Deciphering the Variability in Mg/Ca and Stable Oxygen Isotopes of Individual Foraminifera.

Mg/Ca climate variability individual foraminifer analyses planktic foraminifera δ18O

Journal

Paleoceanography and paleoclimatology
ISSN: 2572-4525
Titre abrégé: Paleoceanogr Paleoclimatol
Pays: United States
ID NLM: 101736509

Informations de publication

Date de publication:
May 2019
Historique:
received: 30 11 2018
revised: 10 03 2019
accepted: 15 03 2019
entrez: 20 8 2019
pubmed: 20 8 2019
medline: 20 8 2019
Statut: ppublish

Résumé

Foraminifera are commonly used in paleoclimate reconstructions as they occur throughout the world's oceans and are often abundantly preserved in the sediments. Traditionally, foraminifera-based proxies like δ

Identifiants

pubmed: 31423481
doi: 10.1029/2018PA003533
pii: PALO20716
pmc: PMC6686659
doi:

Types de publication

Journal Article

Langues

eng

Pagination

755-773

Références

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pubmed: 31423481
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Auteurs

Jeroen Groeneveld (J)

Alfred Wegener Institute Helmholtz Center for Polar and Marine Research Potsdam Germany.
MARUM-Center for Marine Environmental Sciences University of Bremen Bremen Germany.

Sze Ling Ho (SL)

Alfred Wegener Institute Helmholtz Center for Polar and Marine Research Potsdam Germany.
Now at Institute of Oceanography National Taiwan University Taipei Taiwan.

Andreas Mackensen (A)

Alfred Wegener Institute Helmholtz Center for Polar and Marine Research Bremerhaven Germany.

Mahyar Mohtadi (M)

MARUM-Center for Marine Environmental Sciences University of Bremen Bremen Germany.

Thomas Laepple (T)

Alfred Wegener Institute Helmholtz Center for Polar and Marine Research Potsdam Germany.

Classifications MeSH