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Mineralogical response of the Mediterranean crustose coralline alga Lithophyl...
Red calcareous coralline algae are thought to be among the organisms most vulnerable to ocean acidification due to the high solubility of their magnesium calcite skeleton.... -
Seawater carbonate chemistry and Posidonia oceanica epiphytic community compo...
Alterations in seagrass epiphytic communities are expected under future ocean acidification conditions, yet this hypothesis has been little tested in situ. A Free Ocean Carbon... -
Effect of ocean acidification and pH fluctuations on the growth and developme...
Coralline algae are susceptible to the changes in the seawater carbonate system associated with ocean acidification (OA). However, the coastal environments in which corallines... -
Diurnal fluctuations in seawater pH influence the response of a calcifying ma...
Coastal ecosystems that are characterized by kelp forests encounter daily pH fluctuations, driven by photosynthesis and respiration, which are larger than pH changes owing to... -
Phenotypic plasticity of coralline algae in a High CO2 world
It is important to understand how marine calcifying organisms may acclimatize to ocean acidification to assess their survival over the coming century. We cultured the cold water... -
Dolomite-rich coralline algae in reefs resist dissolution in acidified condit...
Coral reef ecosystems develop best in high-flow environments but their fragile frameworks are also vulnerable to high wave energy. Wave-resistant algal rims, predominantly made... -
Seawater carbonate chemistry and elemental composition of purple sea urchin (...
Ocean acidification will likely have negative impacts on invertebrates producing skeletons composed of calcium carbonate. Skeletal solubility is partly controlled by the... -
Petrography, carbonate mineralogy and texture of carbonate rocks of Meteor an...
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Chemical composition of bottom sediments from the Barents Sea and adjacent areas
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(Table 2) X-ray diffractometry analyses of carbonate samples from station Geo...
CO - lithified coccolith ooze; TZ - Transition Zone; YA - Yellowish Aragonite* Badly defined LMC (104)-peak hampered unambiguous determination of d-value.MgCO3, weighted mean =... -
(Table 1) XRD and geochemical bulk sediment analyses on specific lithological...
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(Table 8) Elemental atomic ratios to Al and calculated protodolomite composit...
Sediment depth is given in mbsf. Blank spaces indicate that no data were obtained. The composition of the protodolomites was calculated as follows: The Ca/Al, Mg/Al, and Fe/Al... -
(Table T5) Major compositon and atomic formulas of carbonates from ODP Leg 16...
Sediment depth is given in mbsf. Formulas have been calculated on the basis of six oxygens per unit cell. -
(Table 2) Composition of siderites from DSDP Holes 70-506G and 70-507B
Sample 506 (1-23) is a hyalopilitic, fine-grained, highly vesicular basalt with rare plagioclase and clinopyroxene phenocrysts. It shows a 2-2.5-mm-wide black halo. Sample 507... -
(Table 3) Carbonate mineralogy at DSDP Leg 57 Holes
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(Table 1) Mineralogy at DSDP Hole 62-463
?1 = presence uncertain epmty cells = no data. -
(Table 1) Stratigraphy, composition, and isotopes at DSDP Leg 63 Holes carbon...
Sediment depth is given in mbsf. #0 = indicates either no dolomite or calcite or only minor calcite present. Empty cells = no data available. # in d13C and d18O values indicates... -
(Table 4) Sample descriptions and isotopic compositions of carbonate nodules ...
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(Table 4) Chemical composition of calcite and dolomite at DSDP Site 76-533 se...
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(Table 3) Mineralogic, elemental, and stable isotopic composition of bulk car...
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