Antarctic palaeoclimate evolution and vegetation history after the formation of a continent-scale cryosphere at the Eocene-Oligocene boundary, 33.9 million years ago, has remained a matter of controversy. In particular, the reconstruction of terrestrial climate and vegetation has been strongly hampered by uncertainties in unambiguously identifying non-reworked as opposed to reworked sporomorphs that have been transported into Antarctic marine sedimentary records by waxing and waning ice sheets. Whereas reworked sporomorph grains over longer non-successive geological timescales are easily identifiable within younger sporomorph assemblages (e.g. Permian sporomorphs in Pliocene sediments), distinguishing non-reworked from reworked material in ...
During the Cenozoic Era (the last 65 Ma), Antarctica’s climate has evolved from ice free conditions ...
During IODP Expedition 318 (January–March 2010, Wellington to Hobart), ~2000 m of Eocene to Quatern...
International audienceThe possible causes of the onset of Antarctic glaciation around the Eocene-Oli...
Antarctic palaeoclimate evolution and vegetation history after the formation of a continent-scale cr...
The question whether Pliocene climates were warm enough to support a substantial vegetation cover on...
Significant climate and vegetation changes have occurred during the Cenozoic era (66 Ma - present), ...
The Eocene-Oligocene transition (EOT) marks the onset of Antarctic glaciation at 33.7 Ma. Although t...
The early Eocene epoch was characterized by extreme global warmth, which in terrestrial settings was...
Diverse pollen and spore assemblages, spanning the Late Eocene preglacial-glacial transition, have b...
The Antarctic region has significantly influenced global climate throughout the Cenozoic. In order t...
The Cenozoic Era is one of the most intriguing periods in Earth\u2019s geological, climatic and biol...
Twenty-three core catcher samples from Site 1166 (Hole 1166A) in Prydz Bay were analyzed for their p...
The early Eocene epoch was characterized by extreme global warmth, which in terrestrial settings was...
The Eocene – Oligocene transition (EOT; ca. 34–33.5 Ma) is widely considered to be the biggest step ...
During the Cenozoic Era (the last 65 Ma), Antarctica’s climate has evolved from ice free conditions ...
During IODP Expedition 318 (January–March 2010, Wellington to Hobart), ~2000 m of Eocene to Quatern...
International audienceThe possible causes of the onset of Antarctic glaciation around the Eocene-Oli...
Antarctic palaeoclimate evolution and vegetation history after the formation of a continent-scale cr...
The question whether Pliocene climates were warm enough to support a substantial vegetation cover on...
Significant climate and vegetation changes have occurred during the Cenozoic era (66 Ma - present), ...
The Eocene-Oligocene transition (EOT) marks the onset of Antarctic glaciation at 33.7 Ma. Although t...
The early Eocene epoch was characterized by extreme global warmth, which in terrestrial settings was...
Diverse pollen and spore assemblages, spanning the Late Eocene preglacial-glacial transition, have b...
The Antarctic region has significantly influenced global climate throughout the Cenozoic. In order t...
The Cenozoic Era is one of the most intriguing periods in Earth\u2019s geological, climatic and biol...
Twenty-three core catcher samples from Site 1166 (Hole 1166A) in Prydz Bay were analyzed for their p...
The early Eocene epoch was characterized by extreme global warmth, which in terrestrial settings was...
The Eocene – Oligocene transition (EOT; ca. 34–33.5 Ma) is widely considered to be the biggest step ...
During the Cenozoic Era (the last 65 Ma), Antarctica’s climate has evolved from ice free conditions ...
During IODP Expedition 318 (January–March 2010, Wellington to Hobart), ~2000 m of Eocene to Quatern...
International audienceThe possible causes of the onset of Antarctic glaciation around the Eocene-Oli...