Variability in climate and productivity during the Paleocene–Eocene Thermal Maximum in the western Tethys (Forada section)
- Standort
-
Deutsche Nationalbibliothek Frankfurt am Main
- Umfang
-
Online-Ressource
- Sprache
-
Englisch
- Erschienen in
-
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
- Urheber
-
Giusberti, L.
Boscolo Galazzo, F.
Thomas, E.
- DOI
-
10.5194/cp-12-213-2016
- URN
-
urn:nbn:de:101:1-2017102712341
- Rechteinformation
-
Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Letzte Aktualisierung
-
15.08.2025, 07:30 MESZ
Datenpartner
Dieses Objekt wird bereitgestellt von:
Deutsche Nationalbibliothek. Bei Fragen zum Objekt wenden Sie sich bitte an den Datenpartner.
Deutsche Nationalbibliothek. Bei Fragen zum Objekt wenden Sie sich bitte an den Datenpartner.
Beteiligte
- Giusberti, L.
- Boscolo Galazzo, F.
- Thomas, E.
Ähnliche Objekte (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