The early Paleogene experienced the most pronounced long-term warming trend of the
Cenozoic, superimposed by transient warming events such as the Paleocene–Eocene …

Carbon mineralization is an emerging field of research in carbon sequestration. In this
process, dissolved inorganic carbon reacts with mineral cations such as Ca 2+ and Mg 2+ to …

Arranging organisms into functional groups aids ecological research by grou** organisms
(irrespective of phylogenetic origin) that interact with environmental factors in similar ways …

Abstract The Barents Sea is presently undergoing rapid warming and the sea-ice edge and
the productive zones are retreating northward at accelerating rates. Planktonic foraminifers …

Under projections of global climate change and other stressors, significant changes in the
ecology, structure and function of coral reefs are predicted. Current management strategies …

Abstract The Barents Sea is a highly dynamic and productive marine ecosystem and a
hotspot of global warming. Variability in sea ice extent is a common feature in the Barents …

Ongoing ocean acidification is widely reported to reduce the ability of calcifying marine
organisms to produce their shells and skeletons. Whereas increased dissolution due to …

Large benthic foraminifera are major carbonate components in tropical carbonate platforms,
important carbonate producers, stratigraphic tools and powerful bioindicators (proxies) of …

Widely regarded as an imminent threat to our oceans, ocean acidification has been
documented in all oceanic basins. Projected changes in seawater chemistry will have …

Coccolithophores are major contributors to global marine planktonic calcification, and in
nature coccolithophores are invariably calcified through almost all of their life cycle. The …