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Stable carbon isotope ratios and the formation of dolomite in ODP Leg 175 sites
We examine the link between organic matter degradation, anaerobic methane oxidation (AMO), and sulfate depletion and explore how these processes potentially influence... -
AMS radiocarbon dates and pollen analysis of ODP Hole 175-1078C
ODP Site 1078 situated under the coast of Angola provides the first record of the vegetation history for Angola. The upper 11 m of the core covers the past 30 thousand years,... -
Pollen analysis of sediment cores from the mouth of the river Congo to Walvis...
The distribution of pollen in marine sediments is used to record vegetation changes over the past 30,000 years on the adjacent continent. A transect of marine pollen sequences... -
Distribution of pollen and spores in sediments of ODP Hole 175-1078C
The distribution of pollen in marine sediments is used to record vegetation change on the continent. Generally, a good latitudinal correspondence exists between the distribution... -
Diatom abundance index and biogenic opal content for ODP Leg 175 holes
Several sites of Ocean Drilling Program Leg 175 between 20° and 30°S (1081, 1082, 1083, 1084 and 1085) in the Benguela Current system show a distinct opal (and diatom) maximum... -
Sand fraction, carbonate and organic carbon contents of ODP Hole 175-1085A
Site 1085 is located on the continental rise of southwest Africa at a water depth of 1713 m off the mouth of the Orange River in the Cape Basin. The site is part of the suite of... -
Late Cenozoic radiolarians of ODP Hole 175-1082A
Latest Miocene to Pleistocene poorly to well-preserved radiolarians were recovered from Hole 1082A in the Walvis Basin by Ocean Drilling Program Leg 175. Having moderate... -
Petrographic, cathodoluminescent, and compositional characters of organic dol...
The main objective of Leg 175 was to reconstruct the Late Neogene paleoceanographic history of the Benguela Current and associated upwelling regimes along the southwest African... -
Late Quaternary planktonic foraminifera of ODP Hole 175-1087A
Planktonic foraminiferal assemblages from the upper Pleistocene part of Hole 1087A (0 to 12.1 meters below seafloor) are investigated to assess the role of global and local... -
Carbon, opal, and isotope concentration of ODP Leg 175 holes
One of the goals of Ocean Drilling Program (ODP) Leg 175 was to reconstruct the history of upwelling-induced biological productivity along the coast of Africa from the Congo... -
Marine and terrigenous lipids in ODP Leg 175 holes
Lipid compositions of sediments recovered during Ocean Drilling Program Leg 175 in the eastern South Atlantic reflect a variety of oceanographic and climatological environments.... -
Sea-surface temperature reconstruction of ODP Hole 175-1078C
A prominent feature in the Southeast Atlantic is the Angola-Benguela Front (ABF), the convergence between warm tropical and cold subtropical upwelled waters. At present, the... -
Grain size analysis and sedimentation rates of ODP Hole 175-1085A off the Nam...
Sediments from the ODP Site 1085A were studied to investigate the impacts of global cooling in the Middle and Late Miocene on the climate in Southwestern Africa. The size... -
Age models of ODP Leg 175 holes
A multiproxy approach including the use of stable isotopes, magnetic characterization analyses, and organic geochemistry has been adopted to consider factors such as... -
Sedimentology of ODP sites in the Cape Basin, southeast Atlantic Ocean
Middle/late Miocene to early Pliocene sedimentary sequences along the continental margin of southwest Africa have changes that correspond to the carbonate crash (12-9 Ma) and... -
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... -
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)... -
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... -
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... -
TOC, carbonate, opal composition and trace element concentration from ODP Hol...
Distinctive light-dark color cycles in sediment beneath the Benguela Current Upwelling System indicate repetitive alternations in sediment delivery and deposition. Geochemical...