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Last Interglacial

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135: 4400: 239: 388:(GCM) with reconstructed Last Interglacial temperatures for Europe. Central Europe (north of the Alps) was found to be 1–2 Â°C (1.8–3.6 Â°F) warmer than present; south of the Alps, conditions were 1–2 Â°C cooler than today. The model (generated using observed greenhouse gas concentrations and Last Interglacial orbital parameters) generally reproduces these observations, leading them to conclude that these factors are enough to explain the Last Interglacial temperatures. 452: 28: 4159: 20: 440: 519: 352:, Finland. At the peak of the Last Interglacial, the Northern Hemisphere winters were generally warmer and wetter than now, though some areas were actually slightly cooler than today. A cooling event similar to but not exactly mirroring the 8.2-kiloyear event is recorded from Beckentin during the E5 phase of the Eemian, some 6,290 years after the start of interglacial afforestation. A 2018 study based on soil samples from 191:(Mediterranean faunal province). More information on the molluscan assemblages is given by LoriĂ© (1887), and Spaink (1958). Since their discovery, Last Interglacial beds in the Netherlands have mainly been recognized by their marine molluscan content combined with their stratigraphical position and other palaeontology. The marine beds there are often underlain by 727:
during this time. During the Last Interglacial, Neanderthals engaged in a variety of food-gathering activities, including fishing, as well as big-game hunting, including the largest animals living in Europe at the time, straight-tusked elephants. Modern humans were present outside Africa in Arabia during this interval, as far east as the
376:(AMOC) began to cool the eastern Mediterranean region. The period closed as temperatures steadily fell to conditions cooler and drier than the present, with a 468-year-long aridity pulse in central Europe at about 116,000 BC, and by 112,000 BC, ice caps began to form in southern Norway, marking the start of a new 364:, lasting hundreds of years and causing temperature drops of a few degrees and vegetation changes in these regions. In Northern Europe, winter temperatures rose over the course of the Last Interglacial while summer temperatures fell. During an insolation maximum from 133,000 to 130,000 BP, meltwater from the 1260:
Johnsen, SigfĂșs J.; Clausen, Henrik B.; Dansgaard, Willi; Gundestrup, Niels S.; Hammer, Claus U.; Andersen, Uffe; Andersen, Katrine K.; Hvidberg, Christine S.; Dahl-Jensen, Dorthe; Steffensen, JĂžrgen P.; Shoji, Hitoshi; SveinbjörnsdĂłttir, Árny E.; White, Jim; Jouzel, Jean; Fisher, David (30 November
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in the atmosphere was about 280 parts per million. The Last Interglacial was one of the warmest periods of the last 800,000 years, with temperatures comparable to and at times warmer (by up to on average 2 degrees Celsius) than the contemporary Holocene interglacial, with the maximum sea level being
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Barlow, Natasha L. M.; McClymont, Erin L.; Whitehouse, Pippa L.; Stokes, Chris R.; Jamieson, Stewart S. R.; Woodroffe, Sarah A.; Bentley, Michael J.; Callard, S. Louise; Ó Cofaigh, Colm; Evans, David J. A.; Horrocks, Jennifer R.; Lloyd, Jerry M.; Long, Antony J.; Margold, Martin; Roberts, David H.
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Sea level at peak was probably 6 to 9 metres (20 to 30 feet) higher than today, with Greenland contributing 0.6 to 3.5 m (2.0 to 11.5 ft), thermal expansion and mountain glaciers contributing up to 1 m (3.3 ft), and an uncertain contribution from Antarctica. A 2007 study found
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During the northern summer, temperatures in the Arctic region were about 2–4 Â°C higher than in 2011. The Arctic Last Interglacial climate was highly unstable, with pronounced temperature swings revealed by ÎŽO fluctuations in Greenlandic ice cores, though some of the instability inferred from
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managed to colonise the higher latitudes of Europe during this time interval, after having retreated from the region due to unfavourable conditions during the Penultimate Glacial Period. However, unlike previous interglacials, they were absent from Britain, likely due to Britain being an island
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Willerslev, E.; Cappellini, E.; Boomsma, W.; Nielsen, R.; Hebsgaard, M. B.; Brand, T. B.; Hofreiter, M.; Bunce, M.; Poinar, H. N.; Dahl-Jensen, D.; Johnsen, S.; Steffensen, J. P.; Bennike, O.; Schwenninger, J. -L.; Nathan, R.; Armitage, S.; De Hoog, C. -J.; Alfimov, V.; Christl, M.; Beer, J.;
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Pearce, Elena A.; Mazier, Florence; Normand, Signe; Fyfe, Ralph; Andrieu, ValĂ©rie; Bakels, Corrie; Balwierz, Zofia; BiƄka, Krzysztof; Boreham, Steve; Borisova, Olga K.; Brostrom, Anna; de Beaulieu, Jacques-Louis; Gao, Cunhai; GonzĂĄlez-SampĂ©riz, PenĂ©lope; Granoszewski, Wojciech (2023-11-10).
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Brovkin, Victor; BrĂŒcher, Tim; Kleinen, Thomas; Zaehle, Sönke; Joos, Fortunat; Roth, Raphael; Spahni, Renato; Schmitt, Jochen; Fischer, Hubertus; Leuenberger, Markus; Stone, Emma J.; Ridgwell, Andy; Chappellaz, JĂ©rĂŽme; Kehrwald, Natalie; Barbante, Carlo (1 April 2016).
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Thomas, Zoë A.; Jones, Richard T.; Turney, Chris S. M.; Golledge, Nicholas; Fogwill, Christopher; Bradshaw, Corey J. A.; Menviel, Laurie; McKay, Nicholas P.; Bird, Michael; Palmer, Jonathan; Kershaw, Peter; Wilmshurst, Janet; Muscheler, Raimund (April 2020).
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The Last Interglacial is known as the Eemian in northern Europe (sometimes used to describe the global interglacial), Ipswichian in Britain, the Mikulino (also spelled Milukin) interglacial in Russia, the Kaydaky in Ukraine, the Valdivia interglacial in
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Shackleton, S.; Baggenstos, D.; Menking, J. A.; Dyonisius, M. N.; Bereiter, B.; Bauska, T. K.; Rhodes, R. H.; Brook, E. J.; Petrenko, V. V.; McConnell, J. R.; Kellerhals, T.; HĂ€berli, M.; Schmitt, J.; Fischer, H.; Severinghaus, J. P. (2020-01-02).
