Tropical Atlantic Climate and Ecosystem Regime Shifts during the Paleocene-Eocene Thermal Maximum
- Standort
-
Deutsche Nationalbibliothek Frankfurt am Main
- Umfang
-
Online-Ressource
- Sprache
-
Englisch
- Erschienen in
-
Tropical Atlantic Climate and Ecosystem Regime Shifts during the Paleocene-Eocene Thermal Maximum ; year:2017 ; pages:1-23
Climate of the past discussions ; (2017), 1-23
- Urheber
-
Frieling, Joost
Reichart, Gert-Jan
Middelburg, Jack J.
Röhl, Ursula
Westerhold, Thomas
Bohaty, Steven M.
Sluijs, Appy
- DOI
-
10.5194/cp-2017-76
- URN
-
urn:nbn:de:101:1-2017102716146
- Rechteinformation
-
Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Letzte Aktualisierung
-
15.08.2025, 07:34 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
- Frieling, Joost
- Reichart, Gert-Jan
- Middelburg, Jack J.
- Röhl, Ursula
- Westerhold, Thomas
- Bohaty, Steven M.
- Sluijs, Appy
Ähnliche Objekte (12)
Tropical Atlantic climate and ecosystem regime shifts during the Paleocene–Eocene Thermal Maximum
Mercury anomalies across the Palaeocene-Eocene Thermal Maximum
Ecosystem Shifts: Implications for Groundwater Management
Revisiting carbonate chemistry controls on planktic foraminifera Mg / Ca: implications for sea surface temperature and hydrology shifts over the Paleocene–Eocene Thermal Maximum and Eocene–Oligocene transition
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
Ecosystem damage by increasing tropical cyclones
Response of coastal California hydroclimate to the Paleocene–Eocene Thermal Maximum
Productivity response of calcareous nannoplankton to Eocene Thermal Maximum 2 (ETM2)
Shallow-water hydrothermal venting linked to the Palaeocene–Eocene Thermal Maximum
Response of Coastal California Hydroclimate to the Paleocene-Eocene Thermal Maximum
Tropical Atlantic climate and ecosystem regime shifts during the Paleocene–Eocene Thermal Maximum
Mercury anomalies across the Palaeocene-Eocene Thermal Maximum
Ecosystem Shifts: Implications for Groundwater Management
Revisiting carbonate chemistry controls on planktic foraminifera Mg / Ca: implications for sea surface temperature and hydrology shifts over the Paleocene–Eocene Thermal Maximum and Eocene–Oligocene transition
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
Ecosystem damage by increasing tropical cyclones
Response of coastal California hydroclimate to the Paleocene–Eocene Thermal Maximum
Productivity response of calcareous nannoplankton to Eocene Thermal Maximum 2 (ETM2)
Shallow-water hydrothermal venting linked to the Palaeocene–Eocene Thermal Maximum
Response of Coastal California Hydroclimate to the Paleocene-Eocene Thermal Maximum
Tropical Atlantic climate and ecosystem regime shifts during the Paleocene–Eocene Thermal Maximum
Mercury anomalies across the Palaeocene-Eocene Thermal Maximum
Ecosystem Shifts: Implications for Groundwater Management
Revisiting carbonate chemistry controls on planktic foraminifera Mg / Ca: implications for sea surface temperature and hydrology shifts over the Paleocene–Eocene Thermal Maximum and Eocene–Oligocene transition
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
Ecosystem damage by increasing tropical cyclones
Response of coastal California hydroclimate to the Paleocene–Eocene Thermal Maximum
Productivity response of calcareous nannoplankton to Eocene Thermal Maximum 2 (ETM2)
Shallow-water hydrothermal venting linked to the Palaeocene–Eocene Thermal Maximum