Multiple early Eocene benthic foraminiferal assemblage and δ13C fluctuations at DSDP Site 401 (Bay of Biscay—NE Atlantic)
Within the last decade, several early Eocene hyperthermals have been detected globally.
These transient warming events have mainly been characterized geochemically–using …
These transient warming events have mainly been characterized geochemically–using …
Moving beyond the age–depth model paradigm in deep-sea palaeoclimate archives: dual radiocarbon and stable isotope analysis on single foraminifera
Late-glacial palaeoclimate reconstructions from deep-sea sediment archives provide
valuable insight into past rapid changes in ocean chemistry. Unfortunately, only a small …
valuable insight into past rapid changes in ocean chemistry. Unfortunately, only a small …
Breathing more deeply: Deep ocean carbon storage during the mid-Pleistocene climate transition
The∼ 100 ky cyclicity of the late Pleistocene ice ages started during the mid-Pleistocene
transition (MPT), as ice sheets became larger and persisted for longer. The climate system …
transition (MPT), as ice sheets became larger and persisted for longer. The climate system …
A high‐Fidelity benthic stable isotope record of late Cretaceous–early Eocene climate change and carbon‐cycling
Abstract The Late Cretaceous–Early Paleogene is the most recent period in Earth history
that experienced sustained global greenhouse warmth on multimillion year timescales. Yet …
that experienced sustained global greenhouse warmth on multimillion year timescales. Yet …
Global change across the Oligocene‐Miocene transition: High‐resolution stable isotope records from IODP Site U1334 (equatorial Pacific Ocean)
Abstract The Oligocene‐Miocene transition (OMT)(~ 23 Ma) is interpreted as a transient
global cooling event, associated with a large‐scale Antarctic ice sheet expansion. Here we …
global cooling event, associated with a large‐scale Antarctic ice sheet expansion. Here we …
Deep water temperature, carbonate ion, and ice volume changes across the Eocene‐Oligocene climate transition
AE Pusz, RC Thunell, KG Miller - Paleoceanography, 2011 - Wiley Online Library
Paired benthic foraminiferal stable isotope and Mg/Ca data are used to estimate bottom
water temperature (BWT) and ice volume changes associated with the Eocene‐Oligocene …
water temperature (BWT) and ice volume changes associated with the Eocene‐Oligocene …
Ocean overturning since the Late Cretaceous: Inferences from a new benthic foraminiferal isotope compilation
Benthic foraminiferal oxygen isotopic (δ18O) and carbon isotopic (δ13C) trends, constructed
from compilations of data series from multiple ocean sites, provide one of the primary means …
from compilations of data series from multiple ocean sites, provide one of the primary means …
Orbital climate forcing of δ13C excursions in the late Paleocene–early Eocene (chrons C24n–C25n)
High‐resolution stable carbon isotope records for upper Paleocene–lower Eocene sections
at Ocean Drilling Program Sites 1051 and 690 and Deep Sea Drilling Project Sites 550 and …
at Ocean Drilling Program Sites 1051 and 690 and Deep Sea Drilling Project Sites 550 and …
Global perturbation of the carbon cycle at the onset of the Miocene Climatic Optimum
Abstract The Miocene Climatic Optimum (MCO; ca. 17–14.7 Ma) represents one of several
major interruptions in the long-term cooling trend of the past 50 my To date, the processes …
major interruptions in the long-term cooling trend of the past 50 my To date, the processes …