[PDF][PDF] On carbon burial and net primary production through Earth's history
The carbonate carbon isotope record has been traditionally interpreted as evidence of
stability in the globally integrated ratio of organic to total carbon burial from Earth9s surface …
stability in the globally integrated ratio of organic to total carbon burial from Earth9s surface …
Decadal variability in twentieth-century ocean acidification in the California Current Ecosystem
Oceanic uptake of CO2 can mitigate climate change, but also results in global ocean
acidification. Ocean acidification-related changes to the marine carbonate system can …
acidification. Ocean acidification-related changes to the marine carbonate system can …
Cd/Ca in late Miocene benthic foraminifera and changes in the global organic carbon budget
ML Delaney, EA Boyle - Nature, 1987 - nature.com
The late Miocene carbon shift (∼ 6.2 Myr)—a 0.5–1.0‰, δ13C decrease in benthic and
planktonic foraminifera—has been ascribed to changes in global inventory, deep-ocean …
planktonic foraminifera—has been ascribed to changes in global inventory, deep-ocean …
Anthropogenic CO2 invasion into the northeast Pacific based on concurrent δ13CDIC and nutrient profiles from the California Current
The stable isotopic signature of dissolved inorganic carbon (δ13CDIC) in the northeast
Pacific Ocean is lower in near‐surface waters by≈ 1.1‰ relative to values predicted from …
Pacific Ocean is lower in near‐surface waters by≈ 1.1‰ relative to values predicted from …
Similar glacial and Holocene deep water circulation inferred from southeast Pacific benthic foraminiferal carbon isotope composition
K Matsumoto, J Lynch‐Stieglitz - Paleoceanography, 1999 - Wiley Online Library
We present Holocene and last glacial maximum (LGM) oxygen and carbon isotope
measurements on Planulina wuellerstorfi in six southeast Pacific cores. Sedimentation rates …
measurements on Planulina wuellerstorfi in six southeast Pacific cores. Sedimentation rates …
New constraints on massive carbon release and recovery processes during the Paleocene-Eocene Thermal Maximum
Recent geochemical and sedimentological evidence constrains the response of seawater
chemistry to carbon injection during the Paleocene-Eocene Thermal Maximum (PETM) …
chemistry to carbon injection during the Paleocene-Eocene Thermal Maximum (PETM) …
[HTML][HTML] Biological and physical controls in the Southern Ocean on past millennial-scale atmospheric CO2 changes
Millennial-scale climate changes during the last glacial period and deglaciation were
accompanied by rapid changes in atmospheric CO2 that remain unexplained. While the role …
accompanied by rapid changes in atmospheric CO2 that remain unexplained. While the role …
Deep Pacific CaCO3 compensation and glacial–interglacial atmospheric CO2
Benthic foraminiferal δ13C suggests that there was a net shift of isotopically light metabolic
CO2 from the upper ocean into the deep ocean during the last glacial period. According to …
CO2 from the upper ocean into the deep ocean during the last glacial period. According to …
Marine carbon burial flux and the carbon isotope record of Late Cretaceous (Coniacian–Santonian) Oceanic Anoxic Event III
R Locklair, B Sageman, A Lerman - Sedimentary Geology, 2011 - Elsevier
Episodes of widespread distribution of organic-rich marine facies within relatively narrow
stratigraphic intervals have been interpreted as Oceanic Anoxic Events (OAEs). There are a …
stratigraphic intervals have been interpreted as Oceanic Anoxic Events (OAEs). There are a …
Millennial and centennial CO2 release from the Southern Ocean during the last deglaciation
For its greenhouse effects, atmospheric CO2 can critically influence the global climate on
millennial and centennial timescales. Pleistocene atmospheric CO2 variations must involve …
millennial and centennial timescales. Pleistocene atmospheric CO2 variations must involve …