Productivity response of calcareous nannoplankton to Eocene Thermal Maximum 2 (ETM2)

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Location: Deutsche Nationalbibliothek Frankfurt am Main

Extent: Online-Ressource

Language: Englisch

Bibliographic citation: Productivity response of calcareous nannoplankton to Eocene Thermal Maximum 2 (ETM2) ; volume:8 ; number:3 ; year:2012 ; pages:977-993
Climate of the past ; 8, Heft 3 (2012), 977-993

Creator: Dedert, M.
Stoll, H. M.
Kroon, D.
Shimizu, N.
Kanamaru, K.
Ziveri, P.

DOI: 10.5194/cp-8-977-2012

URN: urn:nbn:de:101:1-201710276723

Rights: Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.

Last update: 15.08.2025, 7:23 AM CEST

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Associated

Dedert, M.
Stoll, H. M.
Kroon, D.
Shimizu, N.
Kanamaru, K.
Ziveri, P.

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Modelling the carbon cycle during the Paleocene-Eocene Thermal Maximum

Reduced carbon cycle resilience across the Palaeocene–Eocene Thermal Maximum

Reduced Carbon Cycle Resilience across the Palaeocene-Eocene Thermal Maximum

Variability in climate and productivity during the Paleocene–Eocene Thermal Maximum in the western Tethys (Forada section)

Response of coastal California hydroclimate to the Paleocene–Eocene Thermal Maximum

Shallow-water hydrothermal venting linked to the Palaeocene–Eocene Thermal Maximum

Response of Coastal California Hydroclimate to the Paleocene-Eocene Thermal Maximum

Astrochronology of the Paleocene-Eocene Thermal Maximum on the Atlantic Coastal Plain

Tropical Atlantic climate and ecosystem regime shifts during the Paleocene–Eocene Thermal Maximum

Expanded subsurface ocean anoxia in the Atlantic during the Paleocene-Eocene Thermal Maximum

Productivity feedback did not terminate the Paleocene-Eocene Thermal Maximum (PETM)

Mercury anomalies across the Palaeocene-Eocene Thermal Maximum

Hochschulschrift

Modelling the carbon cycle during the Paleocene-Eocene Thermal Maximum

Reduced carbon cycle resilience across the Palaeocene–Eocene Thermal Maximum

Reduced Carbon Cycle Resilience across the Palaeocene-Eocene Thermal Maximum

Variability in climate and productivity during the Paleocene–Eocene Thermal Maximum in the western Tethys (Forada section)

Response of coastal California hydroclimate to the Paleocene–Eocene Thermal Maximum

Shallow-water hydrothermal venting linked to the Palaeocene–Eocene Thermal Maximum

Response of Coastal California Hydroclimate to the Paleocene-Eocene Thermal Maximum

Astrochronology of the Paleocene-Eocene Thermal Maximum on the Atlantic Coastal Plain

Tropical Atlantic climate and ecosystem regime shifts during the Paleocene–Eocene Thermal Maximum

Expanded subsurface ocean anoxia in the Atlantic during the Paleocene-Eocene Thermal Maximum

Productivity feedback did not terminate the Paleocene-Eocene Thermal Maximum (PETM)

Mercury anomalies across the Palaeocene-Eocene Thermal Maximum

Hochschulschrift

Modelling the carbon cycle during the Paleocene-Eocene Thermal Maximum

Reduced carbon cycle resilience across the Palaeocene–Eocene Thermal Maximum

Reduced Carbon Cycle Resilience across the Palaeocene-Eocene Thermal Maximum

Variability in climate and productivity during the Paleocene–Eocene Thermal Maximum in the western Tethys (Forada section)

Response of coastal California hydroclimate to the Paleocene–Eocene Thermal Maximum

Shallow-water hydrothermal venting linked to the Palaeocene–Eocene Thermal Maximum

Response of Coastal California Hydroclimate to the Paleocene-Eocene Thermal Maximum

