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Ogasawara annual Sr/Ca, U/Ca, stable isotope and δ¹⁸O seawater data of coral ...
This dataset has no description
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Ogasawara bimonthly Sr/Ca, U/Ca, and stable isotope data of coral core OGA-02-1
This dataset has no description
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Age model, stable isotopes and Sr/Ca record of coral core BDA100
Coral material older than 1928 is potentially diagenetically altered -
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... -
Seawater carbonate chemistry and elemental ratios in biogenic marine calcium ...
Elemental ratios in biogenic marine calcium carbonates are widely used in geobiology, environmental science, and paleoenvironmental reconstructions. It is generally accepted... -
Seawater carbonate chemistry and pH of the extracellular calcifying fluid and...
Ocean acidification (OA) threatens the growth and function of coral reef ecosystems. A key component to coral health is the microbiome, but little is known about the impact of... -
Carbonate associated trace metal and uranium isotope data for the PETM
The Paleocene Eocene Thermal Maximum (PETM) represents a major carbon cycle and climate perturbation that was associated with ocean de-oxygenation, in a qualitatively similar... -
Seawater carbonate chemistry and trace element composition of bivalve shell
We sought to determine how pCO2 will affect the incorporation of trace elements into bivalve shell. This was to validate that under high pCO2 conditions reconstruction of animal... -
Sea-ice biomarkers, benthic and planktonic foraminiferal geochemistry, and be...
The dataset compiles sea-ice biomarkers (IP25, HBI II, HBI III, Triene E, Brassicasterol, Campesterol, Cholesterol, β- sitosterol) together with benthic and planktonic... -
Trace element data covering 96-7 ka BP from stalagmite CM (Santo Tomas Cave, ...
We present a new speleothem trace element and stable isotope record, which extends previous paleoclimate evidence from Cuban speleothems to the last 96 ka.Stable isotope samples... -
Sea-ice biomarkers, benthic and planktonic foraminiferal geochemistry, and be...
The dataset compiles sea-ice biomarkers (IP25, HBI II, HBI III, Triene E, Brassicasterol, Campesterol, Cholesterol, β- sitosterol) together with benthic and planktonic... -
Seawater carbonate chemistry and incorporation of Mg, Sr, Ba, U, and B in Hig...
Measurement of elemental ratios (E/Ca) have been performed in two symbiont-bearing species of high-Mg calcite benthic foraminifers (hyaline, Baculogypsina sphaerulata and... -
Seawater carbonate chemistry and otolith development and chemistry in a diadr...
Ocean acidification threatens marine ecosystems by altering ocean chemistry and calcification processes in marine organisms. This study investigated the effects of predicted... -
Seawater carbonate chemistry and boron isotope and trace elements incorporati...
Early-life stages of reef-building corals are vital to coral existence and reef maintenance. It is therefore crucial to study juvenile coral response to future climate change... -
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... -
The influence of seawater pH on U/ Ca ratios in the scleractinian cold-water ...
The increasing pCO2 in seawater is a serious threat for marine calcifiers and alters the biogeochemistry of the ocean. Therefore, the reconstruction of past-seawater properties... -
d11B and metal/Ca ratios versus size fractions in the Surface and deep dwelli...
We have assessed the reliability of several foraminifer-hosted proxies of the ocean carbonate system (d11B, B/Ca, and U/Ca) using Holocene samples from the Atlantic and Pacific... -
Seawater carbonate chemistry and benthic foraminifera Ammonia sp. uranium inc...
The chemical and isotopic composition of foraminiferal shells (so-called proxies) reflects the physico-chemical properties of the seawater. In current day paleoclimate research,... -
Boron isotopes, trace elements and pH calculation for Norwegian deep sea cora...
d11B and trace results obtained for a deep sea coral specimen Madrepora oculata collected from the Norwegian Sea (67°N, 9°E, 340 m) during the RV Polarstern ARK/II/Ia cruise... -
Seawater carbonate chemistry, Acropora digitifera growth and skeletal U/Ca ra...
The impact of ocean acidification caused by the increasing atmospheric CO2 has been studied in marine calcifiers, including hermatypic corals. However, the effect of elevated...