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Levy, Elan J.; Vonhof, Hubert B.; Bar-Matthews, Miryam; MartĂ­nez-GarcĂ­a, Alfredo; Ayalon, Avner; Matthews, Alan; Silverman, Vered; Raveh-Rubin, Shira; Zilberman, Tami; Yasur, Gal; Schmitt, Mareike; Haug, Gerald H. (25 August 2023).
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ZilhĂŁo, J.; Angelucci, D. E.; Igreja, M. AraĂșjo; Arnold, L. J.; Badal, E.; Callapez, P.; Cardoso, J. L.; d’Errico, F.; Daura, J.; Demuro, M.; Deschamps, M.; Dupont, C.; Gabriel, S.; Hoffmann, D. L.; Legoinha, P. (2020-03-27).
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Wassenburg, Jasper A.; Vonhof, Hubert B.; Cheng, Hai; MartĂ­nez-GarcĂ­a, Alfredo; Ebner, Pia-Rebecca; Li, Xianglei; Zhang, Haiwei; Sha, Lijuan; Tian, Ye; Edwards, R. Lawrence; Fiebig, Jens; Haug, Gerald H. (18 November 2021).
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Froese, Duane; Stiller, Mathias; Heintzman, Peter D.; Reyes, Alberto V.; Zazula, Grant D.; Soares, André E. R.; Meyer, Matthias; Hall, Elizabeth; Jensen, Britta J. L.; Arnold, Lee J.; MacPhee, Ross D. E. (March 28, 2017).
480:. Recent research on marine sediment cores offshore of the West Antarctic Ice Sheet suggest that the sheet melted during the Last Interglacial, and that ocean waters rose as fast as 2.5 meters per century. Global mean 1391:
Salonen, J. Sakari; Helmens, Karin F.; Brendryen, Jo; Kuosmanen, Niina; VĂ€liranta, Minna; Goring, Simon; Korpela, Mikko; Kylander, Malin; Philip, Annemarie; Plikk, Anna; Renssen, Hans; Luoto, Miska (20 July 2018).
417:(now tundra) to have boreal forest, although inadequate precipitation caused a reduction in the forest cover in interior Alaska and Yukon Territory despite warmer conditions. The prairie-forest boundary in the 263:
The Last Interglacial climate is believed to have been warmer than the current Holocene. The temperature of the Last Interglacial peaked during the early part of the period, around 128,000 to 123,000 years
1298:"CH 4 and ÎŽ 18 O of O 2 records from Antarctic and Greenland ice: A clue for stratigraphic disturbance in the bottom part of the Greenland Ice Core Project and the Greenland Ice Sheet Project 2 ice cores" 484:
are thought to have been higher than in the Holocene, but not by enough to explain the rise in sea level through thermal expansion alone, and so melting of polar ice caps must also have occurred.
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age for late Last Interglacial deposits from this borehole of 118,200 ± 6,300 years ago. A historical review of Dutch Last Interglacial research is provided by Bosch, Cleveringa and Meijer, 2000.
1709:"Re-investigation of the Bispingen palaeolake sediment succession (northern Germany) reveals that the Last Interglacial (Eemian) in northern-central Europe lasted at least ~15 000 years" 4298: 2996:"First occurrence of <i>Panthera atrox</i> (Felidae, Pantherinae) in the Mexican state of Hidalgo and a review of the record of felids from the Pleistocene of Mexico" 697:(which is first known from the Snowmass site in Colorado, dating to around 120,000 years ago) and ultimately all North American bison species, and marking the beginning of the 1962: 830: 268:, before declining during the latter half of the period. Changes in the Earth's orbital parameters from today (greater obliquity and eccentricity, and perihelion), known as 672:
that occurred during the following Last Glacial Period, has been suggested as a "baseline" reference point for the analysis and restoration of modern European ecosystems.
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Van Leeuwen, R.J., Beets, D., Bosch, J.H.A., Burger, A.W., Cleveringa, P., van Harten, D., Herngreen, G.F.W., Langereis, C.G., Meijer, T., Pouwer, R., de Wolf, H., 2000.
2586: 2363:; Marshall, Shawn J.; Overpeck, Jonathan T.; Miller, Gifford H.; Hu, Aixue (2006). "Simulating Arctic Climate Warmth and Icefield Retreat in the Last Interglaciation". 1885:"A tentative reconstruction of the last interglacial and glacial inception in Greenland based on new gas measurements in the Greenland Ice Core Project (GRIP) ice core" 226:
glacial basin in the Amsterdam-Terminal borehole and was the subject of a multidisciplinary investigation (Van Leeuwen, et al., 2000). These authors also published a
1238: 203:. In contrast to e.g. the deposits in Denmark, the Last Interglacial deposits in the type area have never been found overlain by tills, nor in ice-pushed positions. 3035:
Roebroeks, Wil; MacDonald, Katharine; Scherjon, Fulco; Bakels, Corrie; Kindler, Lutz; Nikulina, Anastasia; Pop, Eduard; Gaudzinski-Windheuser, Sabine (2021-12-17).
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Davoli, Marco; Monsarrat, Sophie; Pedersen, Rasmus Østergaard; Scussolini, Paolo; Karger, Dirk Nikolaus; Normand, Signe; Svenning, Jens-Christian (January 2024).
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Because of the sea level drop since the Last Interglacial, exposed fossil coral reefs are common in the tropics, especially in the Caribbean and along the
2621:"A new record of Pleistocene hippopotamus from River Severn terrace deposits, Gloucester, UK—palaeoenvironmental setting and stratigraphical significance" 467:. Foreground shows corals truncated by erosion; behind the geologist is a post-erosion coral pillar which grew on the surface after sea level rose again. 1461:
Wegwerth, Antje; Dellwig, Olaf; Wulf, Sabine; Plessen, Birgit; Kleinhanns, Ilka C.; Nowaczyk, Norbert R.; Jiabo, Liu; Arz, Helge W. (1 September 2019).
4242: 4195: 3499: 122:). As the most recent point in time with a climate comparable to the Holocene, the Last Interglacial is also of relevance as a point of reference ( 691:) migrated into the heartlands of North America from Alaska at the beginning of the Last Interglacial, giving rise to the giant long-horned bison 2204:
Scherer, RP; Aldahan, A; Tulaczyk, S; Possnert, G; Engelhardt, H; Kamb, B (3 July 1998). "Pleistocene collapse of the west antarctic ice sheet".
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Cuffey, K. M.; Marshall, S. J. (2000). "Substantial contribution to sea-level rise during the last interglacial from the Greenland ice sheet".
