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DOI10.1016/j.palaeo.2018.11.010
A multi-proxy palaeolimnological record of the last 16;600 years from coastal Lake Kushu in northern Japan
Schmidt M.; Leipe C.; Becker F.; Goslar T.; Hoelzmann P.; Mingram J.; Müller S.; Tjallingii R.; Wagner M.; Tarasov P.E.
发表日期2019
ISSN0031-0182
起始页码613
结束页码626
卷号514
英文摘要Based on diatom, aquatic pollen and non-pollen palynomorph (NPP), lake sediment microfacies, and X-ray fluorescence (XRF) analyses we define three main phases of lake basin development including a marshy phase (ca. 16,600–9400 cal. yr BP), lagoon phase (ca. 9400–5900 cal. yr BP) and freshwater lake phase (since ca. 5900 cal. yr BP). Marine influence on the lake system linked to global sea-level rise and the Holocene marine transgression reached a maximum between ca. 8000 and 6000 cal. yr BP. An increase of Aulacoseira subarctica at 5530 cal. yr BP marks the end of the Holocene Thermal Optimum (i.e. onset of Middle Holocene cooling) in the study region. Our results further suggest that freshwater Lake Kushu had a significant effect on the initial habitation of Rebun Island by sedentary hunter-gatherer populations. The reconstructed onset of stable freshwater conditions (ca. 5100 cal. yr BP) coincided with the appearance of the earliest permanent settlements during the Middle Jomon culture phase (ca. 5000–4000 cal. yr BP). On the other hand, there is evidence for human-induced changes in the limnological conditions. This includes enhanced sediment and nutrient input into Lake Kushu resulting in high eutrophication levels that caused strongly reduced diatom productivity and enhanced green algae growth, which can be attributed to human activities apparently associated with the Okhotsk (ca. 1450–950 cal. yr BP) and Classic Ainu (ca. 350–100 cal. yr BP) culture periods. © 2018 Elsevier B.V.
英文关键词Diatoms; Holocene Optimum; Hunter-gatherer occupation; Microfacies; Non-pollen palynomorphs; X-ray fluorescence
语种英语
scopus关键词basin evolution; coastal zone; diatom; eutrophication; freshwater ecosystem; Holocene; hunter-gatherer; lacustrine deposit; microfacies; paleolimnology; palynomorph; pollen; transgression; X-ray fluorescence; Hokkaido; Japan; Khabarovsk [Russian Federation]; Okhotsk; Rebun Island; Russian Federation; Aulacoseira subarctica; Bacillariophyta; Chlorophyta
来源期刊Palaeogeography, Palaeoclimatology, Palaeoecology
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/151132
作者单位Institute of Geological Sciences, Paleontology, Freie Universität Berlin, Malteserstr. 74-100, Berlin, 12249, Germany; Nagoya University, Institute for Space-Earth Environmental Research (ISEE), Research Institutes Building II, Furo-cho, Nagoya, 464-8601, Japan; Institute of Geographical Sciences, Physical Geography, Freie Universität Berlin, Malteserstr. 74-100, Berlin, 12249, Germany; Faculty of Physics, Adam Mickiewicz University, Umultowska, Poznan, 85, Poland; Poznan Radiocarbon Laboratory, Foundation of the A. Mickiewicz University, Rubiez 46, Poznan, Poland; Helmholtz Centre Potsdam, GeoForschungsZentrum, Telegrafenberg, Potsdam, 14473, Germany; Eurasia Department and Beijing Branch Office, German Archaeological Institute, Im Dol 2-6, Berlin, 14195, Germany
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Schmidt M.,Leipe C.,Becker F.,等. A multi-proxy palaeolimnological record of the last 16;600 years from coastal Lake Kushu in northern Japan[J],2019,514.
APA Schmidt M..,Leipe C..,Becker F..,Goslar T..,Hoelzmann P..,...&Tarasov P.E..(2019).A multi-proxy palaeolimnological record of the last 16;600 years from coastal Lake Kushu in northern Japan.Palaeogeography, Palaeoclimatology, Palaeoecology,514.
MLA Schmidt M.,et al."A multi-proxy palaeolimnological record of the last 16;600 years from coastal Lake Kushu in northern Japan".Palaeogeography, Palaeoclimatology, Palaeoecology 514(2019).
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