Articles | Volume 11, issue 6
https://doi.org/10.5194/se-11-2047-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/se-11-2047-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Lithological and geomorphological indicators of glacial genesis in the upper Quaternary strata, Nadym River basin, Western Siberia
Oleg Sizov
Oil and Gas Research Institute, Russian Academy of Sciences, Moscow,
Russia
Anna Volvakh
Sobolev Institute of Geology and Mineralogy, Siberian Branch of
Russian Academy of Sciences, Novosibirsk, Russia
Anatoly Molodkov
Department of Geology, Tallinn University of Technology, Tallinn, Estonia
Andrey Vishnevskiy
Department of Geology and Geophysics, Novosibirsk State University, Novosibirsk, Russia
Andrey Soromotin
Research Institute of Ecology and Natural Resource Management, Tyumen State University, Tyumen, Russia
Department of Applied Ecology, Saint-Petersburg State University, Saint Petersburg, Russia
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Persistent warm urban temperature anomalies – urban heat islands – significantly enhance already amplified climate warming in the Arctic. This study presents the surface urban heat islands in all circum-Arctic settlements with more than 3000 inhabitants. It reveals strong and persistent urban temperature anomalies during both summer and winter seasons that vary in different cities from 0.5 °C to more than 6.0 °C.
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In changing climate, tundra is expected to turn into shrubs and trees, diminishing reindeer pasture and increasing risks of tick-borne diseases. However, this transition may require a disturbance. Fires in Siberia are increasingly widespread. We studied wildfire dynamics and tundra–forest transition over 60 years in northwest Siberia near the Arctic Circle. Based on satellite data analysis, we found that transition occurs in 40 %–85 % of burned tundra compared to 5 %–15 % in non-disturbed areas.
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This study presents, for the first time, a characterisation of soil organic matter from the Gydan Peninsula in the Yamal Region, Western Siberia, Russia. We provide evidences that soils in this region accumulate lowly decomposed organic matter with a high mineralisation potential. This emphasises the vulnerability of this soil carbon pool to be remobilised as CO2 to the atmosphere under climate warming effects.
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E. Maksimova and E. Abakumov
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Revised manuscript not accepted
Related subject area
Subject area: The evolving Earth surface | Editorial team: Stratigraphy, sedimentology, geomorphology, morphotectonics, and palaeontology | Discipline: Quaternary geology
Submarine groundwater discharge site in the First Salpausselkä ice-marginal formation, south Finland
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This study establishes the local stratigraphy and 3-D aquifer geometry of a submarine groundwater discharge site in the Hanko Peninsula, south Finland. The study is based on a rich dataset of marine seismic profiles, multibeam and side-scan sonar images of the seafloor, and onshore ground-penetrating radar and refraction seismic profiles. The groundwater discharge takes place through metre-scale pockmarks on the seafloor, confirmed by elevated radon concentrations in the overlying water.
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Short summary
Analysing the genesis of Quaternary sediments is important for understanding the glaciation history and development of marine sediments in the northern part of Western Siberia. The key features of sedimentation and landform formation have been characterised for the first time in an example of a lithological column from the lower sources of the Nadym River. A comprehensive analysis was performed on the lithological, petrographic and geomorphological data from the upper Quaternary stratum.
Analysing the genesis of Quaternary sediments is important for understanding the glaciation...