Review and revision of Cenozoic tropical planktonic foraminiferal biostratigraphy and calibration to the geomagnetic polarity and astronomical time scale
Planktonic foraminifera are widely utilized for the biostratigraphy of Cretaceous and
Cenozoic marine sediments and are a fundamental component of Cenozoic …
Cenozoic marine sediments and are a fundamental component of Cenozoic …
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 …
Middle Miocene climate cooling linked to intensification of eastern equatorial Pacific upwelling
Abstract During the Middle Miocene, Earth's climate transitioned from a relatively warm
phase (Miocene climatic optimum) to a colder mode with reestablishment of permanent ice …
phase (Miocene climatic optimum) to a colder mode with reestablishment of permanent ice …
Stratigraphic continuity and fragmentary sedimentation: the success of cyclostratigraphy as part of integrated stratigraphy
The Milankovitch theory of climate change is widely accepted, but the registration of the
climate changes in the stratigraphic record and their use in building high-resolution …
climate changes in the stratigraphic record and their use in building high-resolution …
In situ Strontium isotope stratigraphy of fish teeth in deep-sea sediments from the western Clarion-Clipperton Fracture Zone, eastern Pacific Ocean
T Wang, Y Dong, F Chu, W Zhang, X Li, R Su, L Tian - Chemical Geology, 2023 - Elsevier
The geochronology of deep-sea sediments beneath the carbonate compensation depth
(CCD) presents a challenge due to the calcareous microfossils dissolution, low …
(CCD) presents a challenge due to the calcareous microfossils dissolution, low …
Eccentricity pacing of eastern equatorial Pacific carbonate dissolution cycles during the Miocene Climatic Optimum
Abstract The Miocene Climatic Optimum (MCO;~ 16.9 to 14.7 Ma) provides an outstanding
opportunity to investigate climate‐carbon cycle dynamics during a geologically recent …
opportunity to investigate climate‐carbon cycle dynamics during a geologically recent …
The middle to late Miocene “Carbonate Crash” in the equatorial Indian Ocean
J Lübbers, W Kuhnt, AE Holbourn… - Paleoceanography …, 2019 - Wiley Online Library
We integrate benthic foraminiferal stable isotopes, X‐ray fluorescence elemental ratios, and
carbonate accumulation estimates in a continuous sedimentary archive recovered at …
carbonate accumulation estimates in a continuous sedimentary archive recovered at …
Testing the impact of diagenesis on the δ18O and δ13C of benthic foraminiferal calcite from a sediment burial depth transect in the equatorial Pacific
Stable oxygen and carbon isotope (δ18O and δ13C) values measured in foraminiferal
calcite are one of the primary tools used in paleoceanography. Diagenetic recrystallization …
calcite are one of the primary tools used in paleoceanography. Diagenetic recrystallization …
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 …
Changes in sea-surface conditions in the Equatorial Pacific during the middle Miocene–Pliocene as inferred from coccolith geochemistry
This study presents a new alkenone-derived Sea Surface Temperature (SST) record and
δ18ONoelaerhabdaceae data of the 2–5μm carbonate fractions from the IODP site U1338 …
δ18ONoelaerhabdaceae data of the 2–5μm carbonate fractions from the IODP site U1338 …