| Journal Title |
Article Title |
Year |
DOI |
|
Earth-Science Reviews
|
Mantle plumes from top to bottom |
2006
|
10.1016/j.earscirev.2006.03.007
|
|
Geological Society of America Bulletin
|
An Antarctic stratigraphic record of stepwise ice growth through the Eocene-Oligocene transition |
2017
|
10.1130/B31482.1
|
|
Palynology
|
Species of the acritarch genuspalaeostomocystisdeflandre 1937: Potential indicators of neritic subpolar to polar environments in Antarctica during the Cenozoic |
2009
|
10.1080/01916122.2009.9989682
|
|
International Journal of Earth Sciences
|
Clay mineralogy of the ocean sediments from the Wilkes Land margin, east Antarctica: implications on the paleoclimate, provenance and sediment dispersal pattern |
2014
|
10.1007/s00531-014-1043-4
|
|
Paleoceanography
|
Environmental forcings of Paleogene Southern Ocean dinoflagellate biogeography |
2011
|
10.1029/2009PA001905
|
|
Review of Palaeobotany and Palynology
|
Middle Eocene dinoflagellate cysts from Santa Cruz Province, Argentina: Biostratigraphy and paleoenvironment |
2014
|
10.1016/j.revpalbo.2014.09.002
|
|
Geochemistry, Geophysics, Geosystems
|
Early Eocene to middle Miocene cooling and aridification of East Antarctica |
2013
|
10.1002/ggge.20106
|
|
Nature
|
Temperate rainforests near the South Pole during peak Cretaceous warmth |
2020
|
10.1038/s41586-020-2148-5
|
|
Progress in Natural Science
|
Cenozoic terrestrial palynological assemblages in the glacial erratics from the Grove Mountains, east Antarctica |
2009
|
10.1016/j.pnsc.2008.01.040
|
|
Climate of the Past
|
Vegetation change across the Drake Passage region linked to late Eocene cooling and glacial disturbance after the Eocene–Oligocene transition |
2022
|
10.5194/cp-18-209-2022
|
|
Geological Society, London, Special Publications
|
Late Eocene Glaciofluvial to Glaciomarine transition in the Lambert Graben: constraints from lithofacies and mineralogy of ODP Site 1166 sediments, Prydz Bay, Antarctica |
2013
|
10.1144/SP381.24
|
|
Climate of the Past
|
Eocene to Oligocene vegetation and climate in the Tasmanian Gateway region were controlled by changes in ocean currents and <i>p</i>CO<sub>2</sub> |
2022
|
10.5194/cp-18-525-2022
|