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Sirocko, F.; Seelos, K.; Schaber, K.; Rein, B.; Dreher, F.; Diehl, M.; Lehne, R.; JĂ€ger, K.; Krbetschek, M.; Degering, D. (11 August 2005).
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Hrynowiecka, Anna; Stachowicz-Rybka, Renata; Niska, Monika; Moskal-del Hoyo, Magdalena; Börner, Andreas; Rother, Henrik (20 December 2021).
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Wilson, M. A.; Curran, H. A.; White, B. (2007). "Paleontological evidence of a brief global sea-level event during the last interglacial".
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coastlines. These reefs often contain internal erosion surfaces showing significant sea level instability during the Last Interglacial.
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Stratigraphy and integrated facies analysis of the Saalian and Eemian sediments in the Amsterdam-Terminal borehole, the Netherlands
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on which Amersfoort is located. Harting noticed the marine molluscan assemblages to be very different from the modern fauna of the
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was glaciated during the Last Interglacial, which implies that Greenland could have contributed at most 2 m (6.6 ft) to
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NoguĂ©s-Bravo, David; RodrĂ­guez, JesĂșs; Hortal, JoaquĂ­n; Batra, Persaram; AraĂșjo, Miguel B (2008-04-01). Barnosky, Anthony (ed.).
2772:"The Pleistocene easternmost distribution in Eurasia of the species associated with the Eemian Palaeoloxodon antiquus assemblage" 1302: 1267: 31: 542:
The warmness of the interval allowed temperate-adapted taxa to extend their range considerably northward, with the range of the
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Bravo-Cuevas, Victor Manuel; Priego-Vargas, Jaime; Cabral-Perdomo, Miguel Ángel; Pineda Maldonado, Marco Antonio (2016-07-20).
1263:"The ÎŽ 18 O record along the Greenland Ice Core Project deep ice core and the problem of possible Eemian climatic instability" 3492: 3460:
Vegetation, climate and radiocarbon datings in the Late Pleistocene of the Netherlands. Part 1: Eemian and Early Weichselian.
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by this time, representing the earliest split of modern human populations that persists to the present time (associated with
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up to 6 to 9 metres higher than at present, with global ice volume likely also being smaller than the Holocene interglacial.
175:. Many species from the Last Interglacial layers nowadays show a much more southern distribution, ranging from South of the 3351: 1246: 308: 218:
was re-investigated using old and new data in a multi-disciplinary approach (Cleveringa et al., 2000). At the same time a
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records may be a result of mixing of Last Interglacial ice with ice from the preceding or succeeding glacial intervals.
3259:"Beyond arrows on a map: The dynamics of Homo sapiens dispersal and occupation of Arabia during Marine Isotope Stage 5" 272:, probably led to greater seasonal temperature variations in the Northern Hemisphere. As the Last Interglacial cooled, 4181: 4119: 3406:
MĂŒller, Ulrich C.; et al. (2005). "Cyclic climate fluctuations during the last interglacial in central Europe".
2491: 1528:"Weakened AMOC related to cooling and atmospheric circulation shifts in the last interglacial Eastern Mediterranean" 709:) appeared and become widespread across North America, having descended from populations of the Eurasian cave lion ( 4283: 4109: 3812: 3485: 3339:
Archives NĂ©erlandaises Sciences Exactes et Naturelles de la SociĂ©tĂ© Hollandaise des Sciences (Harlem), 10: 443–454.
1463:"Major hydrological shifts in the Black Sea "Lake" in response to ice sheet collapses during MIS 6 (130–184 ka BP)" 1102:
Arctic Council, Impacts of a Warming Climate: Arctic Climate Impact Assessment, Cambridge U. Press, Cambridge, 2004
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Dahl-Jensen, D.; Albert, M. R.; Aldahan, A.; Azuma, N.; Balslev-Clausen, D.; Baumgartner, M.; et al. (2013).
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The warmest peak of the Last Interglacial was around 125,000 years ago, when forests reached as far north as
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Two ice core temperature records; the Last Interglacial is at a depth of about 1500–1800 meters in the lower graph
2543:"Quaternary development and evolution of the sedimentary environments in the Central Mediterranean Spanish coast" 1889: 3325:
Cleveringa, P., Meijer, T., van Leeuwen, R.J.W., de Wolf, H., Pouwer, R., Lissenberg T. and Burger, A.W., 2000.
1341:"Eemian (MIS 5e) climate oscillations based on palaeobotanical analysis from the Beckentin profile (NE Germany)" 554:
in northern England, though their range outside of southern Europe did not extend much further east of than the
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Nicholson, Samuel Luke; Hosfield, Rob; Groucutt, Huw S.; Pike, Alistair W.G.; Fleitmann, Dominik (June 2021).
3202:"Hunting and processing of straight-tusked elephants 125.000 years ago: Implications for Neanderthal behavior" 2812:"Substantial light woodland and open vegetation characterized the temperate forest biome before Homo sapiens" 3328:
The Eemian stratotype locality at Amersfoort in the central Netherlands: a re-evaluation of old and new data
898: 3540: 1756: 770: 669: 4379: 4291: 3903: 838: 380:. The Eemian lasted about 1,500 to 3,000 years longer in Southern Europe than in Northern Europe. Kaspar 436:
Interglacial conditions ended on Antarctica while the Northern Hemisphere was still experiencing warmth.
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Meltwater pulse 2B, approximately 133,000 BP, substantially weakened the Indian Summer Monsoon (ISM).
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Contributions a la géologie des Pays Bas III. Le Diluvium plus récent ou sableux et le systÚme Eémien
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caused the Black and Caspian Seas to connect. During the middle of the Last Interglacial, a weakened
111: 103: 3101: 2385: 860: 66:. It was the second-to-latest interglacial period of the current Ice Age, the most recent being the 4369: 4069: 3861: 3800: 3453:
Foraminiferen aus dem Eemien (Riss-WĂŒrm-Interglazial) in der Bohrung Amersfoort I (Locus Typicus).
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Along the Central Mediterranean Spanish coast, sea levels were comparable to those of the present.
3818: 3258: 2713:"Megafauna diversity and functional declines in Europe from the Last Interglacial to the present" 2620: 1340: 974: 829:
Shackleton, Nicholas J.; Sånchez-Goñi, Maria Fernanda; Pailler, Delphine; Lancelot, Yves (2003).
