.5 Ma ago[37] | A polycotylid. also present in the Pierre Shale Formation | ||
Brimosaurus[38] | B. grandis | Kansas[38] | Fort Hays Limestone[38] | A nomen dubium. | ||
Styxosaurus[36] | S. snowii[36] | Smoky Hill Chalk[36] | 85-81.5 Ma ago[37] | A large elasmosaurid, also present in the Pierre Shale Formation | ||
Elasmosaurus[36] | "E." sternbergi[36] | Smoky Hill Chalk[36] | 84.5-81.5 Ma ago | Most likely not referable to Elasmosaurus. |
Pterosaurs
Two genre of pterosaurs are present in the formation, both within Pterodactyloidea: the pteranodontid Pteranodon (sometimes broken into several genera like Geosternbergia and Dawndraco, though this is dubious) and the nyctosaurid Nyctosaurus. They are large pterosaurs with elongated cranial crests. The pterosaurs of Niobrara probably spent most of their time at sea and rarely went on land, with Nyctosaurus being a probably fully pelagic animal. Pteranodon probably foraged on the ocean surface, while Nyctosaurus was a frigatebird-like aerial predator.[39]
Genus | Species | Member | Time span | Notes | Images |
---|---|---|---|---|---|
N. gracilis[40] |
Smoky Hill Chalk[40] | 85–84.5 Ma ago[37] | A nyctosaurid ornithocheiroid. | ||
P. longiceps[40] | Smoky Hill Chalk[40] | 86–84.5 Ma ago[37] | A large and very abundant pteranodontid ornithocheiroid. | ||
G. sternbergi | Smoky Hill Chalk | 86–84.5 Ma ago | A species of Pterosaur that is regarded by a few Paleontologists to be a species of Pteranodon, though most regard it as a distinct species. | ||
Turtles
Sea turtles have been found from the Niobrara Chalk that reached large sizes. The biggest, Archelon, was considerably larger than its distant relative, the leatherback sea turtle, which is the largest of the sea turtles alive today. The sea turtles most likely fed on ammonites, squid, and other cephalopods.
Genus | Species | Member | Abundance | Notes | Images |
---|---|---|---|---|---|
B. barberi[42] |
Smoky Hill Chalk[42] | ||||
Chelosphargis[42] | C. advena[42] | Smoky Hill Chalk[42] | |||
C. stenopora[42] |
Smoky Hill Chalk[42] | ||||
Porthochelys[42] | P. laticeps[42] | Smoky Hill Chalk[42] | A toxichelid cryptodire | ||
Protostega[42] | P. gigas[42] | Smoky Hill Chalk[42] | A protostegid cryptodire | ||
Toxochelys[42] | T. latiremis[42] | Smoky Hill Chalk[42] | A chelonioid cryptodire |
Footnotes
- ^ a b c d e f g h i j k l m n o p q r s t "Table 13.1: Bony Fish", Everhart (2005), page 244.
- ^ Viegas, Jennifer (18 February 2010), SUV-Sized Fish Were Earliest Filter-Feeders, Discovery News, retrieved 1 April 2010
- ^ a b c d e f g h i j k l m n o p q r s t u v w x y z aa ab ac ad ae af ag ah ai aj ak al am an ao ap aq ar as at au av aw ax ay az ba bb bc bd be bf bg bh bi bj bk bl bm bn bo bp bq br bs bt bu bv bw bx by bz ca cb "Table 13.1: Bony Fish", Everhart (2005), page 245.
- ^ Fielitz, C.; Stewart, J. D.; & Wiffen, J. 1999. Aethocephalichthys hyainarhinos gen. et sp. nov., a new and enigmatic Late Cretaceous actinopterygian from North America and New Zealand. Mesozoic Fishes 2 – Systematics and Fossil Record, G. Arratia & H.-P. Schultze (eds.): pp. 95-106, 7 figs.
