- Holocene
The Holocene is a
geological epoch which began approximately 10,000 years ago (about 8000 BC). According to traditional geological thinking, the Holocene continues to the present. The Holocene is part of theNeogene andQuaternary periods. Its name comes from the Greek words polytonic|ὅλος ("holos", whole or entire) and polytonic|καινός ("kainos", new), meaning "entirely recent". It has been identified with MIS 1 and can be considered aninterglacial in the currentice age .Overview
It is generally accepted that the Holocene started approximately 10 ka (thousand years)
Before Present . The period follows the Weichsel glacial. The Holocene can be subdivided into five chronozones based on climatic fluctuations:
*Preboreal (10 ka – 9 ka),
*Boreal (9 ka – 8 ka),
*Atlantic (8 ka – 5 ka),
*Subboreal (5 ka – 2.5 ka) and
*Subatlantic (2.5 ka – present).Human civilization dates almost entirely within the Holocene. The
Blytt-Sernander classification of climatic periods defined, initially, by plant remains in peat mosses, is now of purely historical interest. The scheme was defined for north Europe, but the climate changes have been claimed to occur more widely. The periods of the scheme include a few of the final, pre-Holocene, oscillations of the last glacial period and then classify climates of more recent prehistory.Paleontologists have defined no
faunal stage s for Holocene. If subdivision is necessary, periods of human technological development such as theMesolithic ,Neolithic , andBronze Age are usually used. However, the time periods referenced by these terms vary with the emergence of those technologies in different parts of the world.Climatically, the Holocene may be divided evenly into the Hypsithermal and Neoglacial periods; the boundary coincides with the start of the Bronze Age in western civilization. According to some scholars, a third division, the
Anthropocene , began in the 18th Century [Fred Pearce (2007). "With Speed and Violence". Page 21. ISBN 978-0-8070-8576-9] . It is debatable whether this is an age within, or follows, the Holoceneepoch . Fact|date=May 2007Geology
Continental motions are less than a kilometre over a span of only 10 ka. However, ice melt caused world sea levels to rise about 35 m (110 ft) in the early part of the Holocene. In addition, many areas above about 40 degrees north latitude had been depressed by the weight of the Pleistocene glaciers and rose as much as 180 m (600 ft) over the late Pleistocene and Holocene, and are still rising today.
The sea level rise and temporary land depression allowed temporary marine incursions into areas that are now far from the sea. Holocene marine fossils are known from
Vermont ,Quebec ,Ontario , andMichigan . Other than higher latitude temporary marine incursions associated with glacial depression, Holocene fossils are found primarily in lakebed, floodplain, and cave deposits. Holocene marine deposits along low-latitude coastlines are rare because the rise in sea levels during the period exceeds any likely upthrusting of non-glacial origin.Post-glacial rebound in theScandinavia region resulted in the formation of theBaltic Sea . The region continues to rise, still causing weakearthquake s acrossNorthern Europe . The equivalent event in North America was the rebound ofHudson Bay , as it shrank from its larger, immediate post-glacialTyrrell Sea phase, to near its present boundaries.Climate
Although geographic shifts in the Holocene were minor, climatic shifts were very large.
Ice core records show that before the Holocene there were global warming and cooling periods, but climate changes became more regional at the start of theYounger Dryas . However, theHuelmo/Mascardi Cold Reversal in the Southern Hemisphere began before the Younger Dryas, and the maximum warmth flowed south to north from 11,000 to 7,000 years ago. It appears that this was influenced by the residual glacial ice remaining in theNorthern Hemisphere until the latter date.The hypsithermal was a period of warming in which the global climate became 0.5–2°C warmer than today. However, the warming was probably not uniform across the world. This period ended about 5,500 years ago, when the earliest human civilizations in
Asia andAfrica were flourishing. This period of warmth ended with the descent into theNeoglacial . At that time, the climate was not unlike today's, but there was a slightly warmer period from the 10th–14th centuries known as theMedieval Warm Period . This was followed by theLittle Ice Age , from the 13th or 14th century to the mid 19th century, which was a period of significant cooling, though not everywhere as severe as previous times during neoglaciation.The Holocene warming is an interglacial period and there is no reason to believe that it represents a permanent end to the current ice age. However, the current
global warming may result in the Earth becoming warmer than theEemian Interglacial , which peaked at roughly 125,000 years ago and was warmer than the Holocene. This prediction is sometimes referred to as a "super-interglacial".Compared to glacial conditions, habitable zones have expanded northwards, reaching their northernmost point during the hypsithermal. Greater moisture in the polar regions has caused the disappearance of
steppe-tundra .Ecological developments
Animal and plant life have not evolved much during the relatively short Holocene, but there have been major shifts in the distributions of plants and animals. A number of large animals including
mammoth s andmastodon s,saber-toothed cat s like "Smilodon " and "Homotherium ", andgiant sloth s disappeared in the late Pleistocene and early Holocene—especially in North America, where animals that survived elsewhere (including horses and camels) became extinct. This extinction of Americanmegafauna has been explained as caused by the arrival of the ancestors ofAmerindian s; though most scholars assert that climatic change also contributed.Throughout the world, ecosystems in cooler climates that were previously regional have been isolated in higher altitude ecological "islands."
