Triassic in the northernmost Atlantic—Linking North Greenland and the southwestern Barents Sea

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Standard

Triassic in the northernmost Atlantic—Linking North Greenland and the southwestern Barents Sea. / Bjerager, Morten; Alsen, Peter; Bojesen-Koefoed, Jørgen A.; Fyhn, Michael B. W.; Hovikoski, Jussi; Keulen, Nynke; Lindström, Sofie; Therkelsen, Jens; Thomsen, Tonny B. .

I: Terra Nova, Bind 35, Nr. 4, 2023, s. 250-259.

Publikation: Bidrag til tidsskrift › Tidsskriftartikel › Forskning › fagfællebedømt

Harvard

Bjerager, M, Alsen, P, Bojesen-Koefoed, JA, Fyhn, MBW, Hovikoski, J, Keulen, N, Lindström, S, Therkelsen, J & Thomsen, TB 2023, 'Triassic in the northernmost Atlantic—Linking North Greenland and the southwestern Barents Sea', Terra Nova, bind 35, nr. 4, s. 250-259. https://doi.org/10.1111/ter.12649

APA

Bjerager, M., Alsen, P., Bojesen-Koefoed, J. A., Fyhn, M. B. W., Hovikoski, J., Keulen, N., Lindström, S., Therkelsen, J., & Thomsen, T. B. (2023). Triassic in the northernmost Atlantic—Linking North Greenland and the southwestern Barents Sea. Terra Nova, 35(4), 250-259. https://doi.org/10.1111/ter.12649

Vancouver

Bjerager M, Alsen P, Bojesen-Koefoed JA, Fyhn MBW, Hovikoski J, Keulen N o.a. Triassic in the northernmost Atlantic—Linking North Greenland and the southwestern Barents Sea. Terra Nova. 2023;35(4):250-259. https://doi.org/10.1111/ter.12649

Author

Bjerager, Morten ; Alsen, Peter ; Bojesen-Koefoed, Jørgen A. ; Fyhn, Michael B. W. ; Hovikoski, Jussi ; Keulen, Nynke ; Lindström, Sofie ; Therkelsen, Jens ; Thomsen, Tonny B. . / Triassic in the northernmost Atlantic—Linking North Greenland and the southwestern Barents Sea. I: Terra Nova. 2023 ; Bind 35, Nr. 4. s. 250-259.

Bibtex

@article{c39efe7e3eaf41479efd2ab77a08f05e,
title = "Triassic in the northernmost Atlantic—Linking North Greenland and the southwestern Barents Sea",
abstract = "The Wandel Sea Basin in North Greenland was part of the epicontinental Boreal Sea in Triassic time. The basin formed the western margin of the northernmost Atlantic elongated sea connecting southwards with basins along the conjugate Greenland—Norwegian margins. A multidisciplinary dataset including sedimentology, biostratigraphy, organic geochemistry and sedimentary provenance, allow to document its basin evolution. The Wandel Sea Basin was transgressed in the Dienerian with marine deposition prevailing until the Norian. Sediments were mainly sourced from the Greenlandic Caledonian basement and deposited on a 100 km wide shallow marine shelf during the Early Triassic. In Middle Triassic, oil-prone mudstones formed in oxygen-depleted deep shelf settings, including eastern Wandel Sea Basin. Detrital zircon U–Pb ages show that by Carnian times, the >1000 km wide, Uralian-sourced, deltaic shelf had prograded westward across the Barents Sea reaching the eastern north Greenland and de facto nearly closed the northernmost Atlantic Sea.",
author = "Morten Bjerager and Peter Alsen and Bojesen-Koefoed, {J{\o}rgen A.} and Fyhn, {Michael B. W.} and Jussi Hovikoski and Nynke Keulen and Sofie Lindstr{\"o}m and Jens Therkelsen and Thomsen, {Tonny B.}",
year = "2023",
doi = "10.1111/ter.12649",
language = "English",
volume = "35",
pages = "250--259",
journal = "Terra Nova",
issn = "0954-4879",
publisher = "Wiley-Blackwell",
number = "4",

}

RIS

TY - JOUR

T1 - Triassic in the northernmost Atlantic—Linking North Greenland and the southwestern Barents Sea

AU - Bjerager, Morten

AU - Alsen, Peter

AU - Bojesen-Koefoed, Jørgen A.

AU - Fyhn, Michael B. W.

AU - Hovikoski, Jussi

AU - Keulen, Nynke

AU - Lindström, Sofie

AU - Therkelsen, Jens

AU - Thomsen, Tonny B.

PY - 2023

Y1 - 2023

N2 - The Wandel Sea Basin in North Greenland was part of the epicontinental Boreal Sea in Triassic time. The basin formed the western margin of the northernmost Atlantic elongated sea connecting southwards with basins along the conjugate Greenland—Norwegian margins. A multidisciplinary dataset including sedimentology, biostratigraphy, organic geochemistry and sedimentary provenance, allow to document its basin evolution. The Wandel Sea Basin was transgressed in the Dienerian with marine deposition prevailing until the Norian. Sediments were mainly sourced from the Greenlandic Caledonian basement and deposited on a 100 km wide shallow marine shelf during the Early Triassic. In Middle Triassic, oil-prone mudstones formed in oxygen-depleted deep shelf settings, including eastern Wandel Sea Basin. Detrital zircon U–Pb ages show that by Carnian times, the >1000 km wide, Uralian-sourced, deltaic shelf had prograded westward across the Barents Sea reaching the eastern north Greenland and de facto nearly closed the northernmost Atlantic Sea.

AB - The Wandel Sea Basin in North Greenland was part of the epicontinental Boreal Sea in Triassic time. The basin formed the western margin of the northernmost Atlantic elongated sea connecting southwards with basins along the conjugate Greenland—Norwegian margins. A multidisciplinary dataset including sedimentology, biostratigraphy, organic geochemistry and sedimentary provenance, allow to document its basin evolution. The Wandel Sea Basin was transgressed in the Dienerian with marine deposition prevailing until the Norian. Sediments were mainly sourced from the Greenlandic Caledonian basement and deposited on a 100 km wide shallow marine shelf during the Early Triassic. In Middle Triassic, oil-prone mudstones formed in oxygen-depleted deep shelf settings, including eastern Wandel Sea Basin. Detrital zircon U–Pb ages show that by Carnian times, the >1000 km wide, Uralian-sourced, deltaic shelf had prograded westward across the Barents Sea reaching the eastern north Greenland and de facto nearly closed the northernmost Atlantic Sea.

U2 - 10.1111/ter.12649

DO - 10.1111/ter.12649

M3 - Journal article

VL - 35

SP - 250

EP - 259

JO - Terra Nova

JF - Terra Nova

SN - 0954-4879

IS - 4

ER -

ID: 341337618