The global Hangenberg Crisis (Devonian–Carboniferous transition): review of a first-order mass extinction
Abstract The global Hangenberg Crisis near the Devonian–Carboniferous boundary (DCB)
represents a mass extinction that is of the same scale as the so-called 'Big Five'first-order …
represents a mass extinction that is of the same scale as the so-called 'Big Five'first-order …
From greenhouse to icehouse; organic-walled dinoflagellate cysts as paleoenvironmental indicators in the Paleogene
Dinoflagellates are an important component of the extant eukaryotic plankton. Their organic-
walled, hypnozygotic cysts (dinocysts) provide a rich, albeit incomplete, history of the group …
walled, hypnozygotic cysts (dinocysts) provide a rich, albeit incomplete, history of the group …
Significant Southern Ocean warming event in the late middle Eocene
A prominent middle Eocene warming event is identified in Southern Ocean deep-sea cores,
indicating that long-term cooling through the middle and late Eocene was not monotonic. At …
indicating that long-term cooling through the middle and late Eocene was not monotonic. At …
Middle Eocene–late Oligocene climate variability: calcareous nannofossil response at Kerguelen Plateau, Site 748
A major deterioration in global climate occurred through the Eocene–Oligocene time
interval, characterized by long-term cooling in both terrestrial and marine environments …
interval, characterized by long-term cooling in both terrestrial and marine environments …
Step-wise change of Asian interior climate preceding the Eocene–Oligocene Transition (EOT)
Understanding the global climate change from greenhouse to icehouse conditions at the
Eocene–Oligocene Transition (EOT) 34millionyears ago requires climatic records from …
Eocene–Oligocene Transition (EOT) 34millionyears ago requires climatic records from …
The evolution of western Scandinavian topography: a review of Neogene uplift versus the ICE (isostasy–climate–erosion) hypothesis
Tectonics and erosion are the driving forces in the evolution of mountain belts, but the
identification of their relative contributions remains a fundamental scientific problem in …
identification of their relative contributions remains a fundamental scientific problem in …
The Eocene–oligocene transition
HK Coxall, PN Pearson - 2007 - pubs.geoscienceworld.org
A diverse array of fossil, geochemical and sedimentary data shows patterns of major change
at or near the Eocene–Oligocene boundary, indicating a period of fundamental climatic and …
at or near the Eocene–Oligocene boundary, indicating a period of fundamental climatic and …
Patterns of Phanerozoic reef crises
E Flügel, W Kiessling - 2002 - pubs.geoscienceworld.org
The global carbonate production of reefs is applied as a measure of the health of the reef
ecosystem in a given time interval. Hence global reef crises are defined as significant drops …
ecosystem in a given time interval. Hence global reef crises are defined as significant drops …
[HTML][HTML] Modelling evidence for late Eocene Antarctic glaciations
It is generally believed that a large scale Antarctic ice sheet formed at the Eocene-Oligocene
transition (34.44-33.65 Ma). However, oxygen isotope excursions during the late Eocene (38 …
transition (34.44-33.65 Ma). However, oxygen isotope excursions during the late Eocene (38 …
The Eocene–Oligocene transition: Changes in sea level, temperature or both?
AJP Houben, CA van Mourik, A Montanari… - Palaeogeography …, 2012 - Elsevier
The Eocene–Oligocene Transition (EOT~ 34Ma) reflects the onset of major Antarctic
glaciation. The primary geochemical signature of the EOT is two~ 300kyr spaced shifts in …
glaciation. The primary geochemical signature of the EOT is two~ 300kyr spaced shifts in …