Cretaceous/Paleogene boundary bathyal paleo-environments in the central North Pacific (DSDP Site 465), the Northwestern Atlantic (ODP Site 1049), the Gulf of …
L Alegret, E Thomas - Palaeogeography, Palaeoclimatology …, 2005 - Elsevier
Uppermost Maastrichtian benthic foraminiferal assemblages (> 63 μm) are diverse,
indicating mesotrophic conditions in lower bathyal DSDP Hole 465A (Hess Rise, central …
indicating mesotrophic conditions in lower bathyal DSDP Hole 465A (Hess Rise, central …
Expanded oxygen minimum zones during the late Paleocene‐early Eocene: Hints from multiproxy comparison and ocean modeling
Anthropogenic warming could well drive depletion of oceanic oxygen in the future. Important
insight into the relationship between deoxygenation and warming can be gleaned from the …
insight into the relationship between deoxygenation and warming can be gleaned from the …
Greenhouse shoreline migration: Wilcox deltas
In contrast to the high-frequency and high-amplitude sea level changes of icehouse times,
eustatic sea level changes in greenhouse times are now generally accepted as significantly …
eustatic sea level changes in greenhouse times are now generally accepted as significantly …
Faunal turnovers in central Pacific benthic foraminifera during the Paleocene–Eocene thermal maximum
K Takeda, K Kaiho - Palaeogeography, Palaeoclimatology, Palaeoecology, 2007 - Elsevier
Although it is well known that the Paleocene/Eocene thermal maximum (PETM) coincided
with a major benthic foraminiferal extinction event, the detailed pattern of the faunal turnover …
with a major benthic foraminiferal extinction event, the detailed pattern of the faunal turnover …
Benthic foraminifera across the Cretaceous/Paleogene boundary in the Southern Ocean (ODP Site 690): Diversity, food and carbonate saturation
L Alegret, E Thomas - Marine Micropaleontology, 2013 - Elsevier
The impact of an asteroid at the Cretaceous/Paleogene (K/Pg) boundary triggered dramatic
biotic, biogeochemical and sedimentological changes in the oceans that have been …
biotic, biogeochemical and sedimentological changes in the oceans that have been …
Middle Eocene through early Oligocene climate history and paleoceanography in the Southern Ocean: Stable oxygen and carbon isotopes from ODP sites on Maud …
A Mackensen, WU Ehrmann - Marine Geology, 1992 - Elsevier
Paleogene stable oxygen and carbon isotopes were measured in formainifera from ODP
Sites 689 and 690 at Maud Rise in the Atlantic Ocean sector of the Southern Ocean, and …
Sites 689 and 690 at Maud Rise in the Atlantic Ocean sector of the Southern Ocean, and …
A view of Antarctic ice-sheet evolution from sea-level and deep-sea isotope changes during the Late Cretaceous–Cenozoic
The imperfect direct record of Antarctic glaciation has led to the delayed recognition of the
initiation of a continentsized ice sheet. Early studies interpreted initiation in the middle …
initiation of a continentsized ice sheet. Early studies interpreted initiation in the middle …
Benthic foraminiferal response to the Middle Eocene climatic optimum (MECO) in the south-eastern Atlantic (ODP Site 1263)
The response of marine biota to the Middle Eocene Climatic Optimum (MECO) is still poorly
constrained. Specifically, changes in deep-sea benthic foraminiferal faunas have been …
constrained. Specifically, changes in deep-sea benthic foraminiferal faunas have been …
The northern Gulf of Mexico during OAE2 and the relationship between water depth and black shale development
Abstract Despite their name, Oceanic Anoxic Events (OAEs) are not periods of uniform
anoxia and black shale deposition in ancient oceans. Shelf environments account for the …
anoxia and black shale deposition in ancient oceans. Shelf environments account for the …
Middle Eocene to early Oligocene paleoceanography of the Antarctic Ocean (Maud Rise, ODP Leg 113, Site 689): change from a low to a high productivity ocean
L Diester-Haass - Palaeogeography, Palaeoclimatology, Palaeoecology, 1995 - Elsevier
The sediment record from the middle Eocene (about 45 Ma) to the early Oligocene (about 33
Ma) on Maud Rise Site 689, Weddell Sea (paleodepth 1400–1650 m), has been studied by …
Ma) on Maud Rise Site 689, Weddell Sea (paleodepth 1400–1650 m), has been studied by …