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Age models for ODPO Leg 130 sites
The Neogene carbonate stratigraphy of five sites drilled on Ontong Java Plateau during Leg 130 reveals a number of patterns which are unexpected, and which we refer to as loss... -
Biomarkers, stable carbon isotope record and pollen distribution of the soutw...
This is part 2 of a study examining southwest African continental margin sediments from nine sites on a north-south transect from the Congo Fan (4°S) to the Cape Basin (30°S)... -
Ice-rafted fossils in ODP LEg 104 Pleistocene-Pliocene sediments
Ice-rafted fossils of late Cretaceous and Tertiary age were detected in Pleistocene-Pliocene glacially influenced sediments of the Vdring Plateau, eastern Norwegian Sea. The... -
Silicoflagellates, ebridians and actiniscidians from ODP Leg 104 holes
The lower Miocene to Pleistocene at Sites 642 and 644 is subdivided into eight silicoflagellate zones and nine ebridian-actiniscidian zones. Due to the bioevents selected, the... -
Sea surface temperature reconstruction of ODP Site 175-1087
Successful application of the alkenone palaeothermometer, the UK'37 index, relies upon the assumption that fossil alkenone synthesisers responded to growth-temperature changes... -
Neogene magneto- and biostratigraphy of ODP Leg 104 holes
Silicoflagellate assemblages of ODP Leg 104 Neogene sequences are the basis of an interpretation of changes in the Neogene paleoenvironment of the Norwegian Sea. Fluctuations in... -
Neogene silicoflaggelates in ODP Leg 104 holes
A quantative study was made of silicoflagellates recovered from Sites 642 (lower Miocene-upper Pliocene), 643 (lower Miocene-upper Miocene), and 644 (upper Pliocene-Quaternary)... -
Geochemistry and stable isotope record of benthic foraminifera of Miocene sed...
The processes causing the middle Miocene global cooling, which marked the Earth's final transition into an 'icehouse' climate about 13.9 million years ago (Myr ago) (Flower and... -
Mg/Ca and stable isotope record of benthic foraminifera of the Paleocene-Eoce...
A rapid increase in greenhouse gas levels is thought to have fueled global warming at the Paleocene-Eocene Thermal Maximum (PETM). Foraminiferal magnesium/calcium ratios... -
Carbon cycle change in the Eocene
The transition from the extreme global warmth of the early Eocene 'greenhouse' climate ~55 million years ago to the present glaciated state is one of the most prominent changes... -
Pollen distribution and stable oxygen isotope record of foraminifera from ODP...
A late Pliocene high-resolution pollen record from the southeast Atlantic (Ocean Drilling Program Site 1082) registers vegetation development in southwest Africa. The marine... -
Calcareous nannofossils of the Norwegian-Greenland Sea
Ocean Drilling Program Leg 104 recovered sediments containing calcareous nannofossils of latest Oligocene to Holocene age from the Voring Plateau in the Norwegian-Greenland Sea.... -
Sea surface temperature record of ODP Site 202-1233
We present the first high-resolution alkenone-derived sea surface temperature (SST) reconstruction in the southeast Pacific (Ocean Drilling Program Site 1233) covering the major... -
Stable oxygen isotope record of benthic foraminifera from the tropical Atlantic
Benthic foraminiferal oxygen isotope ratios from two sediment cores recovered at 426 and 1299 m water depth in the eastern and western tropical Atlantic show that a slowdown of... -
Magnetostratigraphy of ODP Leg 178 holes
We present revised magnetostratigraphic interpretations for Ocean Drilling Program Sites 1095, 1096, and 1101, cored in sediment drifts located off the Pacific margin of the... -
Neogene diatoms from the western Antarctic Peninsula
During Ocean Drilling Program Leg 178 we cored nine sites on the continental rise (Sites 1095, 1096, and 1101), continental shelf (Sites 1097, 1100, 1102, and 1103), and in an... -
Stable isotope composition of secondary carbonates from basalric lavas of ODP...
Hole 642E is located near the outer margin of the Voring Plateau in the Norwegian Sea. The thick pile of basaltic lavas penetrated during drilling are variably altered with... -
Rb-Sr systematics of volcanic rocks and alteration minerals of ODP Hole 104-642E
Subaerially erupted tholeiites at Hole 642E were never exposed to the high-temperature seawater circulation and alteration conditions that are found at subaqueous ridges.... -
Age determination and planktonic foraminifera og ODP Site 159-958
Site 958 was drilled to monitor the late Neogene history of both continental aridity in northwestern Africa and the Canary Current distant from nearshore upwelling. Based on... -
Diatom abundance in ODP Leg 178 holes
This paper documents the biostratigraphic distribution and abundance of diatoms from sites drilled during Ocean Drilling Program Leg 178, off the Pacific margin of the Antarctic...
