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Planktonic foraminiferal Mg/Ca as a proxy for past oceanic temperatures: a methodological overview and data compilation for the Last Glacial Maximum
As part of the Multi-proxy Approach for the Reconstruction of the Glacial Ocean (MARGO)
incentive, published and unpublished temperature reconstructions for the Last Glacial …
incentive, published and unpublished temperature reconstructions for the Last Glacial …
The Mg isotopic composition of Cenozoic seawater–evidence for a link between Mg-clays, seawater Mg/Ca, and climate
Cooling of Earth's climate over the Cenozoic has been accompanied by large changes in
the magnesium and calcium content of seawater whose origins remain enigmatic. The …
the magnesium and calcium content of seawater whose origins remain enigmatic. The …
Potential and limitations of Sr/Ca ratios in coccolith carbonate: new perspectives from cultures and monospecific samples from sediments
The Sr/Ca ratio of coccoliths was recently proposed as a potential indicator of past growth
rates of coccolithophorids, marine algae, which play key roles in both the global carbonate …
rates of coccolithophorids, marine algae, which play key roles in both the global carbonate …
Environmental and biological controls on elemental (Mg/Ca, Sr/Ca and Mn/Ca) ratios in shells of the king scallop Pecten maximus
The relationship between potential elemental proxies (Mg/Ca, Sr/Ca and Mn/Ca ratios) and
environmental factors was investigated for the bivalve Pecten maximus in a detailed field …
environmental factors was investigated for the bivalve Pecten maximus in a detailed field …
Strong kinetic effects on Sr/Ca ratios in the calcitic bivalve Pecten maximus
Abstract Although Sr/Ca ratios in abiogenic calcite are strongly controlled by precipitation
rates, such a kinetic effect has never been demonstrated in calcitic bivalve shells. Therefore …
rates, such a kinetic effect has never been demonstrated in calcitic bivalve shells. Therefore …
The first 150 million years history of calcareous nannoplankton: biosphere–geosphere interactions
E Erba - Palaeogeography, Palaeoclimatology, Palaeoecology, 2006 - Elsevier
The Mesozoic evolution of calcareous nannoplankton is here compared to global changes
in the Earth system to derive possible causal links between biosphere–geosphere …
in the Earth system to derive possible causal links between biosphere–geosphere …
Records of Neogene seawater chemistry and diagenesis in deep-sea carbonate sediments and pore fluids
Deep-sea pore fluids are potential archives of ancient seawater chemistry. However, the
primary signal recorded in pore fluids is often overprinted by diagenetic processes. Recent …
primary signal recorded in pore fluids is often overprinted by diagenetic processes. Recent …
Sponge bioerosion accelerated by ocean acidification across species and latitudes?
In many marine biogeographic realms, bioeroding sponges dominate the internal bioerosion
of calcareous substrates such as mollusc beds and coral reef framework. They …
of calcareous substrates such as mollusc beds and coral reef framework. They …
Metal-ion partitioning during low-temperature precipitation and dissolution of anhydrous carbonates and sulphates
ME Böttcher, M Dietzel - 2011 - pubs.geoscienceworld.org
Anhydrous carbonate and sulphate-bearing solids are formed on Earth under very different
environmental conditions and are the most abundant constituents in so-called chemical …
environmental conditions and are the most abundant constituents in so-called chemical …
Role of silicon in the development of complex crystal shapes in coccolithophores
The development of calcification by the coccolithophores had a profound impact on ocean
carbon cycling, but the evolutionary steps leading to the formation of these complex …
carbon cycling, but the evolutionary steps leading to the formation of these complex …