567: 558:. The temperate landscapes of Europe were inhabited by large now extinct megafauna including the 481: 402: 184: 3102:"Testing Human Presence During the Last Interglacial (MIS 5e): A Review of the British Evidence" 2542: 1660: 214:, providing a subdivision of this stage into pollen stages. At the end of the 20th century, the 4419: 4262: 4247: 3951: 3855: 3794: 3782: 3580: 2380: 855: 750: 740: 361: 227: 63: 3438:
Wetenschappelijke Mededelingen Koninklijke Nederlandse Natuurhistorische Vereniging 29, 44 pp.
2252:; Haile, J.; Taberlet, P.; Gilbert, M. T. P.; Casoli, A.; Campani, E.; Collins, M. J. (2007). 4384: 4267: 4094: 4029: 3927: 3705: 3659: 3520: 1532: 1398: 575: 531: 522:
Collage of temperate forest environments in Europe during the Eemian, with animals including
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Gaudzinski-Windheuser, Sabine; Kindler, Lutz; MacDonald, Katharine; Roebroeks, Wil (2023).
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Lauterbach, Stefan; Neumann, Frank H.; Tjallingii, Rik; Brauer, Achim (12 February 2024).
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Stage of North America, the Last Interglacial is equivalent to either all or part of it.
71: 59: 51: 3419: 3367: 3308: 3217: 3052: 2944: 2844: 2811: 2728: 2678: 2636: 2556: 2504: 2439: 2424:
Voosen, Paul (20 December 2018). "Antarctic ice melt 125,000 years ago offers warning".
2376: 2322: 2269: 2217: 2180: 2118: 2101:"Quantification of Greenland ice-sheet contribution to Last Interglacial sea-level rise" 2054: 1980: 1902: 1829: 1812:"Penultimate deglaciation Asian monsoon response to North Atlantic circulation collapse" 1769: 1678: 1614: 1572: 1545: 1527: 1480: 1411: 1354: 1195: 1129: 1038: 990: 934: 851: 791: 219: 4342: 4134: 4129: 4064: 3387: 3234: 3201: 3113: 3077: 3036: 2993: 2971: 2928: 2903: 2868: 2487:"Stratigraphy and evolution of emerged Pleistocene reefs at the Red Sea coast of Sudan" 2467: 2406: 2342: 2286: 2074: 2040: 2000: 1947: 1791: 1634: 1500: 1438: 1393: 1366: 1157: 1112:
Bova, Samantha; Rosenthal, Yair; Liu, Zhengyu; Godad, Shital P.; Yan, Mi (2021-01-28).
1058: 1023:"Lack of evidence for a substantial sea-level fluctuation within the Last Interglacial" 1002: 954: 811: 294: 115: 99: 4357: 3618: 3144: 869: 360:
identified abrupt cold spells ca. 120,000 years ago caused by shifts in the
134: 4347: 4252: 4162: 4139: 4034: 3720: 3608: 3379: 3239: 3182: 3174: 3117: 3082: 3064: 3017: 2976: 2958: 2929:"Fossil and genomic evidence constrains the timing of bison arrival in North America" 2908: 2890: 2849: 2831: 2791: 2787: 2752: 2690: 2592: 2564: 2516: 2512: 2459: 2451: 2426: 2398: 2334: 2291: 2229: 2066: 2004: 1992: 1967: 1916: 1853: 1816: 1732: 1686: 1626: 1596: 1577: 1559: 1504: 1492: 1443: 1425: 1394:"Abrupt high-latitude climate events and decoupled seasonal trends during the Eemian" 1370: 1321: 1219: 1161: 1149: 1141: 1113: 1062: 1050: 1006: 958: 946: 803: 4313: 3391: 2471: 2410: 2025:
Kopp, RE; Simons, FJ; Mitrovica, JX; Maloof, AC; Oppenheimer, M (17 December 2009).
1795: 1488: 1204: 1177: 1022: 998: 918: 4332: 4257: 3669: 3423: 3371: 3312: 3270: 3229: 3221: 3164: 3156: 3109: 3072: 3056: 3007: 2966: 2948: 2898: 2880: 2839: 2823: 2783: 2742: 2732: 2682: 2640: 2560: 2508: 2443: 2390: 2346: 2326: 2281: 2273: 2221: 2184: 2132: 2122: 2078: 2058: 2031: 1984: 1943: 1906: 1843: 1833: 1781: 1773: 1722: 1713: 1682: 1638: 1618: 1601: 1567: 1549: 1484: 1433: 1415: 1358: 1311: 1296:
Chappellaz, JérÎme; Brook, Ed; Blunier, Thomas; Malaizé, Bruno (30 November 1997).
1276: 1209: 1199: 1133: 1042: 994: 938: 865: 815: 795: 778: 745: 711: 632: 3352:"Paleoclimatic Evidence for Future Ice-Sheet Instability and Rapid Sea-Level Rise" 2995: 2447: 4352: 4327: 4008: 3977: 3909: 3891: 3649: 3628: 3550: 3535: 2885: 2644: 1597:"A late Eemian aridity pulse in central Europe during the last glacial inception" 1362: 1114:"Seasonal origin of the thermal maxima at the Holocene and the last interglacial" 715:) that had migrated into Alaska during the preceding Penultimate Glacial Period. 693: 551: 499: 456: 176: 4203: 2225: 4337: 4237: 4144: 4013: 3972: 3332:
Geologie & Mijnbouw / Netherlands Journal of Geosciences, 79(2/3): 197–216.
2662: 2254:"Ancient Biomolecules from Deep Ice Cores Reveal a Forested Southern Greenland" 2249: 1848: 1838: 1811: 1554: 1420: 1338: 1137: 676: 477: 426: 377: 265: 164: 3317: 3292: 3274: 3199: 2686: 2026: 1046: 942: 4413: 4124: 4089: 3921: 3915: 3885: 3867: 3788: 3730: 3679: 3664: 3623: 3178: 3068: 3021: 2962: 2894: 2835: 2795: 2756: 2694: 2520: 2455: 1920: 1857: 1752:"A model-data comparison of European temperatures in the Eemian interglacial" 1736: 1563: 1496: 1429: 1325: 1223: 1145: 1054: 950: 702: 698: 422: 395: 323: 310: 302: 243: 188: 119: 3375: 3160: 2953: 2394: 2277: 1988: 238: 4074: 4039: 3560: 3555: 3473:
www.foraminifera.eu Foraminifera (Microfossils) of the Eemian Interglacial
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Vegetation and paleoclimate of the last interglacial period, central Alaska
1630: 1581: 1447: 1153: 975:"Tipping elements and amplified polar warming during the Last Interglacial" 807: 728: 684: 543: 460: 418: 207: 144: 107: 3477: 3293:"The Eemian stage in the Netherlands: history, character and new research" 2233: 2127: 2027:"Probabilistic assessment of sea level during the last interglacial stage" 668:). The Last Interglacial ecosystems of Europe, which existed prior to the 4217: 4099: 4084: 4079: 3933: 3725: 3613: 3570: 2747: 2189: 2165:"The role of ocean thermal expansion in Last Interglacial sea level rise" 2164: 1911: 1884: 1777: 723: 637: 523: 495: 464: 451: 200: 160: 92: 2062: 1622: 1178:"Comparative carbon cycle dynamics of the present and last interglacial" 799: 27: 4315: 4205: 4003: 3982: 3715: 3674: 3565: 3169: 653: 211: 156: 3448:
Geologie en Mijnbouw / Netherlands Journal of Geosciences 79, 161–196.
