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Jan Kresten Nielsen

Researcher at Süleyman Demirel University

Publications -  29
Citations -  702

Jan Kresten Nielsen is an academic researcher from Süleyman Demirel University. The author has contributed to research in topics: Arctica islandica & Heat transfer. The author has an hindex of 9, co-authored 29 publications receiving 621 citations. Previous affiliations of Jan Kresten Nielsen include Equinor.

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Names for trace fossils: a uniform approach

TL;DR: The term ‘work of an animal' should be deleted from the code, and ichnotaxa should be based solely on trace fossils as defined herein, and the following emendations are proposed to the International Code of Zoological Nomenclature.
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In defence of an iconic ichnogenus – Oichnus Bromley, 1981

TL;DR: Investigation of the type material of ‘Sedilichnus’ shows that it probably describes variably shaped oscula and thus is a genuine morphological character of the host sponge Prokaliapsisjanus, rather than a bioerosion trace fossil.
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Compound response of marine and terrestrial ecosystems to varying climate: pre-anthropogenic perspective from bivalve shell growth increments and tree-rings.

TL;DR: Despite strong correlation during historical time, palaeoecological evidence suggests that marine and terrestrial ecosystems may show dissimilar growth reaction to recently observed positive winter-NAO phases.
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Shell Growth History of Geoduck Clam (Panopea abrupta) in Parry Passage, British Columbia, Canada: Temporal Variation in Annuli and the Pacific Decadal Oscillation

TL;DR: In this article, an assemblage of geoduck clam shells from the marine environment of coastal British Columbia was studied and the widths of internal shell growth increments, annuli, were measured from the hinge plate.
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Late Holocene climatic variability reconstructed from incremental data from pines and pearl mussels - a multi-proxy comparison of air and subsurface temperatures

TL;DR: Helama et al. as mentioned in this paper presented a multi-proxy reconstruction of temperature histories using a combination of dendrochronological and sclerochronological evidence, and the reconstruction correlated well with the long records of instrumental temperatures from Tornedalen, St. Petersburg, Uppsala and Stockholm.