Biochemical adaptation to ocean acidification
JH Stillman, AW Paganini - The Journal of Experimental …, 2015 - journals.biologists.com
The change in oceanic carbonate chemistry due to increased atmospheric P CO2 has
caused pH to decline in marine surface waters, a phenomenon known as ocean acidification …
caused pH to decline in marine surface waters, a phenomenon known as ocean acidification …
Two massive, rapid releases of carbon during the onset of the Palaeocene–Eocene thermal maximum
The Earth's climate abruptly warmed by 5–8° C during the Palaeocene–Eocene thermal
maximum (PETM), about 55.5 million years ago,. This warming was associated with a …
maximum (PETM), about 55.5 million years ago,. This warming was associated with a …
Macroevolutionary history of the planktic foraminifera
Planktic foraminifera are an abundant component of deep-sea sediment and are critical to
geohistorical research, primarily because as a biological and geochemical system they are …
geohistorical research, primarily because as a biological and geochemical system they are …
Forecasted coral reef decline in marine biodiversity hotspots under climate change
P Descombes, MS Wisz, F Leprieur… - Global Change …, 2015 - Wiley Online Library
Coral bleaching events threaten coral reef habitats globally and cause severe declines of
local biodiversity and productivity. Related to high sea surface temperatures (SST) …
local biodiversity and productivity. Related to high sea surface temperatures (SST) …
Frequency, magnitude and character of hyperthermal events at the onset of the Early Eocene Climatic Optimum
Recent studies have shown that the Early Eocene Climatic Optimum (EECO) was preceded
by a series of short-lived global warming events, known as hyperthermals. Here we present …
by a series of short-lived global warming events, known as hyperthermals. Here we present …
Understanding ocean acidification impacts on organismal to ecological scales
Ocean acidification (OA) research seeks to understand how marine ecosystems and global
elemental cycles will respond to changes in seawater carbonate chemistry in combination …
elemental cycles will respond to changes in seawater carbonate chemistry in combination …
Contact metamorphism and thermogenic gas generation in the Vøring and Møre basins, offshore Norway, during the Paleocene–Eocene thermal maximum
I Aarnes, S Planke, M Trulsvik… - Journal of the …, 2015 - pubs.geoscienceworld.org
Voluminous volcanic intrusive activity took place in the Vøring and Møre basins at the
Paleocene–Eocene boundary at about 56 Ma. This event caused thermal maturation of …
Paleocene–Eocene boundary at about 56 Ma. This event caused thermal maturation of …
Alluvial response to the Paleocene–Eocene thermal maximum climatic event, polecat bench, Wyoming (USA)
The stratigraphic interval spanning the Paleocene–Eocene Thermal Maximum in the
northern Bighorn Basin, Wyoming shows changes in the alluvial record that can be tied to a …
northern Bighorn Basin, Wyoming shows changes in the alluvial record that can be tied to a …
Analysis of bubble plume distributions to evaluate methane hydrate decomposition on the continental slope
HP Johnson, UK Miller, MS Salmi… - Geochemistry …, 2015 - Wiley Online Library
Cascadia margin sediments contain a rich reservoir of carbon derived both from terrestrial
input and sea surface productivity. A portion of this carbon exists as solid gas hydrate within …
input and sea surface productivity. A portion of this carbon exists as solid gas hydrate within …
Experimental evidence for kinetic effects on B/Ca in synthetic calcite: implications for potential B (OH) 4− and B (OH) 3 incorporation
The boron to calcium ratio (B/Ca) in biogenic CaCO 3 is being increasingly utilized as a
proxy for past ocean carbonate chemistry. However, B/Ca of cultured and core-top …
proxy for past ocean carbonate chemistry. However, B/Ca of cultured and core-top …