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Molybdenum and sulphur isotope ratios of early Pleistocene sapropels of ODP H...
Organic-rich sediments (sapropels) deposited in the Mediterranean are presumed to have formed during periods of increased productivity, and/or deep water oxygen depletion,... -
Benthic foraminifera distribution and stable isotope record of ODP Hole 160-963A
New centennial-scale data of benthic foraminifera assemblages and of stable isotopes of foraminifera shells from the Sicily Channel, representative of surface and bottom waters,... -
Sapropels in the Mediterranean Sea
Eastern Mediterranean sediments are characterized by cyclic deposition of organic-rich sediments known as sapropels. Enhanced primary productivity combined with bottom water... -
Benthic foraminifera of Mediterranean deep-sea sediments
Ninety-five species and 19 genera of cosmopolitan, deep-sea benthic foraminifera belonging to the families Pleurostomellidae, Stilostomellidae and Nodosariidae, became extinct... -
Diatoms and laminae of Mediterranean sapropels
The origins of sapropels (sedimentary layers rich in organic carbon) are unclear, yet they may be a key to understanding the influence of climate on ocean eutrophication, the... -
Modes of sapropel formation in the eastern Mediterranean: some constraints ba...
Pyrite formation within and directly below sapropels in the eastern Mediterranean was governed by the relative rates of sulphide production and Fe liberation and supply to the... -
Total organic carbon content and isorenieratene concentrations from three hol...
Carotenoids were analysed in ca. 1-cm thick subsamples of three laterally time-equivalent sapropels from a west-east transect of the eastern Mediterranean Basin to study euxinic... -
Sea surface temperature reconstruction for Mediterranean Sea samples
Alkenone unsaturation ratios and planktonic delta18O records from sediment cores of the Alboran, Ionian and Levantine basins in the Mediterranean Sea show pronounced variations... -
Organic carbon analyses of ODP Site 160-971 in the Mediterranean Sea
Mud volcanism on the Mediterranean Ridge is caused by extrusion of overpressured sediments, with consequent formation of spectacular dome-shaped features composed of mud... -
Organic matter and trace element concentrations in sapropels from ODP Leg 160...
A distinct Pliocene eastern Mediterranean sapropel (i-282), recovered from three Ocean Drilling Program (ODP) Leg 160 Sites, has been investigated for its organic and inorganic... -
Nd isotope data for planktonic foraminifera from within and around sapropels ...
The development of widespread anoxic conditions in the deep oceans is evidenced by the accumulation and preservation of organic-carbon-rich sediments, but its precise cause... -
Boron contents and boron, carbon, and oxygen isotope data for ODP Sites 160-9...
Products of two mud volcanoes from the distal part of the Mediterranean Ridge accretionary complex have been investigated regarding their B, C, and O stable isotope signatures.... -
Oxygen and hydrogen isotope ratios of pore waters from ODP sites in the Medit...
Pore fluids from two ODP sites at Eastern Mediterranean mud volcanoes have been analyzed for their Cl concentration and their delta18O and deltaD isotopic composition. The Cl... -
The sapropel record of the eastern Mediterranean Sea
Research on sediments recovered during Ocean Drilling Leg 160 has concentrated on two issues: the first concerned the stratigraphy of sapropel formation, the second was oriented... -
High-resolution stratigraphic framework for Mediterranean sapropel S5
A high-resolution stratigraphic framework is presented for sapropel S5, which represents the low-mid latitude climate optimum of the previous interglacial period (Eemian). The... -
Geochemistry of sediments cores in the Mediterranean Sea
We investigated five time-equivalent core sections (180-110 kyr BP) from the Balearic Sea (Menorca Rise), the easternmost Levantine Basin and southwest, south, and southeast of... -
Trace element distribution in latest Pliocene sapropels in the Mediterranean Sea
Compositions of productivity- and redox-sensitive trace-metals in two Upper Pliocene sapropel sequences from western Mediterranean ODP Sites 974 and 975 and eastern... -
P-wave velocity (PWS split-core system) on ODP Hole 160-973A
This dataset has no description
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P-wave velocity (PWS split-core system) on ODP Hole 160-972A
This dataset has no description
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P-wave velocity (PWS split-core system) on ODP Hole 160-971B
This dataset has no description
