Stable Oxygen Isotope Composition Is Biased by Shell Calcification Intensity in Planktonic Foraminifera

Author:

Weinkauf M. F. G.12ORCID,Groeneveld J.3ORCID,Waniek J. J.4ORCID,Vennemann T.5ORCID,Martini R.1ORCID

Affiliation:

1. Department of Earth Sciences University of Geneva Geneva Switzerland

2. Now at Institute of Geology and Palaeontology Charles University Prague Czech Republic

3. Helmholtz‐Center for Polar and Marine Sciences Alfred Wegener Institute Potsdam Germany

4. Marine Chemistry Section Leibniz Institute for Baltic Sea Research Warnemünde Rostock Germany

5. Faculty of Geosciences and Environment University of Lausanne Lausanne Switzerland

Funder

Deutsche Forschungsgemeinschaft

Palaeontological Association

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Atmospheric Science,Oceanography

Reference150 articles.

1. A new look at the statistical model identification

2. Calcification in the planktonic foraminifera <i>Globigerina bulloides</i> linked to phosphate concentrations in surface waters of the North Atlantic Ocean

3. Amante C. &Eakins B. W.(2009).ETOPO1 1 arc‐minute global relief model: Procedures data sources and analysis(NESDIS NGDC‐24). National Geophysical Data Center. http://www.ngdc.noaa.gov/mgg/global/relief/ETOPO1/docs/ETOPO1.pdf

4. A revised taxonomic and phylogenetic concept for the planktonic foraminifer species Globigerinoides ruber based on molecular and morphometric evidence

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