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Impact of high CO2 on the geochemistry of the coralline algae Lithothamnion g...
Coralline algae are a significant component of the benthic ecosystem. Their ability to withstand physical stresses in high energy environments relies on their skeletal structure... -
Uranium in larval shells as a barometer of molluscan ocean acidification expo...
As the ocean undergoes acidification, marine organisms will become increasingly exposed to reduced pH, yet variability in many coastal settings complicates our ability to... -
Ocean acidification impairs vermetid reef recruitment
Vermetids form reefs in sub-tropical and warm-temperate waters that protect coasts from erosion, regulate sediment transport and accumulation, serve as carbon sinks and provide... -
Seawater carbonate chemistry, thickness and carbonate elemental composition o...
Continuous anthropogenic CO2 emissions to the atmosphere and uptake by the oceans will cause a reduction of seawater pH and saturation state (Omega) of CaCO3 minerals from which... -
Temperature Dependent Effects of Elevated CO2 on Shell Composition and Mechan...
The majority of marine benthic invertebrates protect themselves from predators by producing calcareous tubes or shells that have remarkable mechanical strength. An elevation of... -
Seawater carbonate chemistry, physiology and skeletal mineralogy of coralline...
Marine organisms inhabiting environments where pCO2/pH varies naturally are suggested to be relatively resilient to future ocean acidification. To test this hypothesis, the... -
CO2-driven ocean acidification alters and weakens integrity of the calcareous...
As a consequence of anthropogenic CO2-driven ocean acidification (OA), coastal waters are becoming increasingly challenging for calcifiers due to reductions in saturation states... -
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... -
Seawater carbonate chemistry and conditions of Mytilus edulis extracellular b...
Mytilus edulis were cultured for 3 months under six different seawater pCO2 levels ranging from 380 to 4000 µatm. Specimen were taken from Kiel Fjord (Western Baltic Sea,... -
Incorporation of Mg and Sr in calcite of cultured benthic foraminifera (Heter...
We investigated the effect of the calcium concentration in seawater and thereby the calcite saturation state (omega) on the magnesium and strontium incorporation into benthic... -
Seawater carbonate chemistry, processes and elements during experiments with ...
We investigate the sensitivity of U/Ca, Mg/Ca, and Sr/Ca to changes in seawater [CO3[2-]] and temperature in calcite produced by the two planktonic foraminifera species,... -
Mg/Ca ratio and sub-surface temperatures derived from benthic foraminifera in...
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(Table 5) Downcore benthic foraminiferal Mg/Ca ratios from Southern Ocean cores
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(Table 4) Mg/Ca of benthic foraminiferal calcite from the Gulf of California,...
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(Table 3) Mg/Ca of benthic foraminiferal calcite from Hawaii Islands core-top...
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(Table 2) Mg/Ca of benthic foraminiferal calcite from Little Bahama Bank core...
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Early Holocene (c. 11.0 - 9.5 ka BP) trace element data from stalagmite NAH14...
This dataset from a speleothem record from the north-eastern Yucatán peninsula (Mexico) provides a high reslution stable isotope and trace elemental record for the early... -
Monthly interpolated geochemical data from modern Tahiti coral TIAREI-4
Here we present monthly resolved geochemical proxy data (Sr/Ca, Mg/Ca, δ18O, δ13C) extracted along the growth axes of Porites modern corals ecovered at Tahiti that grew between... -
Monthly interpolated geochemical data from modern Tahiti coral MARAA-7
Here we present monthly resolved geochemical proxy data (Sr/Ca, Mg/Ca, δ18O, δ13C) extracted along the growth axes of Porites modern corals ecovered at Tahiti that grew between... -
Monthly interpolated geochemical data from modern Tahiti coral TIAREI-3B
Here we present monthly resolved geochemical proxy data (Sr/Ca, Mg/Ca, δ18O, δ13C) extracted along the growth axes of Porites modern corals ecovered at Tahiti that grew between...