The "
8.2 ka event ", an abrupt cold spell recorded as a negative excursion in the delta|18|O|link record lasting 400 years, is the most prominent climatic event occurring in the Holocene epoch, and may have marked a resurgence of ice cover. It is thought that this event was caused by the final drainage ofLake Agassiz which had been confined by the glaciers, disrupting thethermohaline circulation of the Atlantic [http://www.eos.ubc.ca/research/glaciology/research/Publications/ClarkeLeveringtonTellerDyke(QSR-2004).pdf] .Human developments
The beginning of the Holocene corresponds with the beginning of the
Mesolithic age in most of Europe; but in regions such as theMiddle East andAnatolia with a very earlyneolithisation ,Epipaleolithic is preferred in place of Mesolithic. Cultures in this period include:Hamburgian ,Federmesser , and theNatufian culture .Both are followed by the aceramic Neolithic (
Pre-Pottery Neolithic A andPre-Pottery Neolithic B ) and the potteryNeolithic .Impact events
Within the Holocene numerous
meteorite events have been recently discovered in Europe, as well as in seas such as theIndian Ocean and near remoteSiberia . It has been speculated that an impact effect such as that represented today by theBurckle crater [ cite web | url=http://www.signonsandiego.com/uniontrib/20061114/news_1n14meteors.html | title=Meteor 'misfits' find proof in sea | accessdate=2006-11-14 ] or theChiemgau Impact crater [ cite web | url=http://www.chiemgau-impact.com/reply.html | title=The Holocene Tüttensee meteorite impact crater in southeast Germany | accessdate=2006-11-21 ] could have dramatically affected human culture in its early history by the creation ofmegatsunami s, perhaps inspiring deluge or inundation stories such as that ofNoah's Flood . A washout effect from such waves may have breached land bridges with sudden massive erosion, along with violent weather changesClarifyme|date=March 2008. Competing reasons for the various basin floods also include climate change and earthquake fault lines weakening the barriers to ocean encroachmentClarifyme|date=March 2008.Further reading
*Neil Roberts "The Holocene: an environmental history" (Blackwell Publishing)
*Mackay, A.W., Battarbee, R.W., Birks, H.J.B. & Oldfield, F. (2003) Editors. "Global change in the Holocene". Publisher: Arnold, London. 528 pp (29 chapters)ee also
*
8.2 kiloyear event
*Blytt-Sernander
*Deluge (prehistoric)
*Geologic timescale
*Holocene calendar
*Holocene extinction event
*Holocene Impact Working Group
*Impact events
*Neolithic Subpluvial
*Older Peron
*Piora Oscillation
*10th millennium BC
*Last Glacial Maximum
*1 E11 s References
* Ogg, Jim; June, 2004, "Overview of Global Boundary Stratotype Sections and Points (GSSP's)" http://www.stratigraphy.org/gssp.htm Accessed April 30, 2006
External links
* http://extinctanimals.petermaas.nl/
* [http://www.geos.ed.ac.uk/homes/s9741828/8.2ka.html The 8.2 ka event]
* [http://www.pnas.org/cgi/content/full/97/4/1343 Detecting Holocene changes in thermohaline circulation]
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