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Timeline of environmental history: Difference between revisions

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*874 - According to [[Landnámabók]], the settlement of [[Iceland]] begins.
*874 - According to [[Landnámabók]], the settlement of [[Iceland]] begins.


===10th century==
===10th century===
*930 - [[Althing]], oldest [[parliament]]ary institution in the world that is still in existance, is founded
*930 - [[Althing]], oldest [[parliament]]ary institution in the world that is still in existance, is founded
*980s - [[Greenland#Norse_settlement|Greenland]] settled by [[Viking]] colonists from [[Iceland]]
*980s - [[Greenland#Norse_settlement|Greenland]] settled by [[Viking]] colonists from [[Iceland]]

Revision as of 19:23, 25 February 2011

The timeline lists geological, astronomical, and climatological events in relation to events in human history which they influenced. For the history of humanity's perspective on these events, see timeline of the history of environmentalism.

Year(s) Event(s)
Start End
c. 2,588,000 BC c. 12,000 BC Pleistocene era
c. 19,000 BC Last Glacial Maximum/sea-level minimum
c. 20,000 BC c. 12,150 BC Mesolithic 1 period
c. 17,000 BC c. 13,000 BC Oldest Dryas stadial (cool period) during the last Ice age/glaciation in Europe.
c. 13,000 BC Beginning of the Holocene extinction. Earliest evidence of warfare
c. 12,670 BC c. 12,000 BC Bølling oscillation interstadial (warm and moist period) between the Oldest Dryas and Older Dryas stadials (cool periods) at the end of the Last glacial period. In places where the Older Dryas was not seen, it is known as the Bølling-Allerød.
c. 12,340 BC c. 11,140 BC Cemetary 117: site of the world's first battle/war.
c. 12,500 BC c. 10,800 BC Natufian culture begins minor agriculture
c. 12,150 BC c. 11,140 BC Mesolithic 2 (Natufian culture), some sources have Mesolithic 2 ending at 9500 BC
c. 12,000 BC c. 11,700 BC Older Dryas stadial (cool period)
c. 11,700 BC c. 10,800 BC Allerød oscillation
c. 13,000 BC c. 11,000 BC Lake Agassiz forms from glacial meltwater, floods through the Mackenzie River into the Arctic Ocean at 11,000 BC, possibly causing the Younger Dryas cold period
c. 10,900 BC (calibrated) or
c. 8900 BC (non-calibrated)
Younger Dryas impact event suspected at either of these dates.
c. 10,800 BC Younger Dryas cold period begins.
c. 10,000 BC
Year(s) Event(s)
Start End
c. 9700 BC
c. 9660 to 9600 BC Younger Dryas cold period ends. Pleistocene ends and Holocene begins. Large amounts of previously glaciated land become habitable again. Some sources place the Younger Dryas as stretching from 10,800 BC to 9500 BC. This cool period was possibly caused by a shutdown of the North Atlantic thermohaline circulation (Gulf Stream/Jet Stream), due to flooding from Lake Agassiz as it reformed.
c. 9564 BC Destruction of Atlantis, according to theosophic tradition.
c. 9500 BC Ancylus Lake, part of the modern-day Baltic Sea, forms. There is evidence of harvesting, though not necessarily cultivation, of wild grasses in Asia Minor about this time.
c. 9500 BC
  • End of the pre-Boreal period of European climate change.
  • Pollen Zone IV Pre-boreal, associated with juniper, willow, birch pollen deposits.
  • Neolithic era begins in Ancient Near East, first stone structures at Jericho built.
  • Temporary global chilling, as the Gulf Stream pulls southward, and Europe ices over (1990 Rand McNally Atlas).
  • In Antarctica, long-term melting of the Antarctic ice sheets is commencing.
— Antarctica — long-term melting of the Antarctic ice sheets is under way.
— Asia - rising sea levels caused by postglacial warming.
— North America - The glaciers were receding and by 8000 BCE the Wisconsin had withdrawn completely.
World - Inland flooding due to catastrophic glacier melt takes place in several regions.
— Rising sea levels form the Torres Strait, separate Australia from New Guinea.
— Increasing desiccation of the Sahara. End of the Saharan Pluvial period.
— Associated with Pollen Zone VI Atlantic, oak-elm woodlands, warmer and maritime climate. Modern wild fauna plus, increasingly, human introductions, associated with the spread of the Neolithic farming technologies.
— Rising sea levels from glacial retreat flood what will become the Irish Sea, separating the island of Ireland from the British Isles and Continental Europe.
  • ca. 30th century BC, Sumerian Cuneiform script, considered among the oldest alphabets, is created
  • 2900 BC — Floods at Shuruppak from horizon to horizon, with sediments in Southern Iraq, stretching as far north as Kish, and as far south as Uruk, associated with the return of heavy rains in Nineveh and a potential damming of the Karun River to run into the Tigris. This ends the Jemdet Nasr period and ushers in the Early Dynastic Period of Sumer cultures of the area. Possible association of this event with the Biblical deluge.
  • 2650 BC — Sumerian epic of Gilgamesh describes vast tracts of cedar forests in what is now southern Iraq. Gilgamesh defies the gods and cuts down the forest, and in return the gods say they will curse Sumer with fire (or possibly drought). By 2100 BC, soil erosion and salt buildup have devastated agriculture. One Sumerian wrote that the "earth turned white." Civilization moved north to Babylonia and Assyria. Again, deforestation becomes a factor in the rise and subsequent fall of these civilizations.
— Some of the first laws protecting the remaining forests decreed in Ur.
  • 2500 BC — Sahara becomes fully desiccated. Desiccation had been proceeding from 6000 BCE, as a result of the shift in the West African tropical monsoon belt southwards from the Sahel. Subsequent rates of evaporation in the region led to a drying of the Sahara, as shown by the drop in water levels in Lake Chad. Tehenu of the Sahara attempt to enter into Egypt, and there is evidence of a Nile drought in the pyramid of Unas.
  • 2300 BC - Neolithic period ends in China
  • 2200 BC — Beginning of a severe centennial-scale drought in northern Africa, southwestern Asia and midcontinental North America, which very likely caused the collapse of the Old Kingdom in Egypt as well as the Akkadian Empire in Mesopotamia. This is the transition from the Subboreal period to the subatlantic period.
  • 1900 BC — The Atra-Hasis Epic describes Babylonian flood, with warnings of the consequences of human overpopulation.
  • 1450 BC — Minoan civilization in the Mediterranean declines, but scholars are divided on the cause. Possibly a volcanic eruption was the source of the catastrophe (see Minoan eruption). On the other hand, gradual deforestation may have led to materials shortages in manufacturing and shipping. Loss of timber and subsequent deterioration of its land was probably a factor in the decline of Minoan power in the late Bronze Age, according to John Perlin in A Forest Journey.
  • 1206 BC - 1187 BC — Evidence of major droughts in the Eastern Mediterranean. Hittite and Ugarit records show requests for grain were sent to Egypt, probably during the reign of Pharaoh Merenptah. Carpenter has suggested that droughts of equal severity to those of the 1950s in Greece, would have been sufficient to cause the Late Bronze Age collapse. The cause may have been a temporary diversion of winter storms north of the Pyrenees and Alps. Central Europe experienced generally wetter conditions, while those in the Eastern Mediterranean were substantially drier. There seems to have been a general abandonment of peasant subsistence agriculture in favour of nomadic pastoralism in Central Anatolia, Syria and northern Mesopotamia, Palestine, the Sinai and NW Arabia.
  • c 2000 BC -1000 BC - The Sarasvati River dries up. Desertification of the Thar Region begins.
  • 800 BC - 500 BC — Sub-Atlantic period in Western Europe. Pollen Zone VIII, sub-Atlantic. End of last Sea Level rise. Spread of "Celtic fields", Iron Age A, and Haalstadt Celts. Increased prosperity in Europe and the Middle East.
  • 800 - 200 BC - Axial age, a revolution in thinking that we know as Philosophy, begins in China, India, and Europe.
  • 508 BC - Democracy created in Ancient Greece
  • c. 225 BC — The Sub-Atlantic began about 225 BCE (estimated on the basis of radiocarbon dating) and has been characterized by increased rainfall, cooler and more humid climates, and the dominance of beech forests. The fauna of the Sub-Atlantic is essentially modern although severely depleted by human activities. The Sub-Atlantic is correlated with pollen zone IX; sea levels have been generally regressive during this time interval, though North America is an exception.
  • c. 200 BC — Sri Lanka first country in the world to have a nature reserve, King Devanampiyatissa established a wildlife sanctuary

