- Standort
-
Deutsche Nationalbibliothek Frankfurt am Main
- Umfang
-
Online-Ressource
- Sprache
-
Englisch
- Erschienen in
-
Investigating vegetation–climate feedbacks during the early Eocene ; volume:10 ; number:2 ; year:2014 ; pages:419-436
Climate of the past ; 10, Heft 2 (2014), 419-436
- Urheber
-
Loptson, C. A.
Lunt, D. J.
Francis, J. E.
- DOI
-
10.5194/cp-10-419-2014
- URN
-
urn:nbn:de:101:1-2017102710157
- Rechteinformation
-
Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Letzte Aktualisierung
-
15.08.2025, 07:26 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
- Loptson, C. A.
- Lunt, D. J.
- Francis, J. E.
Ähnliche Objekte (12)
Vegetation change across the Drake Passage region linked to late Eocene cooling and glacial disturbance after the Eocene–Oligocene Transition
Measuring and modeling water-related soil–vegetation feedbacks in a fallow plot
Middle Eocene greenhouse warming facilitated by diminished weathering feedback
Investigating the feedbacks between CO2, vegetation and the AMOC in a coupled climate model
Late Quaternary vegetation-climate feedbacks
Productivity feedback did not terminate the Paleocene-Eocene Thermal Maximum (PETM)
Vegetation change across the Drake Passage region linked to late Eocene cooling and glacial disturbance after the Eocene–Oligocene transition
Plant functional diversity affects climate–vegetation interaction
Chapitre XVI. Formations éocène moyen et éocène inférieur
Rainfall intermittency and vegetation feedbacks in drylands
Fossil plant stomata indicate decreasing atmospheric CO 2 prior to the Eocene–Oligocene boundary
Tracing North Atlantic volcanism and seaway connectivity across the Paleocene–Eocene Thermal Maximum (PETM)
Vegetation change across the Drake Passage region linked to late Eocene cooling and glacial disturbance after the Eocene–Oligocene Transition
Measuring and modeling water-related soil–vegetation feedbacks in a fallow plot
Middle Eocene greenhouse warming facilitated by diminished weathering feedback
Investigating the feedbacks between CO2, vegetation and the AMOC in a coupled climate model
Late Quaternary vegetation-climate feedbacks
Productivity feedback did not terminate the Paleocene-Eocene Thermal Maximum (PETM)
Vegetation change across the Drake Passage region linked to late Eocene cooling and glacial disturbance after the Eocene–Oligocene transition
Plant functional diversity affects climate–vegetation interaction
Chapitre XVI. Formations éocène moyen et éocène inférieur
Rainfall intermittency and vegetation feedbacks in drylands
Fossil plant stomata indicate decreasing atmospheric CO 2 prior to the Eocene–Oligocene boundary
Tracing North Atlantic volcanism and seaway connectivity across the Paleocene–Eocene Thermal Maximum (PETM)
Vegetation change across the Drake Passage region linked to late Eocene cooling and glacial disturbance after the Eocene–Oligocene Transition
Measuring and modeling water-related soil–vegetation feedbacks in a fallow plot
Middle Eocene greenhouse warming facilitated by diminished weathering feedback
Investigating the feedbacks between CO2, vegetation and the AMOC in a coupled climate model
Late Quaternary vegetation-climate feedbacks
Productivity feedback did not terminate the Paleocene-Eocene Thermal Maximum (PETM)
Vegetation change across the Drake Passage region linked to late Eocene cooling and glacial disturbance after the Eocene–Oligocene transition
Plant functional diversity affects climate–vegetation interaction
Chapitre XVI. Formations éocène moyen et éocène inférieur
Rainfall intermittency and vegetation feedbacks in drylands
Fossil plant stomata indicate decreasing atmospheric CO 2 prior to the Eocene–Oligocene boundary