- ^ a b c d e f g h i j k l m n o p q r s t u v w x y z aa ab ac ad ae af ag ah ai "Table 13.1: Sharks/Rays", Everhart (2005), page 244
- ^ a b c "Table 13.1: Sharks/Rays," Everhart (2005), page 244. Note that Cretalamna is listed here under the widely used lapsus calami Cretolamna.
- ^ "Introduction", in "Skeletal and Dental Anatomy..." Shimada (2007), page 584
- ^ "Niobrarasaurus". Oceansofkansas.com. Retrieved 2016-04-13.
- ^ "Shark bit dino". Oceansofkansas.com. Retrieved 2016-04-13.
- ^ Everhart, M. J. and K. Ewell. 2006. Shark-bitten dinosaur (Hadrosauridae) vertebrae from the Niobrara Chalk (Upper Coniacian) of western Kansas. Kansas Academy of Science, Transactions, 109 (1-2):27-35.
- ^ Brownstein, Chase D. (February 2018). "The biogeography and ecology of the Cretaceous non-avian dinosaurs of Appalachia". Palaeontologia Electronica. 21 (1.5A): 1–56. doi:10.26879/801. Retrieved 21 March 2021.
- ^ a b c d e f g h i "Table 13.1: Dinosaurs", Everhart (2005), page 246.
- ^ a b c d e f g h i j k l m n o p q r s t u v w x y z aa "Dinosaur distribution (Late Cretaceous; North America; Kansas; Niobrara Chalk Formation)." Weishampel, et al. (2004). Pp. 582.
- ^ "Table 20.1," in Weishampel, et al. (2004). Page 439.
- ^ a b Everhart, Michael J.; Ewell, Keith (April 2006). "Shark-bitten dinosaur (Hadrosauridae) caudal vertebrae from the Niobrara Chalk (Upper Coniacian) of western Kansas". Transactions of the Kansas Academy of Science. 109 (1 & 2): 27–35. doi:10.1660/0022-8443(2006)109[27:sdhcvf]2.0.co;2. ISSN 0022-8443. S2CID 86366930.
- ^ "Table 17.1," in Weishampel, et al. (2004). Page 367.
- ^ "Table 17.1," in Weishampel, et al. (2004). Page 368.
- ^ a b c d e f g h i j k l m n o p q r s t u "Table 13.1: Birds," Everhart (2005), page 246.
- ^ "Dinosaur distribution (Late Cretaceous; North America; Nebraska; Niobrara Chalk Formation)." Weishampel, et al. (2004). Pp. 586.
- ^ "Table 11.1," in Weishampel, et al. (2004). Page 214.
- ^ a b c d "Table 11.1," in Weishampel, et al. (2004). Page 215.
- ^ a b c d e f g h i j k l m n o p q r s t u v w x y z aa "Table 13.1: Invertebrates," Everhart (2005), page 244.
- ^ a b c d e f "Material: YPM 1640," in "The Occurrence of Elasmosaurids..." Everhart (2006), page 172.
- ^ a b Fuchs, D.; Iba, Y.; Heyng, A.; Iijima, M.; Klug, C.; Larson, N.; Schweigert, G. (28 June 2019). "The Muensterelloidea: phylogeny and character evolution of Mesozoic stem octopods". Papers in Palaeontology. 6 (1): 31–92. doi:10.1002/spp2.1254. S2CID 198256507.
- ^ "Tylosaur food". Oceansofkansas.com. 2004-09-26. Retrieved 2016-04-13.
- ^ Everhart, M. J. 2002. New data on plesiosaur remains found as stomach contents of a Tylosaurus proriger (Squamata; Mosasauridae) from the Niobrara Formation of western Kansas. (Abstract) Transactions of the Kansas Academy of Science
- ^ Everhart, M. J. 2004. Late Cretaceous interaction between predators and prey. Evidence of feeding by two species of shark on a mosasaur. PalArch, vertebrate palaeontology series 1(1):1-7.
