New data on changes in the European distribution of the mammoth and the woolly rhinoceros during the second half of the Late Pleistocene and the early Holocene

Маркова, А.К.; Puzachenko, A. Yu.; Kolfschoten, Thijs van; Plicht, van der Johannes; Пономарев, Д. В.

doi:10.1016/j.quaint.2012.11.033

Cited by 44 publications

(28 citation statements)

References 32 publications

Supporting

Mentioning

Contrasting

Unclassified

Order By: Relevance

“…The distribution of mammoths is discussed for the climate-stratigraphic units as described in Table 1. These climate-stratigraphic units are comparable to time windows used in previous papers discussing faunal changes during the Late Pleistocene and Holocene (Baryshnikov andMarkova, 2002, 2009;Markova and Puzachenko, 2007;Markova and van Kolfschoten, 2008;Markova et al, 2010Markova et al, , 2011Markova et al, , 2013.…”

Section: Methodssupporting

confidence: 78%

“…Analysis of this database resulted in several publications, presenting data on the distribution of the mammoth in Europe during the last 50 kyrs for the different time intervals of the last glaciation and the Holocene (Markova et al, 1995(Markova et al, , 2010(Markova et al, , 2011(Markova et al, , 2013Markova and Puzachenko, 2007;Markova and van Kolfschoten, 2008). However, over the last several years, many new radiocarbon dates on mammoth bones have been obtained through joint projects supported by the Netherlands Organization on Scientific Research (NWO) and the Russian Foundation for Basic Research (RFBR).…”

Section: Introductionmentioning

confidence: 99%

See 1 more Smart Citation

The Eurasian mammoth distribution during the second half of the Late Pleistocene and the Holocene: Regional aspects

Puzachenko

Маркова

Косинцев

et al. 2017

Quaternary International

Self Cite

View full text Add to dashboard Cite

a b s t r a c tBased on geographic information (database PALEOFAUNA), in combination with 14 C and other methods of paleo dating (1584 localities, 4033 dates, including 1501 direct dates), we first examined details of changes of mammoth distribution in Eurasia on the whole and in single parts of the range over the last 50ky. The analysis of regional features in the dynamics of mammoth range and the quantity of dated localities acknowledged a leading role of the climatic (environmental) factor in these processes. The maximum size of the Eurasian range, the largest number of remains of mammoths from dated localities and, probably, the maximum total number of population were established for the range of 38.2 e8.6 cal ky BP (Denekamp interstadial ¼ Bryansk interstadial). In Western and Central Europe, the increase of population was observed during Huneborg stadial (40.8e38.2 cal ky BP). In eastern Siberia, the maximum population growth occurred in the Last Glacial Maximum (28.6e22.5 cal ky BP), and in Western Siberia e during Deglaciation (22.5e14.7 cal ky BP). The population dynamics at the periphery of the range (Islands of Japan, British Isles, Northern Europe, Southern Siberia and Northern China, and, but to lesser extent, South-Eastern Europe) differs from the dynamics of its main part. The southernmost parts of the range e Southern Siberia and southeastern Europe experienced similar changes. Population dynamics in the Iberian Peninsula was much alike the changes in Western and Central Europe. We suggested that some peripheral populations could periodically be isolated from the populations of the main part of the range. Direct calibrated radiocarbon dates fixed upper boundary of extinction of this species in different parts of range within time interval from 21 (the Iberian Peninsula) to 4 (northeastern Siberia) thousands years BP. The hypotheses about the causes of the dynamics of the area and population of the mammoth in Eurasia, including those related to the extinction of certain genetic lines of a mammoth in the Late Pleistocene, are being discussed.

show abstract

Section: Methodssupporting

confidence: 78%

Section: Introductionmentioning

confidence: 99%

The Eurasian mammoth distribution during the second half of the Late Pleistocene and the Holocene: Regional aspects

Puzachenko

Маркова

Косинцев

et al. 2017

Quaternary International

Self Cite

View full text Add to dashboard Cite

show abstract

“…2). An important increase of mammoth's population size in Europe took place between 31 and 29 ka BP, which is confirmed by dense radiocarbon dating of mammoth remains collected from almost whole North European Plain (Nadachowski et al, 2011; Ukkonen et al, 2011; Markova et al, 2013). Interestingly, during almost the whole Last Glacial Maximum (LGM), between ca.…”

Section: Woolly Mammoth (Mammuthus Primigenius)mentioning

confidence: 66%

Impact of climatic changes in the Late Pleistocene on migrations and extinctions of mammals in Europe: four case studies

