Articles | Volume 13, issue 4
https://doi.org/10.5194/cp-13-359-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/cp-13-359-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
19 Apr 2017
Research article |
| 19 Apr 2017
Summer temperature evolution on the Kamchatka Peninsula, Russian Far East, during the past 20 000 years
Alfred Wegener Institute Helmholtz Centre for Polar and Marine
Research, Bremerhaven, 27570, Germany
Department of Geosciences University of Bremen, Bremen, 28359,
Germany
Jens Hefter
Alfred Wegener Institute Helmholtz Centre for Polar and Marine
Research, Bremerhaven, 27570, Germany
Gerrit Lohmann
Alfred Wegener Institute Helmholtz Centre for Polar and Marine
Research, Bremerhaven, 27570, Germany
Lars Max
Alfred Wegener Institute Helmholtz Centre for Polar and Marine
Research, Bremerhaven, 27570, Germany
Ralf Tiedemann
Alfred Wegener Institute Helmholtz Centre for Polar and Marine
Research, Bremerhaven, 27570, Germany
Gesine Mollenhauer
Alfred Wegener Institute Helmholtz Centre for Polar and Marine
Research, Bremerhaven, 27570, Germany
Department of Geosciences University of Bremen, Bremen, 28359,
Germany
MARUM – Centre for Environmental Sciences, University of Bremen,
Bremen, 28359, Germany
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- Northeast Siberian Permafrost Ice‐Wedge Stable Isotopes Depict Pronounced Last Glacial Maximum Winter Cooling S. Wetterich et al. 10.1029/2020GL092087
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- Potential palaeoflora of Last Glacial Maximum Eastern Beringia, northwest North America W. Strong 10.1007/s00334-021-00823-4
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- Assessment of long-chain n-alkanes as a paleoclimate proxy in the Bering Sea sediments O. Seki et al. 10.1016/j.pocean.2021.102687
- Sediment provenance variations in the southern Okhotsk Sea over the last 180 ka: Evidence from light and heavy minerals K. Wang et al. 10.1016/j.palaeo.2017.04.017
17 citations as recorded by crossref.
- Sedimentary Ancient DNA From the Subarctic North Pacific: How Sea Ice, Salinity, and Insolation Dynamics Have Shaped Diatom Composition and Richness Over the Past 20,000 Years H. Zimmermann et al. 10.1029/2020PA004091
- Pollen characteristics of Zelyony Mys yedoma and ground squirrel' burrows A. Vasil'chuk & Y. Vasil'chuk 10.7256/2453-8922.2021.1.32985
- Permafrost-carbon mobilization in Beringia caused by deglacial meltwater runoff, sea-level rise and warming V. Meyer et al. 10.1088/1748-9326/ab2653
- Climate and vegetation changes in southern Primorye (Russian Far East) since the Last Glacial Maximum: A quantitative analysis T. Evstigneeva et al. 10.1016/j.palwor.2024.06.009
- Paleoclimate data assimilation with CLIMBER-X: An ensemble Kalman filter for the last deglaciation A. Masoum et al. 10.1371/journal.pone.0300138
- Hypersensitivity of glacial summer temperatures in Siberia P. Bakker et al. 10.5194/cp-16-371-2020
- Overturning circulation, nutrient limitation, and warming in the Glacial North Pacific J. Rae et al. 10.1126/sciadv.abd1654
- A Modeling Perspective on the Lingering Glacial Sea Surface Temperature Conundrum S. Krätschmer et al. 10.1029/2022GL100378
- New global lacustrine brGDGTs temperature calibrations based on machine learning Z. Zhu et al. 10.1016/j.quascirev.2025.109319
- Early Holocene Thermal Maximum recorded by branched tetraethers and pollen in Western Europe (Massif Central, France) C. Martin et al. 10.1016/j.quascirev.2019.106109
- Late Glacial hunter-gatherer pottery in the Russian Far East: Indications of diversity in origins and use S. Shoda et al. 10.1016/j.quascirev.2019.106124
- Northeast Siberian Permafrost Ice‐Wedge Stable Isotopes Depict Pronounced Last Glacial Maximum Winter Cooling S. Wetterich et al. 10.1029/2020GL092087
- Deglacial records of terrigenous organic matter accumulation off the Yukon and Amur rivers based on lignin phenols and long-chain n-alkanes M. Cao et al. 10.5194/cp-19-159-2023
- Oceanographic and Climatic Change in the Bering Sea, Last Glacial Maximum to Holocene B. Pelto et al. 10.1002/2017PA003265
- Potential palaeoflora of Last Glacial Maximum Eastern Beringia, northwest North America W. Strong 10.1007/s00334-021-00823-4
- Evaluation of reconstructed sea surface temperatures based onU37k′from sediment surface samples of the North Pacific L. Max et al. 10.1016/j.quascirev.2020.106496
- Assessment of long-chain n-alkanes as a paleoclimate proxy in the Bering Sea sediments O. Seki et al. 10.1016/j.pocean.2021.102687
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