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

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Location: Deutsche Nationalbibliothek Frankfurt am Main

Extent: Online-Ressource

Language: Englisch

Bibliographic citation: Variability in climate and productivity during the Paleocene–Eocene Thermal Maximum in the western Tethys (Forada section) ; volume:12 ; number:2 ; year:2016 ; pages:213-240
Climate of the past ; 12, Heft 2 (2016), 213-240

Creator: Giusberti, L.
Boscolo Galazzo, F.
Thomas, E.

DOI: 10.5194/cp-12-213-2016

URN: urn:nbn:de:101:1-2017102712341

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

Last update: 15.08.2025, 7:30 AM CEST

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Associated

Giusberti, L.
Boscolo Galazzo, F.
Thomas, E.

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Modelling the carbon cycle during the Paleocene-Eocene Thermal Maximum

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

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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)

Mercury anomalies across the Palaeocene-Eocene Thermal Maximum

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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

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

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

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

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

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

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

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

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

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

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

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

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

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Other Objects (12)

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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