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Nannofossil assemblages of mid-Pliocene sediments from the equatorial Atlantic
Downcore cyclic variation in high-resolution nannofossil abundance records from mid-Pliocene equatorial Atlantic ODP Sites 662 and 926 demonstrate the direct response by several... -
Distribution of planktonic foraminifera in Pleistocene sediments of the New J...
Abundance records of planktonic foraminifera (>150 µm) from the upper 520 m of ODP Site 1073 (Hole 1073A, Leg 174A, 639 m water depth) have been integrated with... -
Calcareous nannofossil bioevents of early-middle Pleistocene sediments from t...
Quantitative distributions of calcareous nannofossils are analysed in the early-middle Pleistocene at the small Gephyrocapsa and Pseudoemiliania lacunosa zone transition in... -
Eocene-Oligocene calcareous nannofossil events of ODP Sites from the Southern...
The evolution of the Southern Ocean climate during the late Eocene-late Oligocene interval is examined through highresolution, quantitative calcareous nannofossil analyses on... -
Benthic foraminiferal faunas of Miocene to Holocene sediments of ODP Site 184...
Deep-sea benthic foraminiferal assemblages from Ocean Drilling Program (ODP) Site 1143 located in the southern South China Sea (SCS) were investigated to evaluate the... -
Late middle Eocene to late Oligocene radiolarian biostratigraphy of ODP Hole ...
We propose a new biostratigraphic scheme comprising the Eucyrtidium spinosum, Eucyrtidium antiquum (new), Lychnocanoma conica (emended), Clinorhabdus robusta (emended) and... -
Stable carbon and oxygen isotope composition of Late Cretaceous benthic foram...
The stable carbon and oxygen isotope composition of different benthic foraminiferal species of the latest Campanian and earliest Maastrichtian from Ocean Drilling Project Hole... -
The Fohsella chronocline in middle Miocene sediments from the Ontong Java Pla...
Micropaleontologists have traditionally recognized the mid-Miocene Fohsella lineage as a flagship for phyletic gradualism within the planktic foraminifera. However, study of a... -
Sedimentology and radiolarian distribution of latest Miocene to Recent sedime...
Estimating past ocean productivity from ocean sediments often gives different results depending on the measurement used. We have examined a suite of paleoproductivity proxies in... -
Planktic foraminifera from the Paleocene-Eocene Thermal Maximum at Shatsky Ri...
High-resolution biostratigraphic and quantitative studies of subtropical Pacific planktonic foraminiferal assemblages (Ocean Drilling Program, Leg 198 Shatsky Rise, Sites 1209... -
Benthic foraminiferal assemblages and paleoproductivity reconstructions for t...
We analyzed foraminiferal and nannofossil assemblages and stable isotopes in samples from ODP Hole 807A on the Ontong Java Plateau in order to evaluate productivity and... -
Planktic foraminiferal distribution and paleotemperature reconstruction for t...
Faunal analyses of planktonic foraminifera and upper-water temperature reconstructions with the modern analog technique are studied and compared to themagnetic susceptibility... -
Determination of sulfite and manganese in sediments from the K/T boundary
The solid-state-physics technique of electron spin resonance (ESR) has been employed in an exploratory study of marine limestones and impact-related deposits from... -
Element composition in various minerlas of ODP Hole 209-1274A peridotites, Mi...
ODP Leg 209 Site 1274 mantle peridotites are highly refractory in terms of lack of residual clinopyroxene, olivine Mg# (up to 0.92) and spinel Cr# (~0.5), suggesting high degree... -
Major element composition of phenocrysts from the volcanic basement of ODP Ho...
Early arc volcanism during Eocene to Oligocene in the Izu forearc region was investigated during ODP Legs 125 and 126 in 1989, and effusive and intrusive volcanics were... -
Pleistocene and upper Pliocene sapropels in the Tyrrhenian Sea, Mediterranean...
A most significant finding of the ODP Leg 107 drilling campaign was the recovery of at least 56 distinct sapropel intervals in upper Pliocene to Pleistocene sediments of six... -
Barium intensities and tie points between holes of Leg 208
The Paleocene - Eocene thermal maximum (PETM) is one of the best known examples of a transient climate perturbation, associated with a brief, but intense, interval of global... -
Carbon and Sulphur concentrations of sediments from Peru, Oman and Benguela u...
Abundances of organic carbon, sulfur, and reactive iron in sediments of three upwelling environments (Peru, Oman and Benguela) suggest that organic carbon/reduced sulfur ratios... -
Element analyses and isotopic composition of basalts from the western Pacific
New Sr- Nd- and Pb-isotopic and trace element data are presented on basalts from the Sulu and Celebes Basins, and the submerged Cagayan Ridge Arc (Western Pacific), recently... -
Geochemistry and stratigraphy on sediment cores from Leg198 and Leg 208
The first complete cyclic sedimentary successions for the early Paleogene from drilling multiple holes have been retrieved during two ODP expeditions: Leg 198 (Shatsky Rise, NW...
