Biomineralization: Integrating mechanism and evolutionary history
Calcium carbonate (CaCO3) biomineralizing organisms have played major roles in the
history of life and the global carbon cycle during the past 541 Ma. Both marine diversification …
history of life and the global carbon cycle during the past 541 Ma. Both marine diversification …
The geochemistry of deep-sea coral skeletons: a review of vital effects and applications for palaeoceanography
Deep-sea corals were discovered over a century ago, but it is only over recent years that
focused efforts have been made to explore the history of the oceans using the geochemistry …
focused efforts have been made to explore the history of the oceans using the geochemistry …
Impact of seawater acidification on pH at the tissue–skeleton interface and calcification in reef corals
Insight into the response of reef corals and other major marine calcifiers to ocean
acidification is limited by a lack of knowledge about how seawater pH and carbonate …
acidification is limited by a lack of knowledge about how seawater pH and carbonate …
CO2 storage and release in the deep Southern Ocean on millennial to centennial timescales
The cause of changes in atmospheric carbon dioxide (CO2) during the recent ice ages is yet
to be fully explained. Most mechanisms for glacial–interglacial CO2 change have centred on …
to be fully explained. Most mechanisms for glacial–interglacial CO2 change have centred on …
Calibration of the boron isotope proxy in the planktonic foraminifera Globigerinoides ruber for use in palaeo-CO2 reconstruction
The boron isotope-pH proxy, applied to mixed-layer planktic foraminifera, has great potential
for estimating past CO2 levels, which in turn is crucial to advance our understanding of how …
for estimating past CO2 levels, which in turn is crucial to advance our understanding of how …
The reef-building coral Siderastrea siderea exhibits parabolic responses to ocean acidification and warming
Anthropogenic increases in atmospheric CO2 over this century are predicted to cause global
average surface ocean pH to decline by 0.1–0.3 pH units and sea surface temperature to …
average surface ocean pH to decline by 0.1–0.3 pH units and sea surface temperature to …
[HTML][HTML] Short-term metabolic and growth responses of the cold-water coral Lophelia pertusa to ocean acidification
Cold-water corals are associated with high local biodiversity, but despite their importance as
ecosystem engineers, little is known about how these organisms will respond to projected …
ecosystem engineers, little is known about how these organisms will respond to projected …
Crystallographic control on the boron isotope paleo-pH proxy
When using the boron isotopic composition (δ 11 B) of marine carbonates as a seawater pH
proxy, it is assumed that only the tetrahedral borate ion is incorporated into the growing …
proxy, it is assumed that only the tetrahedral borate ion is incorporated into the growing …
Boron isotopic compositions of middle Miocene to recent shallow-water carbonates from the South China Sea: Assessing diagenetic effects and implications for …
The partial pressure of atmospheric CO 2 (pCO 2) significantly influences global climate
change and biological evolution through geological history. Boron isotopic composition (δ …
change and biological evolution through geological history. Boron isotopic composition (δ …
Impacts of seawater saturation state (ΩA= 0.4–4.6) and temperature (10, 25 C) on the dissolution kinetics of whole-shell biogenic carbonates
Anthropogenic increase of atmospheric pCO 2 since the Industrial Revolution has caused
seawater pH to decrease and seawater temperatures to increase—trends that are expected …
seawater pH to decrease and seawater temperatures to increase—trends that are expected …