High-resolution analyses of an early Holocene climate event may imply decreased solar forcing as an important climate trigger
Early Holocene lacustrine, tree-ring, ice-core, and marine records reveal that the Northern
Hemisphere underwent a short cooling event at 10 300 calendar yr BP (9100 14C yr BP) …
Hemisphere underwent a short cooling event at 10 300 calendar yr BP (9100 14C yr BP) …
Anomalous shifts in tropical Pacific planktonic and benthic foraminiferal test size during the Paleocene–Eocene thermal maximum
K Kaiho, K Takeda, MR Petrizzo, JC Zachos - Palaeogeography …, 2006 - Elsevier
Paleocene–Eocene warming and changes in oceanic hydrography should have significantly
impacted the ecology of marine microorganisms, both at the surface and on the seafloor. We …
impacted the ecology of marine microorganisms, both at the surface and on the seafloor. We …
High‐resolution (104 years) deep‐sea foraminiferal stable isotope records of the Eocene‐Oligocene climate transition
We have constructed high‐resolution (104–105 years) benthic foraminiferal δ13C and δ18O
records for the upper Eocene through lower Oligocene of two pelagic sequences, Deep Sea …
records for the upper Eocene through lower Oligocene of two pelagic sequences, Deep Sea …
Pleistocene extinctions of deep‐sea benthic foraminifera: The South Atlantic record
TA O'neill, BW Hayward, S Kawagata, AT Sabaa… - …, 2007 - Wiley Online Library
Sixty‐two species and 19 genera of elongate, cylindrical benthic foraminifera disappeared
from the deep‐sea in the south‐east Atlantic (ODP Sites 1082 and 1083) and the Atlantic …
from the deep‐sea in the south‐east Atlantic (ODP Sites 1082 and 1083) and the Atlantic …
Atlantic Ocean thermohaline circulation of the last 150,000 years: Relationship to climate and atmospheric CO2
DW Oppo, RG Fairbanks - Paleoceanography, 1990 - Wiley Online Library
The high‐resolution δ18O and δ13C records of benthic foraminifera from a 150,000‐year
long core from the Caribbean Sea indicate that there was generally high δ13C during …
long core from the Caribbean Sea indicate that there was generally high δ13C during …
Sub sea surface temperatures in the Polar North Atlantic during the Holocene: Planktic foraminiferal Mg/Ca temperature reconstructions
S Aagaard-Sørensen, K Husum, M Hald… - The …, 2014 - journals.sagepub.com
Holocene sea surface temperatures in the eastern Fram Strait are reconstructed based on
Mg/Ca ratios measured on the planktic foraminifer Neogloboquadrina pachyderma (sin) …
Mg/Ca ratios measured on the planktic foraminifer Neogloboquadrina pachyderma (sin) …
The development of a long‐range foraminifer transfer function and application to late Pleistocene North Atlantic climatic extremes
HJ Dowsett - Paleoceanography, 1991 - Wiley Online Library
North Atlantic transfer function GSF18 was developed from simplified core top planktic
foraminifer census data. Simplifications are based upon similar environmental responses of …
foraminifer census data. Simplifications are based upon similar environmental responses of …
The Paleocene–Eocene thermal maximum: new data on microfossil turnover at the Zumaia section, Spain
L Alegret, S Ortiz, X Orue-Etxebarria… - …, 2009 - pubs.geoscienceworld.org
The benthic foraminiferal turnover and extinction event (BEE) associated with the negative
carbon isotope excursion (CIE) across the Paleocene–Eocene Thermal Maximum (PETM) is …
carbon isotope excursion (CIE) across the Paleocene–Eocene Thermal Maximum (PETM) is …
Planktic foraminiferal turnover across the Paleocene-Eocene transition at DSDP site 401, Bay of Biscay, North Atlantic
Planktic foraminifera across the Paleocene-Eocene transition at DSDP Site 401 indicate that
the benthic foraminiferal mass extinction occurred within Subzone P 6a of Berggren and …
the benthic foraminiferal mass extinction occurred within Subzone P 6a of Berggren and …
Closure of the Bering Strait caused mid-Pleistocene transition cooling
Abstract The Mid-Pleistocene Transition (MPT) is characterised by cooling and lengthening
glacial cycles from 600–1200 ka, thought to be driven by reductions in glacial CO2 in …
glacial cycles from 600–1200 ka, thought to be driven by reductions in glacial CO2 in …