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Paleocene/Eocene carbon feedbacks triggered by volcanic activity

Nature communications, 2021-08, Vol.12 (1), p.5186-5186, Article 5186

2021

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West Antarctic Ice Sheet retreat driven by Holocene warm water incursions

Nature (London), 2017-07, Vol.547 (7661), p.43-48

2017

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Closure of the Bering Strait caused Mid-Pleistocene Transition cooling

Nature communications, 2018-12, Vol.9 (1), p.5386-11, Article 5386

2018

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Oceanographic variability on the West Antarctic Peninsula during the Holocene and the influence of upper circumpolar deep water

Quaternary science reviews, 2015-07, Vol.119, p.54-65

2015

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Evolution of South Atlantic density and chemical stratification across the last deglaciation

Proceedings of the National Academy of Sciences - PNAS, 2016-01, Vol.113 (3), p.514-519

2016

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Palaeoclimatic implications of high-resolution clay mineral assemblages preceding and across the onset of the Palaeocene-Eocene Thermal Maximum, North Sea Basin

Clay minerals, 2016-12, Vol.51 (5), p.793-813

2016

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Pliocene‐Pleistocene evolution of sea surface and intermediate water temperatures from the southwest Pacific

Paleoceanography, 2016-06, Vol.31 (6), p.895-913

2016

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Mid Pleistocene foraminiferal mass extinction coupled with phytoplankton evolution

Nature communications, 2016-06, Vol.7 (1), p.11970-8, Article 11970

2016

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Benthic foraminifera indicate Glacial North Pacific Intermediate Water and reduced primary productivity over Bowers Ridge, Bering Sea, since the Mid-Brunhes Transition

Journal of micropalaeontology, 2019-12, Vol.38 (2), p.177-187

2019

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Neodymium Evidence for Increased Circumpolar Deep Water Flow to the North Pacific During the Middle Miocene Climate Transition

Paleoceanography and paleoclimatology, 2018-07, Vol.33 (7), p.672-682

2018

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Identification of the Storegga event offshore Shetland

Marine geology, 2024-08, Vol.474, p.107334, Article 107334

2024

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Pliocene agglutinated benthic Foraminifera from Site U1341 in the Bering Sea (IODP Expedition 323)

Geological quarterly (Warszawa ), 2013-04, Vol.57 (2)

2013

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Coupled climate and subarctic Pacific nutrient upwelling over the last 850,000 years

Earth and planetary science letters, 2019-09, Vol.522, p.87-97

2019

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Palaeoclimatic implications of highresolution clay mineral assemblages preceding and across the onset of the Palaeocene–Eocene Thermal Maximum, North Sea Basin

Clay minerals, 2016-12, Vol.51 (5), p.793-813

2016

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Multi-elemental composition of authigenic carbonates in benthic foraminifera from the eastern Bering Sea continental margin (International Ocean Discovery Program Site U1343)

Geochimica et cosmochimica acta, 2020-01, Vol.268, p.1-21

2020

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Sea-ice response to climate change in the Bering Sea during the Mid-Pleistocene Transition

Quaternary science reviews, 2021-05, Vol.259, p.106918, Article 106918

2021

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Climate and environment of a Pliocene warm world

Palaeogeography, palaeoclimatology, palaeoecology, 2011-08, Vol.309 (1), p.1-8

2011

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Sensitivity of Pliocene ice sheets to orbital forcing

Palaeogeography, palaeoclimatology, palaeoecology, 2011-08, Vol.309 (1), p.98-110

2011

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Reduced upwelling of nutrient and carbon-rich water in the subarctic Pacific during the Mid-Pleistocene Transition

Palaeogeography, palaeoclimatology, palaeoecology, 2020-10, Vol.555, p.109845, Article 109845

2020

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Late quaternary sea-ice and sedimentary redox conditions in the eastern Bering Sea – Implications for ventilation of the mid-depth North Pacific and an Atlantic-Pacific seesaw mechanism