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Hamed, Basher; Bussert, Robert; Dominik, Wilhelm (1 February 2016).
1808: 915: 771:"Eemian interglacial reconstructed from a Greenland folded ice core" 199:, and overlain by local fresh water or wind-blown deposits from the 3987: 3695: 2359: 1661:"A time dependent glaciological model of the Weichselian Ice Sheet" 615: 599: 518: 406: 337: 247: 180: 152: 67: 3145:"Last Interglacial Iberian Neandertals as fisher-hunter-gatherers" 2869:"Climate Change, Humans, and the Extinction of the Woolly Mammoth" 2246: 2045: 439: 4222: 4044: 3654: 3644: 2710: 1750:
Kaspar, F.; KĂŒhl, Norbert; Cubasch, Ulrich; Litt, Thomas (2005).
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Stone, E.J; Lundt, D.J; Annan, J.D.; Hargreaves, J.C. (2013).
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faunal age in North America. Also during this time period the
3700: 3603: 3290: 3256: 1295: 768: 555: 473: 369: 353: 341: 251: 84: 1751: 167:(1875). He named the beds "SystĂšme EĂ©mien", after the river 3710: 3141: 2925: 1174: 661: 349: 273: 192: 88: 3037:"Landscape modification by Last Interglacial Neanderthals" 2158: 1460: 58:
and ended about 115,000 years ago at the beginning of the
2541:
Viñals, María José; Fumanal, María Pilar (January 1995).
2098: 2024: 1077:
Human Mitochondrial DNA and the Evolution of Homo sapiens
971: 506:
being drowned. Vast areas of northwestern Europe and the
345: 210:
from the type site, whereas Zagwijn (1961) published the
168: 1594: 831:"Marine Isotope Substage 5e and the Eemian Interglacial" 2808: 1963:"Ice volume and sea level during the last interglacial" 242:
View of the Last Interglacial–aged coastal terraces of
143:
Picture from Pieter Harting (1886) assigned by him as '
3455:
Mededelingen Geologische Stichting NS 11(1957), 27–39.
91:. Depending on how a specific publication defines the 70:
which extends to the present day (having followed the
54:
which began about 130,000 years ago at the end of the
3100:
G. Lewis, Simon; Ashton, Nick; Jacobi, Roger (2011),
1749: 1111: 675:
In contrast, the range of cold-adapted taxa like the
74:). During the Last Interglacial, the proportion of CO 3291:
Bosch, J. H. A.; Cleveringa, P.; Meijer, T. (2000).
3099: 2591:. New York: Columbia University Press. p. 101. 919:"Global ocean heat content in the Last Interglacial" 405:: currently, the northern limit is further south at 2484: 1090:"Current & Historical Global Temperature Graph" 1933: 1236: 899:"Earth is the warmest it's been in 120,000 years" 16:Interglacial period which began 130,000 years ago 4411: 3462:Mededelingen Geologische Stichting NS 14, 15–45. 1239:"Warm past climates: is our future in the past?" 384:(GRL, 2005) performed a comparison of a coupled 151:The Last Interglacial was first recognized from 3436:De Nederlandse Eemlagen, I: Algemeen overzicht. 2933:Proceedings of the National Academy of Sciences 2660: 1658: 630:), with predators including lions (the extinct 3946:Withrow Moraine and Jameson Lake Drumlin Field 2308: 4299: 4189: 3493: 2540: 1960: 1075:M Richards et al. in: Bandelt et al. (eds.), 498:formed an island due to the area between the 102:and is of some interest for the evolution of 3402:Archives Teyler, Ser. II, Vol. III: 104–160. 3108:, vol. 14, Elsevier, pp. 125–164, 3940:Two Creeks Buried Forest State Natural Area 3507: 3350:Overpeck, Jonathan T.; et al. (2006). 2663:"The Eemian mammal fauna of central Europe" 2159:McKay, Nicholas P.; Overpeck, Jonathan T.; 1243:The National Centre for Atmospheric Science 374:Atlantic Meridional Overturning Circulation 4306: 4292: 4196: 4182: 3500: 3486: 2625:Proceedings of the Geologists' Association 472:evidence that the Greenland ice core site 3316: 3233: 3168: 3076: 3011: 2970: 2952: 2902: 2884: 2843: 2746: 2736: 2384: 2285: 2188: 2138:1983/d05aa57e-0230-4287-94e8-242d43abee77 2136: 2126: 2044: 1910: 1847: 1837: 1785: 1726: 1571: 1553: 1437: 1419: 1315: 1280: 1213: 1203: 859: 3349: 2769: 517: 450: 237: 133: 87:, and the Riss-WĂŒrm interglacial in the 26: 18: 2618: 2584: 1882: 1303:Journal of Geophysical Research: Oceans 1268:Journal of Geophysical Research: Oceans 896: 598:), alongside still-living species like 429:, whereas the current boundary is near 4412: 3874:Ice Age Floods National Geologic Trail 3838:Chippewa Moraine State Recreation Area 3405: 3263:Journal of Anthropological Archaeology 2706: 2704: 2423: 2248:Muscheler, R.; Barker, J.; Sharp, M.; 1961:Dutton, A; Lambeck, K (13 July 2012). 1883:Landais, Amaelle (16 September 2003). 258: 4287: 4177: 3481: 2656: 2654: 2619:Schreve, Danielle C. (January 2009). 206:Van Voorthuysen (1958) described the 195:that are considered to date from the 2661:van Kolfschoten, Th. (August 2000). 