Astrochronology of the Paleocene-Eocene Thermal Maximum on the Atlantic Coastal Plain

Tropical Atlantic climate and ecosystem regime shifts during the Paleocene–Eocene Thermal Maximum

Expanded subsurface ocean anoxia in the Atlantic during the Paleocene-Eocene Thermal Maximum

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Productivity response of calcareous nannoplankton to Eocene Thermal Maximum 2 (ETM2)

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Other Objects (12)

Productivity feedback did not terminate the Paleocene-Eocene Thermal Maximum (PETM)

Mercury anomalies across the Palaeocene-Eocene Thermal Maximum

Modelling the carbon cycle during the Paleocene-Eocene Thermal Maximum

Reduced carbon cycle resilience across the Palaeocene–Eocene Thermal Maximum

Reduced Carbon Cycle Resilience across the Palaeocene-Eocene Thermal Maximum

Variability in climate and productivity during the Paleocene–Eocene Thermal Maximum in the western Tethys (Forada section)

Response of coastal California hydroclimate to the Paleocene–Eocene Thermal Maximum

Shallow-water hydrothermal venting linked to the Palaeocene–Eocene Thermal Maximum

Response of Coastal California Hydroclimate to the Paleocene-Eocene Thermal Maximum

Astrochronology of the Paleocene-Eocene Thermal Maximum on the Atlantic Coastal Plain

Tropical Atlantic climate and ecosystem regime shifts during the Paleocene–Eocene Thermal Maximum

Expanded subsurface ocean anoxia in the Atlantic during the Paleocene-Eocene Thermal Maximum

Productivity feedback did not terminate the Paleocene-Eocene Thermal Maximum (PETM)

Mercury anomalies across the Palaeocene-Eocene Thermal Maximum

Modelling the carbon cycle during the Paleocene-Eocene Thermal Maximum

Reduced carbon cycle resilience across the Palaeocene–Eocene Thermal Maximum

Reduced Carbon Cycle Resilience across the Palaeocene-Eocene Thermal Maximum

Variability in climate and productivity during the Paleocene–Eocene Thermal Maximum in the western Tethys (Forada section)

Response of coastal California hydroclimate to the Paleocene–Eocene Thermal Maximum

Shallow-water hydrothermal venting linked to the Palaeocene–Eocene Thermal Maximum

Response of Coastal California Hydroclimate to the Paleocene-Eocene Thermal Maximum

Astrochronology of the Paleocene-Eocene Thermal Maximum on the Atlantic Coastal Plain

Tropical Atlantic climate and ecosystem regime shifts during the Paleocene–Eocene Thermal Maximum

Expanded subsurface ocean anoxia in the Atlantic during the Paleocene-Eocene Thermal Maximum

Productivity feedback did not terminate the Paleocene-Eocene Thermal Maximum (PETM)

Mercury anomalies across the Palaeocene-Eocene Thermal Maximum

Modelling the carbon cycle during the Paleocene-Eocene Thermal Maximum

Reduced carbon cycle resilience across the Palaeocene–Eocene Thermal Maximum

Reduced Carbon Cycle Resilience across the Palaeocene-Eocene Thermal Maximum

Variability in climate and productivity during the Paleocene–Eocene Thermal Maximum in the western Tethys (Forada section)

Response of coastal California hydroclimate to the Paleocene–Eocene Thermal Maximum

Shallow-water hydrothermal venting linked to the Palaeocene–Eocene Thermal Maximum

Response of Coastal California Hydroclimate to the Paleocene-Eocene Thermal Maximum

Astrochronology of the Paleocene-Eocene Thermal Maximum on the Atlantic Coastal Plain

Tropical Atlantic climate and ecosystem regime shifts during the Paleocene–Eocene Thermal Maximum

Expanded subsurface ocean anoxia in the Atlantic during the Paleocene-Eocene Thermal Maximum

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