The principal paleoceanographic objective of Ocean Drilling Program Leg 115 was to collect a suite of materials that would allow reconstruction of the dynamic features of the late Cenozoic carbonate system in the equatorial Indian Ocean. This goal was achieved with the recovery of sediments from a closely spaced depth transect (1541-4428 m) of five sites (Sites 707 through 711) from on and around the Mascarene Plateau that record the last 50 m.y. of pelagic deposition. More than 2200 measurements of carbonate content are combined here with a highly resolved bio- and magnetostratigraphy to produce the first detailed compilation of bulk, carbonate, and noncarbonate mass accumulation rates (MARs) from the Indian Ocean. These results allow us t...
International audienceThe Cretaceous/Paleogene (K/Pg) boundary is one of the most important mass ext...
Major variations in global carbon cycling occurred between 62 and 48 Ma, and these very likely relat...
I have compiled CaCO3 mass accumulation rates (MARs) for the period 0–25 Ma for 144 Deep Sea Drillin...
The chronostratigraphy, the calcareous nannofossil biochronology, and the biostratigraphy of the Mio...
In the eastern and central Pacific Ocean the most profound change in Neogene calcium carbonate depos...
International audienceWe integrate benthic foraminiferal stable isotopes, X-ray fluorescence element...
International audienceWe integrate benthic foraminiferal stable isotopes, X-ray fluorescence element...
International audienceWe integrate benthic foraminiferal stable isotopes, X-ray fluorescence element...
International audienceWe integrate benthic foraminiferal stable isotopes, X-ray fluorescence element...
Carbonate sediments were studied from two deep sea cores. A suite of samples spanning from the middl...
International audienceWe integrate benthic foraminiferal stable isotopes, X-ray fluorescence element...
International audienceThe Cretaceous/Paleogene (K/Pg) boundary is one of the most important mass ext...
International audienceThe Cretaceous/Paleogene (K/Pg) boundary is one of the most important mass ext...
International audienceThe Cretaceous/Paleogene (K/Pg) boundary is one of the most important mass ext...
Major variations in global carbon cycling occurred between 62 and 48 Ma, and these very likely rela...
International audienceThe Cretaceous/Paleogene (K/Pg) boundary is one of the most important mass ext...
Major variations in global carbon cycling occurred between 62 and 48 Ma, and these very likely relat...
I have compiled CaCO3 mass accumulation rates (MARs) for the period 0–25 Ma for 144 Deep Sea Drillin...
The chronostratigraphy, the calcareous nannofossil biochronology, and the biostratigraphy of the Mio...
In the eastern and central Pacific Ocean the most profound change in Neogene calcium carbonate depos...
International audienceWe integrate benthic foraminiferal stable isotopes, X-ray fluorescence element...
International audienceWe integrate benthic foraminiferal stable isotopes, X-ray fluorescence element...
International audienceWe integrate benthic foraminiferal stable isotopes, X-ray fluorescence element...
International audienceWe integrate benthic foraminiferal stable isotopes, X-ray fluorescence element...
Carbonate sediments were studied from two deep sea cores. A suite of samples spanning from the middl...
International audienceWe integrate benthic foraminiferal stable isotopes, X-ray fluorescence element...
International audienceThe Cretaceous/Paleogene (K/Pg) boundary is one of the most important mass ext...
International audienceThe Cretaceous/Paleogene (K/Pg) boundary is one of the most important mass ext...
International audienceThe Cretaceous/Paleogene (K/Pg) boundary is one of the most important mass ext...
Major variations in global carbon cycling occurred between 62 and 48 Ma, and these very likely rela...
International audienceThe Cretaceous/Paleogene (K/Pg) boundary is one of the most important mass ext...
Major variations in global carbon cycling occurred between 62 and 48 Ma, and these very likely relat...
I have compiled CaCO3 mass accumulation rates (MARs) for the period 0–25 Ma for 144 Deep Sea Drillin...