2530:– via Elsevier Science Direct. 1380:– via Elsevier Science Direct. 718: 670:global wave of megafauna extinctions 550:) notably extending as far north as 394:Trees grew as far north as southern 3880:Ice Age National Scientific Reserve 3193: 3106:Developments in Quaternary Sciences 2763: 2701: 187:faunal province) and even into the 13: 3297:Netherlands Journal of Geosciences 3284: 3114:10.1016/b978-0-444-53597-9.00009-1 2667:Netherlands Journal of Geosciences 2651: 2588:Rising Seas: Past, Present, Future 1948:10.1111/j.1502-3931.1998.tb00513.x 1659:Holmlund, P.; Fastook, J. (1995). 438: 14: 4441: 4314:The cold and warm periods of the 4204:The cold and warm periods of the 3868:Horicon Marsh State Wildlife Area 3466: 2492:Journal of African Earth Sciences 4398: 4158: 4157: 3813:Origin of the Oak Ridges Moraine 2788:10.1111/j.1365-2907.2007.00109.x 2513:10.1016/j.jafrearsci.2015.11.011 897:Kaufman, Mark (27 August 2018). 3346:Album der Natuur, 1886: 95–100. 3250: 3135: 3093: 3028: 2987: 2919: 2860: 2802: 2717:Global Ecology and Biogeography 2612: 2578: 2534: 2478: 2417: 2353: 2302: 2240: 2197: 2152: 2092: 2018: 1954: 1927: 1890:Journal of Geophysical Research 1876: 1864: 1802: 1743: 1700: 1652: 1588: 1518: 1489:10.1016/j.quascirev.2019.07.008 1454: 1384: 1332: 1289: 1253: 1230: 1205:10.1016/j.quascirev.2016.01.028 1168: 1105: 999:10.1016/j.quascirev.2020.106222 3876:, Idaho, Oregon and Washington 1787:11858/00-001M-0000-0011-FED3-9 1215:11858/00-001M-0000-0027-AE16-0 1096: 1082: 1069: 1013: 965: 909: 890: 822: 762: 1: 4120:Huelmo–Mascardi Cold Reversal 3451:Van Voorthuysen, J.H., 1958. 2770:Pushkina, Diana (July 2007). 2448:10.1126/science.362.6421.1339 870:10.1016/S0921-8181(02)00181-9 756: 580:Stephanorhinus kirchbergensis 129: 3541:Glacial history of Minnesota 3344:Het Eemdal en het Eemstelsel 2886:10.1371/journal.pbio.0060079 2645:10.1016/j.pgeola.2009.03.003 2565:10.1016/1040-6182(95)00014-A 2169:Geophysical Research Letters 1757:Geophysical Research Letters 1687:10.1016/1040-6182(94)00060-I 1363:10.1016/j.quaint.2021.01.025 446: 147:' for the Last Interglacial. 38:over the last 400,000 years. 7: 3904:Kettle Moraine State Forest 3807:Lion's Head Provincial Park 2226:10.1126/science.281.5373.82 839:Global and Planetary Change 734: 155:in the area of the city of 126:) for nature conservation. 120:mitochondrial haplogroup L0 10: 4446: 4050:Penultimate Glacial Period 3777:Big Rock (glacial erratic) 1839:10.1038/s41561-021-00851-9 1555:10.1038/s41467-023-40880-z 1468:Quaternary Science Reviews 1421:10.1038/s41467-018-05314-1 1237:Nathaelle Bouttes (2011). 1183:Quaternary Science Reviews 1138:10.1038/s41586-020-03155-x 1079:, Springer (2006), p. 233. 979:Quaternary Science Reviews 572:Stephanorhinus hemitoechus 459:in a fossil coral reef on 288:Greenland ice core project 233: 104:anatomically modern humans 98:The period falls into the 56:Penultimate Glacial Period 4396: 4323: 4213: 4153: 4115:Late Glacial Interstadial 4022: 3996: 3965: 3894:, Minnesota and Wisconsin 3828: 3771:Arrowhead Provincial Park 3763: 3747: 3688: 3637: 3596: 3589: 3546:List of prehistoric lakes 3513: 3318:10.1017/S0016774600021673 3275:10.1016/j.jaa.2021.101269 2687:10.1017/s0016774600021752 1047:10.1038/s41561-018-0195-4 943:10.1038/s41561-019-0498-0 536:straight-tusked elephants 386:general circulation model 112:Skhul and Qafzeh hominins 4070:Holocene glacial retreat 3862:Glacial Lakes State Park 3801:Foothills Erratics Train 2585:Gornitz, Vivien (2013). 2548:Quaternary International 1666:Quaternary International 1346:Quaternary International 560:straight-tusked elephant 513: 482:sea surface temperatures 4110:BĂžlling–AllerĂžd warming 3850:Devil's Lake State Park 3819:Ovayok Territorial Park 3508:Continental glaciations 3376:10.1126/science.1115159 3161:10.1126/science.aaz7943 2954:10.1073/pnas.1620754114 2395:10.1126/science.1120808 2278:10.1126/science.1141758 2161:Otto-Bliesner, Bette L. 1989:10.1126/science.1205749 568:narrow-nosed rhinoceros 64:Marine Isotope Stage 5e 3952:Yosemite National Park 3856:Glacial Lake Wisconsin 3795:Eskers Provincial Park 3783:Cypress Hills (Canada) 3581:Timeline of glaciation 3226:10.1126/sciadv.add8186 3061:10.1126/sciadv.abj5567 3013:10.5194/fr-19-131-2016 2828:10.1126/sciadv.adi9135 751:Timeline of glaciation 741:Marine Isotope Stage 5 564:Palaeoloxodon antiquus 548:Hippopotamus amphibius 539: 468: 443: 425:lay further west near 362:North Atlantic Current 255: 148: 106:, who were present in 39: 24: 4095:Quaternary glaciation 4030:Quaternary glaciation 3928:Mill Bluff State Park 3892:Interstate State Park 3706:Giant current ripples 3521:Cordilleran ice sheet 3458:Zagwijn, W.H., 1961. 