Preservation of benthic foraminifera and reliability of deep‐sea temperature records: Importance of sedimentation rates, lithology, and the need to examine test wall …
Preservation of planktic foraminiferal calcite has received widespread attention in recent
years, but the taphonomy of benthic foraminiferal calcite and its influence on the deep‐sea …
years, but the taphonomy of benthic foraminiferal calcite and its influence on the deep‐sea …
North Atlantic warming during global cooling at the end of the Cretaceous
KG MacLeod, BT Huber, C Isaza-Londoño - Geology, 2005 - pubs.geoscienceworld.org
Differences in regional responses to climate fluctuations are well documented on short time
scales (eg, El Niño–Southern Oscillation), but with the exception of latitudinal temperature …
scales (eg, El Niño–Southern Oscillation), but with the exception of latitudinal temperature …
Episodes of intensified biological productivity in the subtropical Atlantic Ocean during the termination of the Middle Eocene Climatic Optimum (MECO)
I Moebius, O Friedrich, KM Edgar… - Paleoceanography, 2015 - Wiley Online Library
Abstract The Middle Eocene Climatic Optimum (MECO) is an~ 500 kyr interval of
pronounced global warming from which the climate system recovered in< 50 kyr. The deep …
pronounced global warming from which the climate system recovered in< 50 kyr. The deep …
Constraining multiple controls on planktic foraminifera Mg/Ca
Abstract The Mg/Ca of planktic foraminifera is widely used to determine past surface ocean
temperatures but temperature is not the only factor that controls test Mg/Ca. Here we quantify …
temperatures but temperature is not the only factor that controls test Mg/Ca. Here we quantify …
Response of deep ocean circulation to initiation of Northern Hemisphere glaciation (3–2 Ma)
Carbon isotopic records from benthic foraminifera are used to map patterns of deep ocean
circulation between 3 and 2 million years ago, the interval when significant northern …
circulation between 3 and 2 million years ago, the interval when significant northern …
Higher temperatures and lower oceanic pCO2: A climate enigma at the end of the Paleocene Epoch
LD Stott - Paleoceanography, 1992 - Wiley Online Library
One of the largest and most abrupt climatic warming events documented in the geologic
record occurred at the end of the Paleocene epoch. Oceanic deep waters warmed to 10° C …
record occurred at the end of the Paleocene epoch. Oceanic deep waters warmed to 10° C …
Orbitally paced carbon and deep‐sea temperature changes at the peak of the Early Eocene Climatic Optimum
V Lauretano, JC Zachos… - Paleoceanography and …, 2018 - Wiley Online Library
The late Paleocene to early Eocene warming trend was punctuated by a series of orbitally
paced transient warming events, associated with the release of isotopically light carbon into …
paced transient warming events, associated with the release of isotopically light carbon into …
Holocene trends in the foraminifer record from the Norwegian Sea and the North Atlantic Ocean
The early to mid-Holocene thermal optimum is a well-known feature in a wide variety of
paleoclimate archives from the Northern Hemisphere. Reconstructed summer temperature …
paleoclimate archives from the Northern Hemisphere. Reconstructed summer temperature …
Paleocene planktonic foraminiferal biogeography and the paleooceanography of the Atlantic Ocean
A Boersma, IP Silva - Micropaleontology, 1983 - JSTOR
The spatial and temporal distributions of organisms reflect the gradients and dynamics of
that system we call climate. To describe such relationships for the Paleocene, quantitative …
that system we call climate. To describe such relationships for the Paleocene, quantitative …
Repeated near‐collapse of the Pliocene sea surface temperature gradient in the North Atlantic
Sea surface temperature (SST) is used to infer past changes in the state of the climate
system. Here we use a combination of newly generated and published organic …
system. Here we use a combination of newly generated and published organic …