The Mid-Brunhes dissolution interval (MBDI) represents a period of global carbonate dissolution, lasting several hundred thousand\ud years, centred around Marine Isotope Stage (MIS) 11. Here we report the effects of dissolution in ODP core 982, taken from 1134m in\ud the North Atlantic. Paradoxically, records of atmospheric CO2 from Antarctic ice-cores reveal no long term trend over the last 400 kyr\ud and suggest that CO2 during MIS 11 was no higher than during the present interglacial. We suggest that a global increase in pelagic\ud carbonate production during this period, possibly related to the proliferation of the Gephyrocapsa coccolithophore, could have altered\ud marine carbonate chemistry in such a way as to drive increased dissolut...
The marine carbonate pump includes the production of calcium carbonate, CaCO:sub:3:/sub: by marine o...
We present new deep water carbonate ion concentration ([CO3 2-]) records, reconstructed using Cibici...
[1] We examine the effect on atmospheric CO2 of the occurrence of increased shallow water carbonate ...
The Mid-Brunhes dissolution interval (MBDI) represents a period of global carbonate dissolution, las...
The Mid-Brunhes dissolution interval (MBDI) represents a period of global carbonate dissolution, las...
We present new deep water carbonate ion concentration ([CO32-]) records, reconstructed using Cibicid...
Abstract Higher alkalinity is compensation for reduced CaCO3 burial in the deep ocean in response to...
The marine carbonate pump includes the production of calcium carbonate, CaCO:sub:3:/sub: by marine o...
Carbon release from the deep ocean at glacial terminations is a critical component of past climate c...
Dissolution of fossil fuel CO 2 in seawater results in decreasing carbonate ion concentration and lo...
AbstractThe production, transportation, deposition, and dissolution of carbonate profoundly form par...
Changes in deep ocean carbonate chemistry have profound implications for glacial-interglacial atmosp...
The flux of carbon in to and out of the atmosphere exerts a fundamental control over the Earth's cli...
Characterised by long term cooling and abrupt ice sheet expansion on Antarctica ~14 Ma ago, the mid ...
12th International Conference on Paleoceanography (ICP12), 29 August - 2 September 2016, UtrechtThe ...
The marine carbonate pump includes the production of calcium carbonate, CaCO:sub:3:/sub: by marine o...
We present new deep water carbonate ion concentration ([CO3 2-]) records, reconstructed using Cibici...
[1] We examine the effect on atmospheric CO2 of the occurrence of increased shallow water carbonate ...
The Mid-Brunhes dissolution interval (MBDI) represents a period of global carbonate dissolution, las...
The Mid-Brunhes dissolution interval (MBDI) represents a period of global carbonate dissolution, las...
We present new deep water carbonate ion concentration ([CO32-]) records, reconstructed using Cibicid...
Abstract Higher alkalinity is compensation for reduced CaCO3 burial in the deep ocean in response to...
The marine carbonate pump includes the production of calcium carbonate, CaCO:sub:3:/sub: by marine o...
Carbon release from the deep ocean at glacial terminations is a critical component of past climate c...
Dissolution of fossil fuel CO 2 in seawater results in decreasing carbonate ion concentration and lo...
AbstractThe production, transportation, deposition, and dissolution of carbonate profoundly form par...
Changes in deep ocean carbonate chemistry have profound implications for glacial-interglacial atmosp...
The flux of carbon in to and out of the atmosphere exerts a fundamental control over the Earth's cli...
Characterised by long term cooling and abrupt ice sheet expansion on Antarctica ~14 Ma ago, the mid ...
12th International Conference on Paleoceanography (ICP12), 29 August - 2 September 2016, UtrechtThe ...
The marine carbonate pump includes the production of calcium carbonate, CaCO:sub:3:/sub: by marine o...
We present new deep water carbonate ion concentration ([CO3 2-]) records, reconstructed using Cibici...
[1] We examine the effect on atmospheric CO2 of the occurrence of increased shallow water carbonate ...