2128:10.5194/cp-9-621-2013 1533:Nature Communications 1399:Nature Communications 681:Mammuthus primigenius 588:Megaloceros giganteus 521: 454: 442: 415:Saint Lawrence Island 348:grew as far north as 324:71.17250°N 25.79444°E 241: 137: 30: 22: 4318:in the Alpine region 4105:Wisconsin glaciation 4060:Last Glacial Maximum 3576:Post-glacial rebound 3531:Last Glacial Maximum 3526:Laurentide ice sheet 2361:Otto-Bliesner, B. L. 2190:10.1029/2011GL048280 1912:10.1029/2002JD003147 1778:10.1029/2005GL022456 1310:(C12): 26547–26557. 1275:(C12): 26397–26410. 222:was selected in the 62:. It corresponds to 46:, also known as the 4090:Pre-Illinoian Stage 4055:Last Glacial Period 3844:Coteau des Prairies 3755:Greenland ice sheet 3420:2005Geo....33..449M 3368:2006Sci...311.1747O 3362:(5768): 1747–1750. 3342:Harting, P., 1886. 3335:Harting, P., 1875. 3309:2000NJGeo..79..135B 3218:2023SciA....9D8186G 3053:2021SciA....7.5567R 2945:2017PNAS..114.3457F 2729:2024GloEB..33...34D 2679:2000NJGeo..79..269V 2637:2009PrGA..120...58S 2557:1995QuInt..29..119V 2505:2016JAfES.114..133H 2440:2018Sci...362.1339V 2377:2006Sci...311.1751O 2323:2000Natur.404..591C 2270:2007Sci...317..111W 2218:1998Sci...281...82S 2181:2011GeoRL..3814605M 2119:2013CliPa...9..621S 2106:Climate of the Past 2063:10.1038/nature08686 2055:2009Natur.462..863K 1981:2012Sci...337..216D 1903:2003JGRD..108.4563L 1849:20.500.11850/519155 1830:2021NatGe..14..937W 1770:2005GeoRL..3211703K 1679:1995QuInt..27...53H 1623:10.1038/nature03905 1615:2005Natur.436..833S 1546:2023NatCo..14.5180L 1481:2019QSRv..219..126W 1412:2018NatCo...9.2851S 1355:2021QuInt.605...38H 1196:2016QSRv..137...15B 1130:2021Natur.589..548B 1039:2018NatGe..11..627B 991:2020QSRv..23306222T 935:2020NatGe..13...77S 852:2003GPC....36..151S 800:10.1038/nature11789 792:2013Natur.493..489N 620:Capreolus capreolus 508:West Siberian Plain 320: /  270:Milankovitch cycles 259:Global temperatures 140:Bittium reticulatum 72:last glacial period 60:Last Glacial Period 52:interglacial period 4135:4.2 kiloyear event 4130:8.2 kiloyear event 4065:Mousterian Pluvial 3797:, British Columbia 3434:Spaink, G., 1958. 2551:. 29–30: 119–128. 1349:. 605–606: 38–54. 1249:on 13 August 2018. 1021:(September 2018). 683:) contracted. The 576:Merck's rhinoceros 540: 532:Merck's rhinoceros 469: 455:Last Interglacial 444: 403:Arctic Archipelago 329:71.17250; 25.79444 295:North Cape, Norway 256: 149: 100:Middle Paleolithic 40: 25: 4407: 4406: 4390:Last Interglacial 4281: 4280: 4273:Last Interglacial 4171: 4170: 4140:Piora Oscillation 4100:Sangamonian Stage 3961: 3960: 3743: 3742: 3739: 3738: 3398:LoriĂ©, J., 1887. 3337:Le systĂšme Éemien 3123:978-0-444-53597-9 2939:(13): 3457–3462. 2738:10.1111/geb.13778 2598:978-0-231-14739-2 2250:Penkman, K. E. H. 1817:Nature Geoscience 1728:10.1111/bor.12649 1317:10.1029/97JC00164 1282:10.1029/97JC00167 1124:(7843): 548–553. 1027:Nature Geoscience 923:Nature Geoscience 786:(7433): 489–494. 719:Paleoanthropology 301:) well above the 282:remained stable. 44:Last Interglacial 4437: 4425:Paleoclimatology 4402: 4308: 4301: 4294: 4285: 4284: 4208:in North Germany 4198: 4191: 4184: 4175: 4174: 4161: 4160: 3761: 3760: 3686: 3685: 3670:Terminal moraine 3594: 3593: 3502: 3495: 3488: 3479: 3478: 3431: 3428:10.1130/G21321.1 3395: 3322: 3320: 3303:(2/3): 135–145. 3279: 3278: 3254: 3248: 3247: 3237: 3206:Science Advances 3197: 3191: 3190: 3172: 3139: 3133: 3132: 3131: 3130: 3097: 3091: 3090: 3080: 3047:(51): eabj5567. 3041:Science Advances 3032: 3026: 3025: 3015: 2991: 2985: 2984: 2974: 2956: 2923: 2917: 2916: 2906: 2888: 2864: 2858: 2857: 2847: 2822:(45): eadi9135. 2816:Science Advances 2806: 2800: 2799: 2767: 2761: 2760: 2750: 2740: 2708: 2699: 2698: 2673:(2–3): 269–281. 2658: 2649: 2648: 2616: 2610: 2609: 2607: 2605: 2582: 2576: 2575: 2573: 2571: 2538: 2532: 2531: 2529: 2527: 2482: 2476: 2475: 2421: 2415: 2414: 2388: 2371:(5768): 1751–3. 2357: 2351: 2350: 2331:10.1038/35007053 2306: 2300: 2299: 2289: 2244: 2238: 2237: 2201: 2195: 2194: 2192: 2156: 2150: 2149: 2147: 2145: 2140: 2130: 2096: 2090: 2089: 2087: 2085: 2048: 2022: 2016: 2015: 2013: 2011: 1958: 1952: 1951: 1931: 1925: 1924: 1914: 1880: 1874: 1868: 1862: 1861: 1851: 1841: 1806: 1800: 1799: 1789: 1747: 1741: 1740: 1730: 1704: 1698: 1697: 1695: 1693: 1656: 1650: 1649: 1647: 1645: 1592: 1586: 1585: 1575: 1557: 1522: 1516: 1515: 1513: 1511: 1458: 1452: 1451: 1441: 1423: 1388: 1382: 1381: 1379: 1377: 1336: 1330: 1329: 1319: 1293: 1287: 1286: 1284: 1257: 1251: 1250: 1245:. Archived from 1234: 1228: 1227: 1217: 1207: 1172: 1166: 1165: 1109: 1103: 1100: 1094: 1093: 1086: 1080: 1073: 1067: 1066: 1017: 1011: 1010: 969: 963: 962: 913: 907: 906: 894: 888: 887: 885: 884: 878: 872:. Archived from 863: 835: 826: 820: 819: 775: 766: 746:Paleoclimatology 712:Panthera spelaea 633:Panthera spelaea 510:were inundated. 