Baca¹,

Nadachowski

Lipecki

et al. 2016

Preprint

View full text Add to dashboard Cite

21Climate changes that occurred during the Late Pleistocene have profound effects on the distribution of 22 many plant and animal species and influenced the formation of contemporary faunas and floras of 23 Europe. The course and mechanisms of responses of species to the past climate changes are now 24 being intensively studied by the use of direct radiocarbon dating and genetic analyses of fossil 25 remains. Here, we review the advances in understanding these processes by the example of four 26 mammal species: woolly mammoth (Mammuthus primigenius), cave bear (Ursus spelaeus s. l.), saiga 27 antelope (Saiga tatarica) and collared lemmings (Dicrostonyx ssp.). The cases discussed here as well 28 as others show that the migrations, range shifts and local extinctions were the main responses to 29 climate changes and that the dynamics of these climate driven processes were much more profound 30 2 than it was previously thought. Each species reacted by its individual manner, which depended on its 31 biology and adaptation abilities to the changing environment and climate conditions. The most severe 32 changes in European ecosystems that affected the largest number of species took place around 33-33 31 ka BP, during the Last Glacial Maximum 22-19 ka BP and the Late Glacial warming 15-13 ka BP. 34 35 37 38 84 2008; Palkopoulou et al., 2013). The divergence of lineages I and II was previously estimated to ca. 1 85 Ma ago (Debruyne et al., 2008; Gilbert and Drautz, 2008), however, most recent estimations suggest 86 much younger date about 300 ka BP (Palkopoulou et al., 2013). Coalescent simulations suggested 87 that actual split of three mammoth populations took place around 200 ka BP and was followed by a 88 demographic expansion that started around 121 ka BP (Palkopoulou et al., 2013). This expansion 89 coincides broadly with the end of Eemian Interstadial, which suggests that mammoths survived this 90 4 warm period confined to refugial areas and expanded as climate got cooler at the beginning of 91 Weichselian glaciation (Palkopoulou et al., 2013). Surprisingly, this was not supported by the analyses 92 of the whole paleogenomes, which indicated a much earlier expansion ca. 280 ka years ago and the 93 maximum effective population size during Eemian (Palkopoulou et al., 2015).94 95 96 Fig. 1. Woolly mammoth (Mammuthus primigenius). A -Bayesian phylogeny of Holarctic woolly 97 mammoths based on mtDNA cytochrome b sequences. The tree is a chronogram where branch 98 lengths denote time elapsed since divergence and the position of tips corresponds to calibrated 99 radiocarbon age of samples; B -distribution of paleontological sites with woolly mammoth 100 remains radiocarbon-dated to the indicated periods. Colours indicate mitochondrial DNA lineages 101 (modified after Palkopoulou et al., 2013). 103Despite, the ambiguities in the early history of mammoth populations, ancient DNA revealed also two 104 more recent population turnovers. In the Eemian Interglacial and Early Weichselian, woolly mammoths 105 that belonged to clad...

show abstract

“…Fig. but the palaeontological record from Kotelny, unfortunately, is still rather limited(Markova et al 2013). Macrofossils from sampled peat.…”

mentioning

confidence: 99%

“…The vegetation in the Kotelny area may have served as food resources for herbivore populations, and grazing may also have had effects on the vegetation composition (cf Zimov 2005). but the palaeontological record from Kotelny, unfortunately, is still rather limited(Markova et al 2013).…”

mentioning

confidence: 99%

Larix during the Mid‐Pleniglacial (Greenland Interstadial 8) on Kotelny Island, northern Siberia

Geel

Протопопов

Protopopova

et al. 2016

Boreas

View full text Add to dashboard Cite

Needles, wood and pollen of Larix, recorded in a peat deposit from Kotelny Island, northern Siberia, indicate the local occurrence of larch around 38 000 cal. a BP, which is during the Middle Pleniglacial (Greenland Interstadial 8) of the Weichselian last glacial period. The pollen record, dominated by Cyperaceae, Poaceae, Betula, Alnus, Salix and Artemisia, indicates steppe‐tundra conditions with some shrubs and trees. The distribution of Larix species plays an important role in the reconstruction of climatic conditions during the Weichselian in Siberia. Nowadays Larix does not occur on Kotelny Island and in the present situation the temperature may not be the limiting factor for Larix, but instead the long, snowy winters and the moist tundra vegetation. Our data may contribute to a better understanding of Larix refugia and Weichselian climatic conditions in northern Siberia.

show abstract

New data on changes in the European distribution of the mammoth and the woolly rhinoceros during the second half of the Late Pleistocene and the early Holocene

Cited by 44 publications

References 32 publications

The Eurasian mammoth distribution during the second half of the Late Pleistocene and the Holocene: Regional aspects

The Eurasian mammoth distribution during the second half of the Late Pleistocene and the Holocene: Regional aspects

Impact of climatic changes in the Late Pleistocene on migrations and extinctions of mammals in Europe: four case studies

Larix during the Mid‐Pleniglacial (Greenland Interstadial 8) on Kotelny Island, northern Siberia

Contact Info

Product

Resources

About