Neanderthals in changing environments from MIS 5 to early MIS 4 in northern Central Europe – Integrating archaeological, (chrono)stratigraphic and paleoenvironmental evidence at the site of Lichtenberg

Publikation: Beiträge in ZeitschriftenZeitschriftenaufsätzeForschungbegutachtet

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Neanderthals in changing environments from MIS 5 to early MIS 4 in northern Central Europe – Integrating archaeological, (chrono)stratigraphic and paleoenvironmental evidence at the site of Lichtenberg. / Weiss, Marcel; Hein, Michael; Urban, Brigitte et al.

in: Quaternary Science Reviews, Jahrgang 284, 107519, 15.05.2022.

Publikation: Beiträge in ZeitschriftenZeitschriftenaufsätzeForschungbegutachtet

Harvard

Weiss, M, Hein, M, Urban, B, Stahlschmidt, MC, Heinrich, S, Hilbert, YH, Power, RC, von Suchodoletz, H, Terberger, T, Böhner, U, Klimscha, F, Veil, S, Breest, K, Schmidt, J, Colarossi, D, Tucci, M, Frechen, M, Tanner, DC & Lauer, T 2022, 'Neanderthals in changing environments from MIS 5 to early MIS 4 in northern Central Europe – Integrating archaeological, (chrono)stratigraphic and paleoenvironmental evidence at the site of Lichtenberg', Quaternary Science Reviews, Jg. 284, 107519. https://doi.org/10.1016/j.quascirev.2022.107519

APA

Weiss, M., Hein, M., Urban, B., Stahlschmidt, M. C., Heinrich, S., Hilbert, Y. H., Power, R. C., von Suchodoletz, H., Terberger, T., Böhner, U., Klimscha, F., Veil, S., Breest, K., Schmidt, J., Colarossi, D., Tucci, M., Frechen, M., Tanner, D. C., & Lauer, T. (2022). Neanderthals in changing environments from MIS 5 to early MIS 4 in northern Central Europe – Integrating archaeological, (chrono)stratigraphic and paleoenvironmental evidence at the site of Lichtenberg. Quaternary Science Reviews, 284, [107519]. https://doi.org/10.1016/j.quascirev.2022.107519

Vancouver

Bibtex

@article{007c29f17114437e91b1671869bd82e2,
title = "Neanderthals in changing environments from MIS 5 to early MIS 4 in northern Central Europe – Integrating archaeological, (chrono)stratigraphic and paleoenvironmental evidence at the site of Lichtenberg",
abstract = "The resilience of Neanderthals towards changing climatic and environmental conditions, and especially towards severely cold climates in northern regions of central Europe, is still under debate. One way to address this is to investigate multi-layered occupation in different climatic intervals, using independently-compiled paleoenvironmental and chronological data. Unfortunately, most open-air sites on the northern European Plain lack a robust chronostratigraphy beyond the radiocarbon dating range, thereby often hampering direct links between human occupation and climate. Here we present the results of integrative research at the Middle Paleolithic open-air site of Lichtenberg, Northern Germany, comprising archaeology, luminescence dating, sedimentology, micromorphology, as well as pollen and phytolith analyses. Our findings clearly show Neanderthal presence in temperate, forested environments during the Mid-Eemian Interglacial, MIS 5e and the latest Br{\"o}rup Interstadial, MIS 5c/GI 22 (Lichtenberg II). For the previously known occupation Lichtenberg I, we revise the chronology from the former early MIS 3 (57 ± 6 ka) to early MIS 4/GS 19 (71.3 ± 7.3 ka), with dominant cold steppe/tundra vegetation. The early MIS 4 occupation suggests that Neanderthals could adjust well to severely cold environments and implies recurring population in the region between MIS 5 and MIS 3. The artefact assemblages differ between the temperate and cold environment occupations regarding size, blank production, typology and tool use. We argue that this distinctness can partially be explained by different site functions and occupation duration, as well as the availability of large and high-quality flint raw material. Raw material availability is in turn governed by changing vegetation cover that hindered or fostered sediment redeposition as a provider of flint from the primary source of the glacial sediments nearby.",
keywords = "Biology, Middle paleolithic, Neanderthals, Quaternary Stratigraphy, Luminescence dating, Palynology",
author = "Marcel Weiss and Michael Hein and Brigitte Urban and Stahlschmidt, {Mareike C.} and Susann Heinrich and Hilbert, {Yamandu H.} and Power, {Robert C.} and {von Suchodoletz}, Hans and Thomas Terberger and Utz B{\"o}hner and Florian Klimscha and Stephan Veil and Klaus Breest and Johannes Schmidt and Debra Colarossi and Mario Tucci and Manfred Frechen and Tanner, {David Colin} and Tobias Lauer",
note = "Publisher Copyright: {\textcopyright} 2022 Elsevier Ltd",
year = "2022",
month = may,
day = "15",
doi = "10.1016/j.quascirev.2022.107519",
language = "English",
volume = "284",
journal = "Quaternary Science Reviews",
issn = "0277-3791",
publisher = "Elsevier B.V.",

}

RIS

TY - JOUR

T1 - Neanderthals in changing environments from MIS 5 to early MIS 4 in northern Central Europe – Integrating archaeological, (chrono)stratigraphic and paleoenvironmental evidence at the site of Lichtenberg

AU - Weiss, Marcel

AU - Hein, Michael

AU - Urban, Brigitte

AU - Stahlschmidt, Mareike C.