2nd century

4th century

6th century

  • 535-536: global climate abnormalities affecting several civilizations.

9th century

10th century

11th century

12th century

13th century

14th century

15th century

  • 1408 - last known recording (a wedding) of norse settlers in Greenland
  • 1453 - Eruption of Kuwae in Pacific contributes to fall of Constantinople. Environmental Science is developed.
  • 1492 - Christopher Columbus lands in Caribbean islands, starting the Columbian Exchange, causing the Aztec Empire and Inca Empire to fall to the Spanish in the next century, as well as bringing various species of animals and plants across the Atlantic Ocean.

17th century

18th century

19th century

20th century

21st century

caption
Year(s) Event
2004 Earthquake causes large tsunamis in the Indian Ocean, killing nearly a quarter of a million people.
2005 Hurricanes Katrina, Rita, and Wilma cause widespread destruction and environmental harm to coastal communities in the US Gulf Coast region, especially the New Orleans area.
2010 Earthquake in Haiti destroyed vital infrastructure.
2010 The eruption of the Eyjafjallajökull volcano affected activities in Europe and across the world.
2010 Deepwater Horizon oil spill in Gulf of Mexico.

References

  1. ^ Wilson, C. J. N. (1980). "A new date for the Taupo eruption, New Zealand". Nature. 288: 252–253. doi:10.1038/288252a0. {{cite journal}}: Cite has empty unknown parameter: |month= (help); Unknown parameter |coauthors= ignored (|author= suggested) (help)
  2. ^ Witze, Alexandra (2008-04-11). "The volcano that changed the world". Nature.Com News. Nature Publishing Group. Retrieved 2008-04-14. {{cite web}}: External link in |work= (help)
  3. ^ Richard H. Grove, “Global Impact of the 1789–93 El Niño,” Nature393 (1998), 318-319.
  4. ^ Kerry A. Odell and Marc D. Weidenmier, Real Shock, Monetary Aftershock: The 1906 San Francisco Earthquake and the Panic of 1907, The Journal of Economic History, 2005, vol. 64, issue 04, p. 1002-1027.
  5. ^ a b "United Nations Population Fund moves Day of 6 Billion based on new population estimates". Population Connection. 1998-10-28. Archived from the original on 2006-02-20. Retrieved 2006-03-11.