335: 334: 332: 331: 330: 325: 321: 318: 317: 316: 313: 114:) as well as in 4445: 4444: 4440: 4439: 4438: 4436: 4435: 4434: 4410: 4409: 4408: 4403: 4394: 4319: 4312: 4282: 4277: 4209: 4202: 4172: 4167: 4149: 4035:Illinoian Stage 4018: 4009:Lambert Glacier 3992: 3978:Killary Harbour 3957: 3910:Lake Bonneville 3830: 3824: 3759: 3735: 3684: 3633: 3629:U-shaped valley 3619:Roche moutonnĂ©e 3585: 3551:Proglacial lake 3536:Canadian Shield 3509: 3506: 3469: 3287: 3285:Further reading 3282: 3255: 3251: 3212:(5): eadd8186. 3198: 3194: 3140: 3136: 3128: 3126: 3124: 3098: 3094: 3033: 3029: 2992: 2988: 2924: 2920: 2865: 2861: 2807: 2803: 2768: 2764: 2709: 2702: 2659: 2652: 2617: 2613: 2603: 2601: 2599: 2583: 2579: 2569: 2567: 2539: 2535: 2525: 2523: 2483: 2479: 2422: 2418: 2386:10.1.1.728.3807 2358: 2354: 2317:(6778): 591–4. 2307: 2303: 2264:(5834): 111–4. 2245: 2241: 2202: 2198: 2157: 2153: 2143: 2141: 2097: 2093: 2083: 2081: 2039:(7275): 863–7. 2023: 2019: 2009: 2007: 1975:(6091): 216–9. 1959: 1955: 1932: 1928: 1881: 1877: 1869: 1865: 1824:(12): 937–941. 1807: 1803: 1748: 1744: 1705: 1701: 1691: 1689: 1657: 1653: 1643: 1641: 1609:(7052): 833–6. 1593: 1589: 1523: 1519: 1509: 1507: 1459: 1455: 1389: 1385: 1375: 1373: 1337: 1333: 1294: 1290: 1258: 1254: 1235: 1231: 1173: 1169: 1110: 1106: 1101: 1097: 1088: 1087: 1083: 1074: 1070: 1018: 1014: 970: 966: 914: 910: 895: 891: 882: 880: 876: 861:10.1.1.470.1677 833: 827: 823: 773: 767: 763: 759: 737: 721: 694:Bison latifrons 596:Bos primigenius 552:North Yorkshire 516: 500:Gulf of Finland 457:erosion surface 449: 328: 326: 322: 319: 314: 311: 309: 307: 306: 280: 261: 236: 177:Strait of Dover 132: 116:Southern Africa 77: 35: 17: 12: 11: 5: 4443: 4433: 4432: 4427: 4422: 4405: 4404: 4397: 4395: 4393: 4392: 4387: 4382: 4380:Haslach/Mindel 4377: 4372: 4367: 4361: 4360: 4355: 4350: 4345: 4340: 4335: 4330: 4324: 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3672: 3667: 3662: 3657: 3652: 3647: 3641: 3639: 3635: 3634: 3632: 3631: 3626: 3621: 3616: 3611: 3609:Glacial striae 3606: 3600: 3598: 3591: 3587: 3586: 3584: 3583: 3578: 3573: 3568: 3563: 3558: 3553: 3548: 3543: 3538: 3533: 3528: 3523: 3517: 3515: 3511: 3510: 3505: 3504: 3497: 3490: 3482: 3476: 3475: 3468: 3467:External links 3465: 3464: 3463: 3456: 3449: 3439: 3432: 3414:(6): 449–452. 3403: 3396: 3347: 3340: 3333: 3323: 3286: 3283: 3281: 3280: 3249: 3192: 3134: 3122: 3092: 3027: 3006:(2): 131–141. 2986: 2918: 2859: 2801: 2782:(3): 224–245. 2762: 2700: 2650: 2611: 2597: 2577: 2533: 2477: 2434:(6421): 1339. 2416: 2352: 2301: 2239: 2212:(5373): 82–5. 2196: 2151: 2113:(2): 621–639. 2091: 2017: 1953: 1942:(3): 241–250. 1926: 1875: 1863: 1801: 1764:(11): L11703. 1742: 1721:(2): 243–261. 1699: 1651: 1587: 1517: 1453: 1383: 1331: 1288: 1252: 1229: 1167: 1104: 1095: 1081: 1068: 1033:(9): 627–634. 1012: 964: 908: 889: 846:(3): 151–155. 821: 760: 758: 755: 754: 753: 748: 743: 736: 733: 720: 717: 707:Panthera atrox 677:woolly mammoth 604:Cervus elaphus 515: 512: 478:sea level rise 448: 445: 427:Lubbock, Texas 378:glacial period 340:trees such as 297:(which is now 278: 266:Before Present 260: 257: 235: 232: 220:parastratotype 165:Pieter Harting 131: 128: 75: 36:concentrations 33: 15: 9: 6: 4: 3: 2: 4442: 4431: 4428: 4426: 4423: 4421: 4420:Interglacials 4418: 4417: 4415: 4401: 4391: 4388: 4386: 4383: 4381: 4378: 4376: 4373: 4371: 4368: 4366: 4363: 4362: 4359: 4356: 4354: 4351: 4349: 4346: 4344: 4341: 4339: 4336: 4334: 4331: 4329: 4326: 4325: 4322: 4317: 4309: 4304: 4302: 4297: 4295: 4290: 4289: 4286: 4274: 4271: 4269: 4266: 4264: 4261: 4259: 4256: 4254: 4251: 4249: 4246: 4244: 4241: 4239: 4236: 4234: 4231: 4229: 4226: 4224: 4221: 4219: 4216: 4215: 4212: 4207: 4199: 4194: 4192: 4187: 4185: 4180: 4179: 4176: 4164: 4156: 4155: 4152: 4146: 4143: 4141: 4138: 4136: 4133: 4131: 4128: 4126: 4125:Younger Dryas 4123: 4121: 4118: 4116: 4113: 4111: 4108: 4106: 4103: 4101: 4098: 4096: 4093: 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Index



CO2 concentrations
interglacial period
Penultimate Glacial Period
Last Glacial Period
Marine Isotope Stage 5e
Holocene
last glacial period
Chile
Alps
Sangamonian
Middle Paleolithic
anatomically modern humans
Western Asia
Skhul and Qafzeh hominins
Southern Africa
mitochondrial haplogroup L0
baseline

Bittium reticulatum
Index fossil
boreholes
Amersfoort
Netherlands
Pieter Harting
Eem
North Sea
Strait of Dover
Portugal

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