Holocene summer temperature reconstruction from plant sedaDNA and chironomids from the northern boreal forest DOI Creative Commons
Roseanna J. Mayfield, Dilli P. Rijal, Peter D. Heintzman

et al.

Quaternary Science Reviews, Journal Year: 2024, Volume and Issue: 345, P. 109045 - 109045

Published: Oct. 31, 2024

Language: Английский

Temporal and spatial climate changes in the mid-Baltic region in the Late Glacial and the Holocene: Pollen-based reconstructions DOI
Laura Gedminienė, Andrej Spiridonov, Miglė Stančikaitė

et al.

CATENA, Journal Year: 2025, Volume and Issue: 252, P. 108851 - 108851

Published: Feb. 21, 2025

Language: Английский

Citations

1

Disruption of boreal lake circulation in response to mid-Holocene warmth; evidence from the varved sediments of Lake Nautajärvi, southern Finland DOI Creative Commons
Paul Lincoln, Rik Tjallingii, Emilia Kosonen

et al.

The Science of The Total Environment, Journal Year: 2025, Volume and Issue: 964, P. 178519 - 178519

Published: Jan. 23, 2025

Language: Английский

Citations

0

Varved sediments of Lake Gorzyńskie, western Poland: a new archive of climatic and environmental changes during the Late Glacial and the Holocene in central Europe DOI Creative Commons

Maria Kril,

Alicja Bonk, Maurycy Żarczyński

et al.

Research Square (Research Square), Journal Year: 2025, Volume and Issue: unknown

Published: Feb. 27, 2025

Abstract In this study, we present a newly discovered varved sediment site located in western Poland, where such records are scarce. The profile from Lake Gorzyńskie is 10.45 meters long and covers the last ca. 13,250 years. Using varve counting thickness measurements together with radiometric dating (14C, 210Pb, 137Cs), robust age-depth model was developed. Sediment lithology, microfacies, statistical analysis of chemical composition allow identification six depositional phases: late Allerød (≈ 13,250–12,675 cal BP), Younger Dryas (12,675–11,600 early Holocene (11,600–9,100 main part (9,100–2,250 two phases (2,250–750 BP, 750 BP–present). remarkably well recorded pronounced increase allochthonous deposition followed by stable sedimentation during increased variability since 9,100 BP. Short-term fluctuations coinciding known paleoclimatic events as Preboreal Oscillation 10.3 k climate event, also evident. Distinct changes associated increasing human impact. record offers not only insights into long-term trends environmental history Poland but short-term paleoclimate Late Glacial.

Language: Английский

Citations

0

Holocene hydroclimate and landscape changes as drivers of organic carbon cycling in a small northern Fennoscandian lake DOI Creative Commons
Lilia E. Orozco, Jan Weckström, Mateusz Płóciennik

et al.

Quaternary Science Reviews, Journal Year: 2025, Volume and Issue: 357, P. 109323 - 109323

Published: March 27, 2025

Language: Английский

Citations

0

The effect of the 8.2 ka cold event on Fennoscandian hunter-gatherer metapopulation inferred from climatic, environmental, and archaeological signals DOI Creative Commons
Mikael A. Manninen, Roope Oskari Kaaronen, Jussi T. Eronen

et al.

Quaternary Environments and Humans, Journal Year: 2025, Volume and Issue: unknown, P. 100065 - 100065

Published: April 1, 2025

Language: Английский

Citations

0

Holocene summer temperature reconstruction from plant sedaDNA and chironomids from the northern boreal forest DOI Creative Commons
Roseanna J. Mayfield, Dilli P. Rijal, Peter D. Heintzman

et al.

Quaternary Science Reviews, Journal Year: 2024, Volume and Issue: 345, P. 109045 - 109045

Published: Oct. 31, 2024

Language: Английский

Citations

1