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Stable isotope ratios measured on foraminifera of DSDP Hole 74-525B
This dataset has no description
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Stable isotope ratios measured on foraminifera of DSDP Hole 74-525A
This dataset has no description
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Stable isotopes on benthic foraminifera from Hole 47-397
This dataset has no description
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Stable isotopes on benthic foraminifera from Hole 41-366
This dataset has no description
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Stable isotope ratios measured on benthic foraminifera Planulina wuellerstorf...
This dataset has no description
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Stable isotope ratios measured on benthic foraminifera Planulina wuellerstorf...
This dataset has no description
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Stable isotope ratio of benthic foraminifera from Hole 47-397
This dataset has no description
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Stable isotope ratio of benthic foraminifera from Hole 41-366
This dataset has no description
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Stable isotopes of benthic foraminifera from Site 122-761
Stable isotopes were measured on Cibicidoides mundulus, and Planulina wuellerstorfi where C. mundulus was absent or rare -
Stable isotope ratios measured on foraminifera of DSDPHole 24-237
This dataset has no description
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Stable isotope ratios measured on foraminifera of DSDP Hole 30-289
This dataset has no description
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(Table 8a) Stable isotope ratios of foraminifera in sediment core MD84-527
This dataset has no description
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Stable isotope ratios measured on foraminifera of DSDP Hole 85-574
This dataset has no description
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Sea Surface Temperature estimates and benthic foraminifera stable isotopes fr...
Here, we present a new record of SST for the time interval 30 to 17 Ma derived from the long‐chain alkenone unsaturation ratio uk'37 and TEX 86 at Integrated Ocean Drilling... -
Megasplice of benthic d13C records over the last 35 Ma
We construct a 35 Myr-long d13Cbenthic megasplice, a record that consists of different high-resolution benthic isotope records 'spliced' together. In contrast to existing... -
Eocene-Oligocene paleomagnetic and foraminiferal stable isotopic and Mg/Ca re...
The Eocene-Oligocene transition (EOT) marked the initiation of large-scale Antarctic glaciation. This fundamental change in Cenozoic climate state is recorded in deep-sea... -
Late Maastrichtian-early Paleocene benthic stable carbon and oxygen isotope r...
The late Maastrichtian warming event was defined by a global temperature increase of about 2.5-5°C, which occurred ~150-300 kyr before the K/Pg (Cretaceous/Paleogene) mass... -
Miocene stable isotope record of benthic foraminifera from IODP Site 320-U1336
Stable carbon and oxygen isotopes (d13C and d18O) of foraminiferal tests are amongst the most important tools in paleoceanography but the extent to which recrystallization can... -
(Table 1) Stable isotope record of Middle Cretaceous benthic foraminifera
Preservation of planktic foraminiferal calcite has received widespread attention in recent years, but the taphonomy of benthic foraminiferal calcite and its influence on the... -
(Table 1) Age determination of ODP Hole 146-893A
To better understand the deglacial upwelling pattern in the east Pacific, we have made radiocarbon (14C) measurements on benthic foraminifera and macrofauna from a 3.5 m long...