The geological record of ocean acidification
Ocean acidification may have severe consequences for marine ecosystems; however,
assessing its future impact is difficult because laboratory experiments and field observations …
assessing its future impact is difficult because laboratory experiments and field observations …
The Paleocene-Eocene Thermal Maximum: A perturbation of carbon cycle, climate, and biosphere with implications for the future
FA McInerney, SL Wing - Annual Review of Earth and Planetary …, 2011 - annualreviews.org
During the Paleocene-Eocene Thermal Maximum (PETM),∼ 56 Mya, thousands of
petagrams of carbon were released into the ocean-atmosphere system with attendant …
petagrams of carbon were released into the ocean-atmosphere system with attendant …
Very large release of mostly volcanic carbon during the Palaeocene–Eocene Thermal Maximum
Abstract The Palaeocene–Eocene Thermal Maximum,(PETM) was a global warming event
that occurred about 56 million years ago, and is commonly thought to have been driven …
that occurred about 56 million years ago, and is commonly thought to have been driven …
[图书][B] Biogeochemistry of marine dissolved organic matter
DA Hansell, CA Carlson - 2014 - books.google.com
Marine dissolved organic matter (DOM) is a complex mixture of molecules found throughout
the world's oceans. It plays a key role in the export, distribution, and sequestration of carbon …
the world's oceans. It plays a key role in the export, distribution, and sequestration of carbon …
History of Seawater Carbonate Chemistry, Atmospheric CO2, and Ocean Acidification
RE Zeebe - Annual review of earth and planetary sciences, 2012 - annualreviews.org
Humans are continuing to add vast amounts of carbon dioxide (CO2) to the atmosphere
through fossil fuel burning and other activities. A large fraction of the CO2 is taken up by the …
through fossil fuel burning and other activities. A large fraction of the CO2 is taken up by the …
[HTML][HTML] Six-fold increase of atmospheric pCO2 during the Permian–Triassic mass extinction
Abstract The Permian–Triassic mass extinction was marked by a massive release of carbon
into the ocean-atmosphere system, evidenced by a sharp negative carbon isotope …
into the ocean-atmosphere system, evidenced by a sharp negative carbon isotope …
Silicate weathering as a feedback and forcing in Earth's climate and carbon cycle
Current understanding of the long-term carbon cycle posits that Earth's climate is stabilized
by a negative feedback involving CO 2 consumption by chemical weathering of silicate …
by a negative feedback involving CO 2 consumption by chemical weathering of silicate …
A Cenozoic record of the equatorial Pacific carbonate compensation depth
Atmospheric carbon dioxide concentrations and climate are regulated on geological
timescales by the balance between carbon input from volcanic and metamorphic outgassing …
timescales by the balance between carbon input from volcanic and metamorphic outgassing …
Past extreme warming events linked to massive carbon release from thawing permafrost
RM DeConto, S Galeotti, M Pagani, D Tracy… - Nature, 2012 - nature.com
Abstract Between about 55.5 and 52 million years ago, Earth experienced a series of
sudden and extreme global warming events (hyperthermals) superimposed on a long-term …
sudden and extreme global warming events (hyperthermals) superimposed on a long-term …
[HTML][HTML] Climate model and proxy data constraints on ocean warming across the Paleocene–Eocene Thermal Maximum
Constraining the greenhouse gas forcing, climatic warming and estimates of climate
sensitivity across ancient large transient warming events is a major challenge to the …
sensitivity across ancient large transient warming events is a major challenge to the …