Quaternary science reviews, 2020-11, Vol.248, p.106549, Article 106549

2020

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Deep ocean carbonate ion increase during mid Miocene CO2 decline

Scientific reports, 2014-02, Vol.4 (1), p.4187, Article 4187

2014

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Antarctic Intermediate Water properties since 400 ka recorded in infaunal (Uvigerina peregrina) and epifaunal (Planulina wuellerstorfi) benthic foraminifera

Earth and planetary science letters, 2015-10, Vol.428, p.193-203

2015

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Isotopic and palynological evidence for a new Early Jurassic environmental perturbation

Palaeogeography, palaeoclimatology, palaeoecology, 2013-03, Vol.374, p.16-27

2013

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Modern deep-water agglutinated Foraminifera from IODP Expedition 323, Bering Sea; ecological and taxonomic implications

Journal of micropalaeontology, 2017-07, Vol.36 (2), p.195-218

2017

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Sea surface temperatures of the mid-Piacenzian Warm Period: A comparison of PRISM3 and HadCM3

Palaeogeography, palaeoclimatology, palaeoecology, 2011-08, Vol.309 (1), p.83-91

2011

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Paleocene/Eocene carbon feedbacks triggered by volcanic activity

West Antarctic Ice Sheet retreat driven by Holocene warm water incursions

Closure of the Bering Strait caused Mid-Pleistocene Transition cooling

Oceanographic variability on the West Antarctic Peninsula during the Holocene and the influence of upper circumpolar deep water

Evolution of South Atlantic density and chemical stratification across the last deglaciation

Palaeoclimatic implications of high-resolution clay mineral assemblages preceding and across the onset of the Palaeocene-Eocene Thermal Maximum, North Sea Basin

Pliocene‐Pleistocene evolution of sea surface and intermediate water temperatures from the southwest Pacific

Mid Pleistocene foraminiferal mass extinction coupled with phytoplankton evolution

Benthic foraminifera indicate Glacial North Pacific Intermediate Water and reduced primary productivity over Bowers Ridge, Bering Sea, since the Mid-Brunhes Transition

Neodymium Evidence for Increased Circumpolar Deep Water Flow to the North Pacific During the Middle Miocene Climate Transition

Identification of the Storegga event offshore Shetland

Pliocene agglutinated benthic Foraminifera from Site U1341 in the Bering Sea (IODP Expedition 323)

Coupled climate and subarctic Pacific nutrient upwelling over the last 850,000 years

Palaeoclimatic implications of highresolution clay mineral assemblages preceding and across the onset of the Palaeocene–Eocene Thermal Maximum, North Sea Basin

Multi-elemental composition of authigenic carbonates in benthic foraminifera from the eastern Bering Sea continental margin (International Ocean Discovery Program Site U1343)

Sea-ice response to climate change in the Bering Sea during the Mid-Pleistocene Transition

Climate and environment of a Pliocene warm world

Sensitivity of Pliocene ice sheets to orbital forcing

Reduced upwelling of nutrient and carbon-rich water in the subarctic Pacific during the Mid-Pleistocene Transition

Late quaternary sea-ice and sedimentary redox conditions in the eastern Bering Sea – Implications for ventilation of the mid-depth North Pacific and an Atlantic-Pacific seesaw mechanism

Deep ocean carbonate ion increase during mid Miocene CO2 decline

Antarctic Intermediate Water properties since 400 ka recorded in infaunal (Uvigerina peregrina) and epifaunal (Planulina wuellerstorfi) benthic foraminifera

Isotopic and palynological evidence for a new Early Jurassic environmental perturbation

Modern deep-water agglutinated Foraminifera from IODP Expedition 323, Bering Sea; ecological and taxonomic implications

Sea surface temperatures of the mid-Piacenzian Warm Period: A comparison of PRISM3 and HadCM3

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