Shallow depositional basins as potential archives of palaeoenvironmental changes in southwestern Greenland over the last 800 years
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F44555601%3A13520%2F20%3A43895642" target="_blank" >RIV/44555601:13520/20:43895642 - isvavai.cz</a>
Alternative codes found
RIV/60076658:12310/21:43904229 RIV/00216208:11310/21:10422158 RIV/60460709:41210/21:82424 RIV/00216224:14310/21:00120914
Result on the web
<a href="https://onlinelibrary.wiley.com/doi/abs/10.1111/bor.12483" target="_blank" >https://onlinelibrary.wiley.com/doi/abs/10.1111/bor.12483</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1111/bor.12483" target="_blank" >10.1111/bor.12483</a>
Alternative languages
Result language
angličtina
Original language name
Shallow depositional basins as potential archives of palaeoenvironmental changes in southwestern Greenland over the last 800 years
Original language description
The Arctic, one of the most sensitive components of the Earth's climate system, experienced pronounced climatic fluctuations during the Late Holocene. In order to obtain a detailed record of past environmental and climatic variability, sedimentary cores from two interconnected infilled depositional basins in the Kobbefjord area, southwestern Greenland, were retrieved and subjected to a multi-proxy investigation. The absolute chronostratigraphy was established through radiocarbon (14C) and short-lived radioisotope (210Pb, 137Cs) dating. We also analysed magnetic susceptibility, grain size, X-ray fluorescence element composition, total content of carbon, nitrogen and sulphur, biogenic silica and diatom assemblages. The palaeoenvironmental reconstruction presented from the upper basin records ~800 years of sedimentation in a former shallow Arctic lake/pond that was modulated by catchment processes and regional hydroclimate. The record is dominated by alternating periods of increased organic and clastic deposition, suggesting warmer/drier and colder/wetter climate, respectively. Comparison of our records with other proxy-based lacustrine, marine and glacier records and instrumental measurements from Greenland and the North Atlantic reveals common climatic trends, consistent with the inferred North Atlantic Oscillation pattern. Periods at ~800-600, ~320-220 and ~140-30 cal. a BP correspond to the main cold phases. The earliest climatic deterioration coincides with the demise of the nearby Norse Western Settlement. The most recent cold period represents the culmination of the Little Ice Age with the maximum Holocene advances of Greenland glaciers. Ameliorated conditions predominated at ~550-320 and ~220-140 cal. a BP. The evolution of both water bodies is concluded by transition into oligotrophic peat bogs after complete infilling of the basins at ~30 cal. a BP. Despite differences in proxy signals between the coring sites, this study endorses the usefulness of shallow lake/pond sediments from infilled basins for environmental reconstructions, as long as local depositional processes do not mask the external driving factors.
Czech name
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Czech description
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Classification
Type
J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database
CEP classification
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OECD FORD branch
10511 - Environmental sciences (social aspects to be 5.7)
Result continuities
Project
Result was created during the realization of more than one project. More information in the Projects tab.
Continuities
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Others
Publication year
2020
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
Boreas
ISSN
0300-9483
e-ISSN
—
Volume of the periodical
50
Issue of the periodical within the volume
1
Country of publishing house
NO - NORWAY
Number of pages
17
Pages from-to
262-278
UT code for WoS article
000587342500001
EID of the result in the Scopus database
2-s2.0-85096775955