This table includes temperatures calculated from carbonate clumped isotope measurements performed on middle Miocene benthic foraminifera from Ocean Drilling Program (ODP) Hole 120-747A, Kerguelen Plateau, and is an accompaniment to the manuscript "Southern Ocean bottom water cooling and ice sheet expansion during the middle Miocene climate transition", Climate of the Past, submitted. A complete set of individual measurement data, including sample labels, depth and raw mass spectrometer data, can be found on the EarthChem database (Leutert et al., 2021 doi:10.26022/IEDA/111808)
We integrate micropaleontological and geochemical records (benthic stable isotopes, neodymium isotop...
Middle Miocene (14.8–11.9 Ma) deep-sea sediments from ODP Hole 747A (Kerguelen Plateau, southern Ind...
International audienceThe Middle Miocene transition from carbonate to biosilica sedimentation at DSD...
This PhD thesis focuses on the clumped isotope paleothermometer and its application to foraminiferal...
Here we present benthic foraminiferal counts, Mg/Ca-based bottom water temperature (BWT) estimates, ...
The middle Miocene climate transition (MMCT), around 14 Ma, was associated with a significant climat...
The sensitivities of benthic foraminiferal Mg/Ca and Li/Ca to bottom water temperature and carbonate...
The Middle and Late Miocene were associated with a global cooling trend, with the development of a p...
The middle Miocene is an important analogue for potential future warm climates. Unfortunately, relat...
The dataset compiles reconstructed changes in bottom water temperature and global ice volume from 0 ...
Paleoceanographic variability at southern high latitude Ocean Drilling Program (ODP) Site 747 was in...
Changes in intermediate and deep ocean circulation likely played a significant role in global carbon...
High-resolution stable isotopic records are presented for the epi-benthic foraminifer Cibicidoides, ...
The sensitivities of benthic foraminiferal Mg/Ca and Li/Ca to bottom water temperature and carbonate...
Oxygen isotopic compositions of the tests of planktonic foraminifera from several Deep Sea Drilling ...
We integrate micropaleontological and geochemical records (benthic stable isotopes, neodymium isotop...
Middle Miocene (14.8–11.9 Ma) deep-sea sediments from ODP Hole 747A (Kerguelen Plateau, southern Ind...
International audienceThe Middle Miocene transition from carbonate to biosilica sedimentation at DSD...
This PhD thesis focuses on the clumped isotope paleothermometer and its application to foraminiferal...
Here we present benthic foraminiferal counts, Mg/Ca-based bottom water temperature (BWT) estimates, ...
The middle Miocene climate transition (MMCT), around 14 Ma, was associated with a significant climat...
The sensitivities of benthic foraminiferal Mg/Ca and Li/Ca to bottom water temperature and carbonate...
The Middle and Late Miocene were associated with a global cooling trend, with the development of a p...
The middle Miocene is an important analogue for potential future warm climates. Unfortunately, relat...
The dataset compiles reconstructed changes in bottom water temperature and global ice volume from 0 ...
Paleoceanographic variability at southern high latitude Ocean Drilling Program (ODP) Site 747 was in...
Changes in intermediate and deep ocean circulation likely played a significant role in global carbon...
High-resolution stable isotopic records are presented for the epi-benthic foraminifer Cibicidoides, ...
The sensitivities of benthic foraminiferal Mg/Ca and Li/Ca to bottom water temperature and carbonate...
Oxygen isotopic compositions of the tests of planktonic foraminifera from several Deep Sea Drilling ...
We integrate micropaleontological and geochemical records (benthic stable isotopes, neodymium isotop...
Middle Miocene (14.8–11.9 Ma) deep-sea sediments from ODP Hole 747A (Kerguelen Plateau, southern Ind...
International audienceThe Middle Miocene transition from carbonate to biosilica sedimentation at DSD...