-
CLAM age model and microcharcoal of sediment core Tswaing_Crater
This dataset has no description
-
CLAM age model and microcharcoal of sediment core Tagua_Tagua
This dataset has no description
-
CLAM age model and microcharcoal of sediment core Siberia1
This dataset has no description
-
Geochemical characterization and the voltammetric investigation of hydrotherm...
Hydrothermal vent fluids are highly enriched in iron (Fe) compared to ambient seawater, and organic ligands may play a role in facilitating the transport of some hydrothermal Fe... -
Hydrochemistry measured on water bottle samples during Aurora Australis cruis...
For definition of quality flags see hdl:10013/epic.31518.d001 -
(Table T1) Pore water chemistry of ODP Site 195-1202 sediments, southern Okin...
Pore water was collected from sediment cores from Holes 1202A and 1202D in the southern Okinawa Trough during Ocean Drilling Program (ODP) Leg 195. Because drilling at this site... -
Seawater carbonate chemistry, length and survival of Inland silverside, Menid...
Absorption of anthropogenic carbon dioxide by the world's oceans is causing mankind's 'other CO2 problem', ocean acidification. Although this process will challenge marine... -
Seawater carbonate chemistry and protein sports of barnicle Balanus amphitrit...
The majority of benthic marine invertebrates have a complex life cycle, during which the pelagic larvae select a suitable substrate, attach to it, and then metamorphose into... -
Seawater carbonate chemistry and biological processes of foraminifera, Globig...
Specimens of two species of planktic foraminifera, Globigerinoides ruber and Globigerinella siphonifera, were grown under controlled laboratory conditions at a range of... -
Abundance of benthic infauna in surface sediments from the North Sea sampled ...
Data were provided through and converted from Schlüter, M & Jerosch, K (2009) Digital Atlas of the North Sea, hdl:10013/epic.34893.d001 (pdf 3.7 MB). -
Seawater carbonate chemistry and shell weights of Laternula elliptica, Yoldia...
Antarctic calcified macroorganisms are particularly vulnerable to ocean acidification because many are weakly calcified, the dissolution rates of calcium carbonate are inversely... -
Seawater carbonate chemistry and biological processes during experiments with...
Anthropogenic elevation of atmospheric pCO2 is predicted to cause the pH of surface seawater to decline by 0.3-0.4 units by 2100 AD, causing a 50% reduction in seawater [CO3]... -
Seawater carbonate chemistry and processes during experiments with coccolitho...
The formation of calcareous skeletons by marine planktonic organisms and their subsequent sinking to depth generates a continuous rain of calcium carbonate to the deep ocean and... -
Seawater carbonate chemistry and community calcification during Reunion Islan...
To assess the contribution of soft-bottoms to the carbon cycle in coral reefs, the net community production (p) was measured in winter at 3 stations on La Saline inner reef flat... -
Geochemistry data of box sediment core PAR93/52-SBX-5B
This dataset has no description
-
Geochemistry data of box sediment core PAR93/52-SBX-3
This dataset has no description
-
Geochemistry data of box sediment core PAR93/52-SBX-2
This dataset has no description
-
Geochemistry data of box sediment core PAR93/52-SBX-1
This dataset has no description
-
Geochemistry data of box sediment core HUD94/9-SBX-S
This dataset has no description
-
Geochemistry data of box sediment core HUD94/9-SBX-B
This dataset has no description
