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  1. Article

    Evolution of subsea permafrost landscapes in Arctic Siberia since the Late Pleistocene: a synoptic insight from acoustic data of the Laptev Sea

    Using high-resolution seismic data, this study aims at investigating the evolution and morphological diversity of subsea permafrost features on the eastern Laptev Sea shelf, Arctic Siberia. Several seismic fac...

    P. Rekant, H. A. Bauch, T. Schwenk, A. Portnov, E. Gusev, V. Spiess in arktos (2015)

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    Article

    Late Pleistocene-Holocene events on the continental slope of the Laptev Sea: Evidence from benthic and planktonic foraminiferal assemblages

    This work is dedicated to the study of benthic and planktonic foraminifers and is a contribution to the multidisciplinary investigations of Core PS51/154-11 from the Laptev Sea. The paleoecological analysis of...

    Ya. S. Ovsepyan, E. E. Taldenkova, H. A. Bauch in Stratigraphy and Geological Correlation (2015)

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    Article

    Migrations of the North Atlantic Polar front during the last 300 ka: Evidence from planktic foraminiferal data

    The main migrations of the Polar front (PF) during the last 300 ka were identified using planktic foraminiferal census data and derived from them sea surface paleotemperature (SST) estimates in two synchronize...

    L. D. Bashirova, E. S. Kandiano, V. V. Sivkov, H. A. Bauch in Oceanology (2014)

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    Article

    Modern data on the biostratigraphy and geochronology of White Sea sediments

    Ye. I. Polyakova, Ye. A. Novichkova, A. P. Lisitzin, H. A. Bauch in Doklady Earth Sciences (2014)

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    Article

    Deep Arctic Ocean warming during the last glacial cycle

    In the Arctic Ocean, a salinity gradient separates a shallow layer of cold, relatively fresh water from the warmer, saltier Atlantic water below. A reconstruction of intermediate water temperatures in the Arct...

    T. M. Cronin, G. S. Dwyer, J. Farmer, H. A. Bauch, R. F. Spielhagen in Nature Geoscience (2012)

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    Article

    Reconstruction of deep-water conditions in the North Atlantic during MIS 9 based on benthic foraminiferal assemblages

    Marine isotope stage (MIS) 9 is one of the least investigated Pleistocene interglaciations. The present study describes reconstructions of deep-water conditions during this time interval based on benthic foram...

    S. A. Kostygov, E. S. Kandiano, H. A. Bauch in Oceanology (2010)

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    Article

    Arctic quaternary ostracods and their use in paleoreconstructions

    The paper deals with original and published data on fossil ostracodal assemblages from the Eurasian Arctic Kara, Laptev and Chuckchi seas. As a whole, six ecologically different assemblages were distinguished ...

    A. Yu. Stepanova, E. E. Taldenkova, H. A. Bauch in Paleontological Journal (2010)

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    Article

    Changes in the Lena River runoff during the Holocene

    The spatial and temporal changes in the Lena River runoff over the last 9 thousand years are reconstructed through studying the freshwater microfossils in sediment cores obtained from the Laptev Sea inner shel...

    Ye. I. Polyakova, T. S. Klyuvitkina, E. A. Novichkova, H. A. Bauch in Water Resources (2009)

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    Article

    Hydrological changes in the Laptev Sea during the Holocene inferred from the studies of aquatic palynomorphs

    Based on the study of aquatic palynomorph assemblages in two Holocene sediment cores obtained from the eastern Laptev Sea shelf, the main stages in the postglacial transgression are reconstructed for the last ...

    T. S. Klyuvitkina, H. A. Bauch in Oceanology (2006)

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    Article

    Palaeoceanographic implications of genetic variation in living North Atlantic Neogloboquadrina pachyderma

    The shells of the planktonic foraminifer Neogloboquadrina pachyderma have become a classical tool for reconstructing glacial–interglacial climate conditions in the North Atlantic Ocean1,2,3. Palaeoceanographers u...

    D. Bauch, K. Darling, J. Simstich, H.A. Bauch, H. Erlenkeuser, D. Kroon in Nature (2003)

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    Article

    Changes in the deposition of terrestrial organic matter on the Laptev Sea shelf during the Holocene: evidence from stable carbon isotopes

    Stable carbon isotope ratios in the organic fraction of surface sediments from the Laptev Sea shelf were analyzed in order to study the modern distribution pattern of terrestrial organic matter. The δ13Corg sign...

    T. Mueller-Lupp, H. A. Bauch, H. Erlenkeuser in International Journal of Earth Sciences (2000)

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    Article

    Glacial–interglacial records of the reflectance of sediments from the Norwegian–Greenland–Iceland Sea (Nordic seas)

     The reflectance of sediments (gray level) were measured on 11 sediment cores from the Norwegian–Greenland–Iceland Sea (Nordic seas). The analyzed time interval covers the past five glacial–interglacial cycles...

    H. A. Bauch, J. P. Helmke in International Journal of Earth Sciences (1999)

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    Chapter

    Distribution of Pollen and Spores in Surface Sediments of the Laptev Sea

    The palynological content of Laptev Sea surface sediments were studied. The pollen-spore spectra in these recent sediments are characterized by a predominance of coniferous pollen and moss spores. The pollen h...

    O. D. Naidina, H. A. Bauch in Land-Ocean Systems in the Siberian Arctic (1999)

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    Chapter

    Planktic Foraminifera in Holocene Sediments from the Laptev Sea and the Central Arctic Ocean: Species Distribution and Paleobiogeographical Implication

    Two sediment cores, one from the Siberian Laptev Sea shelf and another from the central Arctic Ocean were investigated with respect to the temporal distribution of planktic foraminifera as well as the species ...

    H. A. Bauch in Land-Ocean Systems in the Siberian Arctic (1999)

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    Chapter

    Dynamics and History of the Laptev Sea and its Continental Hinterland: A Summary

    Russian and German scientists have investigated the extreme environmental system in and around the Laptev Sea in the Siberian Arctic. For the first time a major comprehensive research program combining the eff...

    J. Thiede, L. Timokhov, H. A. Bauch in Land-Ocean Systems in the Siberian Arctic (1999)