15 pages, 5 figuresThe Middle Pleistocene Transition (MPT, ~641–920 ka) represents a period of the Quaternary climate when, in the absence of substantial changes in orbital forcing, the climate progressively shifted to the 100 ka asymmetrical glacial–interglacial cyclicity characterizing the current climate. The causes of this change remain still uncertain but several lines of evidence suggested the carbon storage of the deep ocean played a relevant role. Here we evaluate the contribution of the eastern deep tropical Pacific to the global ocean carbon sequestration and storage between 760 and 1,040 ka. We present multi‐proxy records for export production and the redox environment at the seabed from Ocean Drilling Program Site 1242 located i...
The storage of inorganic carbon in the deep Pacific Ocean is thought to play an important role in re...
Ocean circulation critically affects the global climate and atmospheric carbon dioxide through redis...
To understand the whereabouts of CO2 during glacials and its pathways during deglacial transitions i...
As the largest reservoir of carbon exchanging with the atmosphere on glacial–interglacial timescales...
The authors acknowledge funding by the Spanish Ministry of Economy, Industry and Competitiveness thr...
Ventilation of carbon stored in the deep ocean is thought to play an important role in atmospheric C...
The ~100 k.y. cyclicity of the late Pleistocene ice ages started during the mid-Pleistocene transiti...
It has been shown that the deep Eastern Equatorial Pacific (EEP) region was poorly ventilated during...
Southern Ocean deep-water circulation plays an important role in the global carbon cycle. On geologi...
Southern Ocean deep-water circulation plays a vital role in the global carbon cycle. On geological t...
Author Posting. © American Geophysical Union, 2018. This article is posted here by permission of Am...
It has been hypothesized that the oceans store CO2 during glacial periods and then release it to the...
12th International Conference on Paleoceanography (ICP12), 29 August - 2 September 2016, UtrechtIt h...
Author Posting. © American Geophysical Union, 2021. This article is posted here by permission of Ame...
Funding information: This work was supported by grants from the National Science Foundation (OCE-201...
The storage of inorganic carbon in the deep Pacific Ocean is thought to play an important role in re...
Ocean circulation critically affects the global climate and atmospheric carbon dioxide through redis...
To understand the whereabouts of CO2 during glacials and its pathways during deglacial transitions i...
As the largest reservoir of carbon exchanging with the atmosphere on glacial–interglacial timescales...
The authors acknowledge funding by the Spanish Ministry of Economy, Industry and Competitiveness thr...
Ventilation of carbon stored in the deep ocean is thought to play an important role in atmospheric C...
The ~100 k.y. cyclicity of the late Pleistocene ice ages started during the mid-Pleistocene transiti...
It has been shown that the deep Eastern Equatorial Pacific (EEP) region was poorly ventilated during...
Southern Ocean deep-water circulation plays an important role in the global carbon cycle. On geologi...
Southern Ocean deep-water circulation plays a vital role in the global carbon cycle. On geological t...
Author Posting. © American Geophysical Union, 2018. This article is posted here by permission of Am...
It has been hypothesized that the oceans store CO2 during glacial periods and then release it to the...
12th International Conference on Paleoceanography (ICP12), 29 August - 2 September 2016, UtrechtIt h...
Author Posting. © American Geophysical Union, 2021. This article is posted here by permission of Ame...
Funding information: This work was supported by grants from the National Science Foundation (OCE-201...
The storage of inorganic carbon in the deep Pacific Ocean is thought to play an important role in re...
Ocean circulation critically affects the global climate and atmospheric carbon dioxide through redis...
To understand the whereabouts of CO2 during glacials and its pathways during deglacial transitions i...