Folgen
Maciej Mateusz Telesiński
Maciej Mateusz Telesiński
Institute of Oceanology, Polish Academy of Sciences, Sopot, Poland
Bestätigte E-Mail-Adresse bei iopan.pl - Startseite
Titel
Zitiert von
Zitiert von
Jahr
Water mass evolution of the Greenland Sea since late glacial times
MM Telesiński, RF Spielhagen, HA Bauch
Climate of the Past 10 (1), 123-136, 2014
422014
A high‐resolution L ateglacial and H olocene palaeoceanographic record from the G reenland S ea
MM Telesiński, RF Spielhagen, EM Lind
Boreas 43 (2), 273-285, 2014
352014
Evolution of the central Nordic Seas over the last 20 thousand years
MM Telesiński, HA Bauch, RF Spielhagen, ES Kandiano
Quaternary Science Reviews 121, 98-109, 2015
322015
Could Norwegian fjords serve as an analogue for the future of the Svalbard fjords? State and fate of high latitude fjords in the face of progressive “atlantification”
A Kujawa, M Łącka, N Szymańska, J Pawłowska, MM Telesiński, ...
Polar Biology 44, 2217-2233, 2021
122021
Palaeoceanographic evolution of the SW Svalbard shelf over the last 14 000 years
MM Telesiński, JE Przytarska, B Sternal, M Forwick, W Szczuciński, ...
Boreas 47 (2), 410-422, 2018
102018
Ventilation history of the Nordic Seas deduced from pelagic‐benthic radiocarbon age offsets
MM Telesiński, MM Ezat, F Muschitiello, HA Bauch, RF Spielhagen
Geochemistry, Geophysics, Geosystems 22 (4), e2020GC009132, 2021
72021
The significance of Atlantic Water routing in the Nordic Seas: the Holocene perspective
MM Telesiński, M Łącka, A Kujawa, M Zajączkowski
The Holocene 32 (10), 1104-1116, 2022
32022
Paleoceanography of the Northwestern Greenland Sea and Return Atlantic Current evolution, 35–4 kyr BP
D Devendra, M Łącka, MM Telesiński, TL Rasmussen, K Sztybor, ...
Global and Planetary Change 217, 103947, 2022
22022
Foraminifera‐derived carbon contribution to sedimentary inorganic carbon pool: A case study from three Norwegian fjords
N Szymańska, M Łącka, K Koziorowska‐Makuch, K Kuliński, J Pawłowska, ...
Geobiology 19 (6), 631-641, 2021
22021
Dinoflagellate cysts and benthic foraminifera from surface sediments of Svalbard fjords and shelves as paleoenvironmental indicators
MM Telesiński, V Pospelova, KN Mertens, M Kucharska, M Zajączkowski
Oceanologia 65 (4), 571-594, 2023
12023
Causes and consequences of Arctic freshwater routing into the Nordic Seas during late Marine Isotope Stage 5
MM Telesiński, HA Bauch, RF Spielhagen
Journal of Quaternary Science 33 (7), 794-803, 2018
12018
Reconstructing Late Glacial Atlantic Water Advection in the Western Fram Strait: Insights from Marine Sediment Cores
M Telesiński, M Zajączkowski
EGU24, 2024
2024
Worldwide consequences of a mid-Holocene cooling in the Nordic Seas
M Telesiński, W Liu, X Ren, M Zajączkowski
EarthArXiv, 2023
2023
A late response of the sea-ice cover to Neoglacial cooling in the western Barents Sea
MM Telesiński, M Kucharska, M Łącka, M Zajączkowski
The Holocene, 09596836241247305, 2023
2023
6.5 ka BP cold spell in the Nordic Seas: a potential trigger for a global cooling event?
MM Telesiński, M Zajączkowski
EGU General Assembly Conference Abstracts, EGU-38, 2023
2023
Nordic Seas origins of a mid-Holocene global cooling event
MM Telesiński, M Zajączkowski
Available at SSRN 4400856, 2023
2023
The significance of Atlantic Water routing in the Nordic Seas during the present interglacial
MM Telesiński, M Łącka, A Kujawa, M Zajączkowski
EGU General Assembly Conference Abstracts, EGU22-1312, 2022
2022
Does foraminiferal test size reflect changes in palaeoenvironmental conditions?—a case study from the southern Svalbard shelf
MM Telesiński, N Szymańska, J Pawłowska, M Zajączkowski
Polar Research, 2020
2020
Changes in the Greenland Sea deep convection since the last glacial-first results
MM Telesiński, M Zajączkowski
EGU General Assembly Conference Abstracts, 12652, 2018
2018
Development of northern Nordic Seas deep convection during the Holocene–implications from surface and bottom water foraminiferal d 13 C records
MM Telesiński, RF Spielhagen, HA Bauch
2015
Das System kann den Vorgang jetzt nicht ausführen. Versuchen Sie es später erneut.
Artikel 1–20