Laboratoire des Sciences du Climat et de l'Environnement, LSCE/IPSL,
CEA–CNRS–UVSQ, Université Paris-Saclay, 91191
Gif-sur-Yvette, France
Earth and Climate Cluster, Department of Earth Science, Faculty of
Science, Vrije Universiteit Amsterdam, de Boelelaan 1085, 1081 HV, Amsterdam, the Netherlands
Laboratoire des Sciences du Climat et de l'Environnement, LSCE/IPSL,
CEA–CNRS–UVSQ, Université Paris-Saclay, 91191
Gif-sur-Yvette, France
Earth and Climate Cluster, Department of Earth Science, Faculty of
Science, Vrije Universiteit Amsterdam, de Boelelaan 1085, 1081 HV, Amsterdam, the Netherlands
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2,556
1,033
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3,654
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Total article views: 1,855 (including HTML, PDF, and XML)
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1,401
409
45
1,855
158
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PDF: 409
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Supplement: 158
BibTeX: 36
EndNote: 38
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1,155
624
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Total article views: 3,654 (including HTML, PDF, and XML)
Thereof 3,129 with geography defined
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Total article views: 1,855 (including HTML, PDF, and XML)
Thereof 1,642 with geography defined
and 213 with unknown origin.
Total article views: 1,799 (including HTML, PDF, and XML)
Thereof 1,487 with geography defined
and 312 with unknown origin.
Planktonic foraminifera construct a shell that, post mortem, settles to the seafloor, prior to collection by Palaeoclimatologists for use as proxies. Such organisms in life are sensitive to the ambient conditions (e.g. temperature, salinity), which therefore means our proxies maybe skewed toward the ecology of organisms. Using a proxy system model, Foraminifera as Modelled Entities (FAME), we assess the potential of extracting ENSO signal from tropical Pacific planktonic foraminifera.
Planktonic foraminifera construct a shell that, post mortem, settles to the seafloor, prior to...