AU - Heinrich, Susann

AU - Hilbert, Yamandu H.

AU - Power, Robert C.

AU - von Suchodoletz, Hans

AU - Terberger, Thomas

AU - Böhner, Utz

AU - Klimscha, Florian

AU - Veil, Stephan

AU - Breest, Klaus

AU - Schmidt, Johannes

AU - Colarossi, Debra

AU - Tucci, Mario

AU - Frechen, Manfred

AU - Tanner, David Colin

AU - Lauer, Tobias

N1 - Publisher Copyright: © 2022 Elsevier Ltd

PY - 2022/5/15

Y1 - 2022/5/15

N2 - The resilience of Neanderthals towards changing climatic and environmental conditions, and especially towards severely cold climates in northern regions of central Europe, is still under debate. One way to address this is to investigate multi-layered occupation in different climatic intervals, using independently-compiled paleoenvironmental and chronological data. Unfortunately, most open-air sites on the northern European Plain lack a robust chronostratigraphy beyond the radiocarbon dating range, thereby often hampering direct links between human occupation and climate. Here we present the results of integrative research at the Middle Paleolithic open-air site of Lichtenberg, Northern Germany, comprising archaeology, luminescence dating, sedimentology, micromorphology, as well as pollen and phytolith analyses. Our findings clearly show Neanderthal presence in temperate, forested environments during the Mid-Eemian Interglacial, MIS 5e and the latest Brörup Interstadial, MIS 5c/GI 22 (Lichtenberg II). For the previously known occupation Lichtenberg I, we revise the chronology from the former early MIS 3 (57 ± 6 ka) to early MIS 4/GS 19 (71.3 ± 7.3 ka), with dominant cold steppe/tundra vegetation. The early MIS 4 occupation suggests that Neanderthals could adjust well to severely cold environments and implies recurring population in the region between MIS 5 and MIS 3. The artefact assemblages differ between the temperate and cold environment occupations regarding size, blank production, typology and tool use. We argue that this distinctness can partially be explained by different site functions and occupation duration, as well as the availability of large and high-quality flint raw material. Raw material availability is in turn governed by changing vegetation cover that hindered or fostered sediment redeposition as a provider of flint from the primary source of the glacial sediments nearby.

AB - The resilience of Neanderthals towards changing climatic and environmental conditions, and especially towards severely cold climates in northern regions of central Europe, is still under debate. One way to address this is to investigate multi-layered occupation in different climatic intervals, using independently-compiled paleoenvironmental and chronological data. Unfortunately, most open-air sites on the northern European Plain lack a robust chronostratigraphy beyond the radiocarbon dating range, thereby often hampering direct links between human occupation and climate. Here we present the results of integrative research at the Middle Paleolithic open-air site of Lichtenberg, Northern Germany, comprising archaeology, luminescence dating, sedimentology, micromorphology, as well as pollen and phytolith analyses. Our findings clearly show Neanderthal presence in temperate, forested environments during the Mid-Eemian Interglacial, MIS 5e and the latest Brörup Interstadial, MIS 5c/GI 22 (Lichtenberg II). For the previously known occupation Lichtenberg I, we revise the chronology from the former early MIS 3 (57 ± 6 ka) to early MIS 4/GS 19 (71.3 ± 7.3 ka), with dominant cold steppe/tundra vegetation. The early MIS 4 occupation suggests that Neanderthals could adjust well to severely cold environments and implies recurring population in the region between MIS 5 and MIS 3. The artefact assemblages differ between the temperate and cold environment occupations regarding size, blank production, typology and tool use. We argue that this distinctness can partially be explained by different site functions and occupation duration, as well as the availability of large and high-quality flint raw material. Raw material availability is in turn governed by changing vegetation cover that hindered or fostered sediment redeposition as a provider of flint from the primary source of the glacial sediments nearby.

KW - Biology

KW - Middle paleolithic

KW - Neanderthals

KW - Quaternary Stratigraphy

KW - Luminescence dating

KW - Palynology

UR - http://www.scopus.com/inward/record.url?scp=85128383577&partnerID=8YFLogxK

U2 - 10.1016/j.quascirev.2022.107519

DO - 10.1016/j.quascirev.2022.107519

M3 - Journal articles

VL - 284

JO - Quaternary Science Reviews

JF - Quaternary Science Reviews

SN - 0277-3791

M1 - 107519

ER -

DOI