- ^ Everhart, M. J. 2002. Remains of immature mosasaurs (Squamata; Mosasauridae) from the Niobrara Chalk (Late Cretaceous) argue against nearshore nurseries. (Abstract) Journal of Vertebrate Paleontology 22(suppl. to 3):52A.
- ^ a b c d e f "Table 13.1: Mosasaurs", Everhart (2005), page 245.
- ^ a b c d e f g h i j k l m "Table 13.1: Mosasaurs", Everhart (2005), page 246.
- ^ Willman, A.J.; Konishi, T.; Caldwell, M.W. (2021). "A new species of Ectenosaurus (Mosasauridae: Plioplatecarpinae) from western Kansas, USA, reveals a novel suite of osteological characters for the genus". Canadian Journal of Earth Sciences. 58 (9): 741–755. doi:10.1139/cjes-2020-0175.
- ^ Kiernan, Caitlin R.; Ebersole, Jun A. (2023). "Two new plioplatecarpine mosasaurs (Mosasauridae; Plioplatecarpinae) of the genus Ectenosaurus from the Upper Cretaceous of North America". PaleoBios. 40 (13). doi:10.5070/P9401362375. ISSN 0031-0298.
- ^ Bardet N, Suberbiola P, Iarochene M, Bouya B, Amaghzaz M (2005). "A new species of Halisaurus from the Late Cretaceous phosphates of Morocco, and the phylogenetical relationships of the Halisaurinae (Squamata: Mosasauridae)". Zoological Journal of the Linnean Society. 143 (3): 447–472. doi:10.1111/j.1096-3642.2005.00152.x.
- ^ Polcyn, M. J., and Everhart, M. J., 2008, Description and phylogenetic analysis of a new species of Selmasaurus (Mosasauridae: Plioplatecarpinae) from the Niobrara Chalk of western Kansas: In: Proceedings of the Second Mosasaur Meeting, edited by Everhart, M. J, Fort Hays Studies, Special Issue number 3, p. 13-28.
- ^ "Field Guide, Part 3; Marine reptiles". Oceansofkansas.com. 2011-01-25. Retrieved 2016-04-13.
- ^ a b c d e f g h i j k l "Table 13.1: Plesiosaurs," Everhart (2005), page 245.
- ^ a b c d e Carpenter, K. (2003). "Vertebrate Biostratigraphy of the Smoky Hill Chalk (Niobrara Formation) and the Sharon Springs Member (Pierre Shale)." High-Resolution Approaches in Stratigraphic Paleontology, 21: 421-437. doi:10.1007/978-1-4020-9053-0
- ^ a b c "Material: YPM 1640," in "The Occurrence of Elasmosaurids..." Everhart (2006), page 173.
- ^ Wilton, Mark P. (2013). Pterosaurs: Natural History, Evolution, Anatomy. Princeton University Press. ISBN 0691150613.
- ^ a b c d e f "Table 13.1: Pterosaurs," Everhart (2005), page 246.
- ^ "Geosternbergia". Pteros. Pteros. Retrieved 28 August 2022.
- ^ a b c d e f g h i j k l m n o p q r "Table 13.1: Turtles," Everhart (2005), page 245.
References
- Everhart, Michael J. Oceans Of Kansas: A Natural History Of The Western Interior Sea (Life of the Past). Bloomington: Indiana University Press, 2005. 322 pp.
- Everhart, Michael J. 2006. "The Occurrence of Elasmosaurids (Reptilia: Plesiosauria) in the Niobrara Chalk of Western Kansas"; Paludicila; 5(4) pp. 170–183
- Shimada, K. 2007. "Skeletal and dental anatomy of lamniform shark, Cretalamna appendiculata from Upper Cretaceous Niobrara Chalk of Kansas". Journal of Vertebrate Paleontology, 27(3):584–602.
- Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. 861 pp. ISBN 0-520-24209-2.