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Seawater carbonate chemistry and encrusting algal communities duirng a mesoco...
Owing to anthropogenic emissions, atmospheric concentrations of carbon dioxide could almost double between 2006 and 2100 according to business-as-usual carbon dioxide emission... -
Seawater carbonate chemistry during a mesocosm experiment, 2007
Owing to anthropogenic emissions, atmospheric concentrations of carbon dioxide could almost double between 2006 and 2100 according to business-as-usual carbon dioxide emission... -
Seawater carbonate chemistry and pteropod Limacina helicina antarctica shell ...
Anthropogenic ocean acidification is likely to have negative effects on marine calcifying organisms, such as shelled pteropods, by promoting dissolution of aragonite shells.... -
Seawater carbonate chemistry, growth rate and PIC and POC production during e...
The coccolithophore Emiliania huxleyi was cultured under a broad range of carbonate chemistry conditions to distinguish the effects of individual carbonate system parameters on... -
Seawater carbonate chemistry, nutrients, growth rate and phytoplnkton communi...
This paper reports for the first time upon the effects of increasing CO2 concentrations on a natural phytoplankton assemblage in a tropical estuary (the Godavari River Estuary... -
Seawater carbonate chemistry and processes during experiments with coral Acro...
The rise in atmospheric CO2 has caused significant decrease in sea surface pH and carbonate ion (CO3-2) concentration. This decrease has a negative effect on calcification in... -
Seawater carbonate chemistry and carbon and oxygen isotopes during experiment...
Stable oxygen and carbon isotope measurements on biogenic calcite and aragonite have become standard tools for reconstructing past oceanographic and climatic change. In aquatic... -
Seawater carbonate chemistry and calcification during an experiment with a co...
Using living corals collected from Okinawan coral reefs, laboratory experiments were performed to investigate the relationship between coral calcification and aragonite... -
Seawater carbonate chemistry, growth rate and processes during experiments wi...
Uptake of half of the fossil fuel CO2 into the ocean causes gradual seawater acidification. This has been shown to slow down calcification of major calcifying groups, such as... -
Seawater carbonate chemistry during a Ishigaki Island (Japan) coral reef seas...
Monitoring seawater CO2 for a full year with seasonal observations of community metabolism in Ishigaki Island, Japan, revealed seasonal variation and anomalous values owing to... -
Seawater carbonate chemistry and particulate organic particles during a semic...
Diazotrophic (N2-fixing) cyanobacteria provide the biological source of new nitrogen for large parts of the ocean. However, little is known about their sensitivity to global... -
Chemistry measurements of pore water from IODP Hole 370-C0023A
This dataset has no description
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Chemistry measurements of pore water from IODP Hole 365-C0010E
This dataset has no description
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Liquid chemistry from IODP Hole 365-C0010A
This dataset has no description
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Chemistry measurements of pore water from IODP Hole 365-C0010C
This dataset has no description
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Chemistry measurements of pore water from IODP Hole 348-C0002P
Geocode = [m CSF-A] Top Core depth (below sea floor) -
Chemistry measurements of pore water from IODP Hole 338-C0021B
Geocode = [m CSF-A] Top Core depth (below sea floor) -
Liquid chemistry from IODP Hole 338-C0021B
Geocode = [m CSF-A] -
Chemistry measurements of pore water from IODP Hole 338-C0002K
Geocode = [m CSF-A] Top Core depth (below sea floor) -
Chemistry measurements of pore water from IODP Hole 338-C0002L
Geocode = [m CSF-A] Top Core depth (below sea floor)
