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is reviewed and it is maintained that the event was a factor in the 8200 BP cooling event, as well as in changes in ocean current patterns and their resultant effects. The EHSLR may also have enhanced volcanic activity, but no clear evidence of a causal link with submarine sliding on continental slopes and shelves can yet be demonstrated. The rise probably influenced rates and patterns of human migrations and cultural changes.
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The rise, of ca 60m, took place over most of the Earth as the volume of the oceans increased during deglaciation and is dated at 11,650–7000 cal. BP. The EHSLR was largely driven by meltwater release from decaying ice masses and the break up of coastal ice streams. The impact of the EHSLR on climate
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ice sheets. At the onset of deglaciation about 19,000 years ago, a brief, at most 500-year long, glacio-eustatic event may have contributed as much as 10 m (33 ft) to sea level with an average rate of about 20 mm (0.8 in)/yr. During the rest of the early
Holocene, the rate of
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events clearly implicate major ice-loss events related to ice sheet collapse. The primary source may have been meltwater from the
Antarctic ice sheet. Other studies suggest a Northern Hemisphere source for the meltwater in the Laurentide Ice Sheet.
78:, between about 20,000 to 7,000 years ago (20–7 ka), the sea level rose by a total of about 100 m (328 ft), at times at extremely high rates, due to the rapid melting of the
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sea level rise varied from a low of about 6.0–9.9 mm (0.2–0.4 in)/yr to as high as 30–60 mm (1.2–2.4 in)/yr during brief periods of accelerated sea level rise.
431:
289:
Turney, Chris S.M.; Brown, Heidi (September 2007). "Catastrophic early
Holocene sea level rise, human migration and the Neolithic transition in Europe".
407:
Blanchon, P.; Shaw, J. (1995). "Reef drowning during the last deglaciation: evidence for catastrophic sea-level rise and icesheet collapse".
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between c. 11.4–11.1 ka, a 7.5 m (25 ft) rise over about 160 years centered at 11.1 ka, which includes the end of
427:
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Törnqvist, Torbjörn E.; et al. (2012), "Links between Early
Holocene Ice-Sheet Decay, Sea-Level Rise and Abrupt Climate Change",
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There is a hypothesis that the EHSLR left some traces in the mythology like flood myths and oral history of
Australian Aborigines.
122:, lasted between c. 14.6–14.3 ka and was a 13.5 m (44 ft) rise over about 290 years centered at 14.2 ka.
388:
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Cronin, T.M.; et al. (October 2007), "Rapid Sea Level Rise and Ice Sheet
Response to 8,200-Year Climate Event",
59:(8,200 years ago), and the loss of coastal land favoured by early farmers, may have contributed to the spread of the
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European coastline: modern (left), during the early
Holocene (center) and during the Last Glacial Maximum (right).
571:
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Smith, D.E.; Harrison, S.; Firth, C.R.; Jordan, J.T. (July 2011). "The early
Holocene sea level rise".
91:
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Hori, Kazuaki; et al. (September 2007), "An Early
Holocene Sea-Level Jump and Delta Initiation",
210: – Time period c. 12,900–11,700 years ago with Northern Hemisphere glacial cooling and SH warming
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interval of reduced sea level rise at about 6.0–9.9 mm (0.2–0.4 in)/yr;
519:"Tempo of Global Deglaciation during the Early Holocene: A Sea Level Perspective"
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The EHSLR spans
Meltwater pulses 1B and 1C, between 12,000 and 7,000 years ago:
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228: – Neolithic culture in upper Mesopotamia and the Levant c. 8800–6500 BC
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428:"Ancient Aboriginal stories preserve history of a rise in sea level"
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Encyclopedia of Modern Coral Reefs: Structure, form and process
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Encyclopedia of Modern Coral Reefs: Structure, form and process
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Blanchon, P. (2011). "Meltwater Pulses". In Hopley, D. (ed.).
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Cronin, T. M. (2012). "Invited review: Rapid sea-level rise".
177: – Series of alternating glacial and interglacial periods
358:. Earth Science Series. Springer-Verlag. pp. 683–690.
147:, a rise of 6.5 m (21 ft) in less than 140 years.
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Blanchon, P. (2011). "Backstepping". In Hopley, D. (ed.).
383:. Earth Science Series. Springer-Verlag. pp. 77–84.
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Pages displaying short descriptions of redirect targets
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43:by about 60 m (197 ft) during the early
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426:Reid, Nick; Nunn, Patrick D. (12 January 2015).
23:Sea level change since the Last Glacial Maximum.
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39:(EHSLR) was a significant jump in
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338:10.1016/j.quascirev.2012.08.021
311:10.1016/j.quascirev.2007.07.003
272:10.1016/j.quascirev.2011.04.019
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139:Meltwater pulse 1C between c.
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37:early Holocene sea level rise
480:Geophysical Research Letters
452:Geophysical Research Letters
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326:Quaternary Science Reviews
291:Quaternary Science Reviews
252:Quaternary Science Reviews
196:Holocene climatic optimum
190:Holocene glacial retreat
226:Pre-Pottery Neolithic B
220:Pre-Pottery Neolithic A
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297:(17–18): 2036–2041.
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175:Next Glacial Maximum
169:Last Glacial Maximum
76:Last Glacial Maximum
65:its Neolithic period
61:Neolithic Revolution
57:8.2 ka cooling event
572:Last Glacial Period
492:2007GeoRL..3418401H
303:2007QSRv...26.2036T
264:2011QSRv...30.1846S
202:8.2-kiloyear event
130:Meltwater pulse 1B
120:Meltwater pulse 1A
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509:Nature Geoscience
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365:978-90-481-2638-5
102:and parts of the
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145:8.0 ka
112:coral reefs
577:Mesolithic
556:Categories
543:1885/23325
526:PAGES News
233:References
214:Doggerland
96:Patagonian
88:Laurentide
74:since the
49:Mesolithic
582:Neolithic
562:Sea level
470:1912/3348
332:: 11–30.
238:Citations
153:meltwater
104:Antarctic
100:Innuitian
41:sea level
567:Holocene
432:Archived
163:See also
45:Holocene
488:Bibcode
409:Geology
299:Bibcode
260:Bibcode
70:During
486:(18),
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