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Carbon dioxide forcing alone insufficient to explain Palaeocene-Eocene Thermal Maximum warming

Nature geoscience, 2009-08, Vol.2 (8), p.576-580

2009

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Environmental precursors to rapid light carbon injection at the Palaeocene/Eocene boundary

Nature, 2007-12, Vol.450 (7173), p.1218-1221

2007

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Eocene (46–44 Ma) Onset of Australia‐Pacific Plate Motion in the Southwest Pacific Inferred From Stratigraphy in New Caledonia and New Zealand

Geochemistry, geophysics, geosystems : G3, 2020-07, Vol.21 (7), p.n/a

2020

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Arctic hydrology during global warming at the Palaeocene/Eocene thermal maximum

Nature, 2006-08, Vol.442 (7103), p.671-675

2006

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Gas hydrate dissociation prolongs acidification of the Anthropocene oceans

Geophysical research letters, 2015-11, Vol.42 (21), p.9337-9344

2015

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Onset of carbon isotope excursion at the Paleocene-Eocene thermal maximum took millennia, not 13 years

Proceedings of the National Academy of Sciences - PNAS, 2014-03, Vol.111 (12), p.E1062-E1063

2014

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Pore water geochemistry along continental slopes north of the East Siberian Sea: inference of low methane concentrations

Biogeosciences, 2017-06, Vol.14 (12), p.2929-2953

2017

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Large-Amplitude Variations in Carbon Cycling and Terrestrial Weathering during the Latest Paleocene and Earliest Eocene: The Record at Mead Stream, New Zealand

The Journal of geology, 2012-09, Vol.120 (5), p.487-505

2012

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The Source and Fate of Massive Carbon Input During the Latest Paleocene Thermal Maximum

Science (American Association for the Advancement of Science), 1999-11, Vol.286 (5444), p.1531-1533

1999

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Stable isotope and calcareous nannofossil assemblage record of the late Paleocene and early Eocene (Cicogna section)

Climate of the past, 2016-04, Vol.12 (4), p.883-909

2016

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Constraints on ocean acidification associated with rapid and massive carbon injections: The early Paleogene record at ocean drilling program site 1215, equatorial Pacific Ocean

Palaeogeography, palaeoclimatology, palaeoecology, 2010-12, Vol.298 (3), p.409-420

2010

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A blast of gas in the latest Paleocene: simulating first-order effects of massive dissociation of oceanic methane hydrate

Geology (Boulder), 1997-03, Vol.25 (3), p.259

1997

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Sulfate-methane transition as a proxy for average methane hydrate saturation in marine sediments

Geophysical research letters, 2008-02, Vol.35 (3), p.L03611-n/a

2008

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The Apectodinium acme and terrestrial discharge during the Paleocene–Eocene thermal maximum: new palynological, geochemical and calcareous nannoplankton observations at Tawanui, New Zealand

Palaeogeography, palaeoclimatology, palaeoecology, 2003-05, Vol.194 (4), p.387-403

2003

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Neogene evolution of the mixed carbonate-siliciclastic system in the Gulf of Papua, Papua New Guinea

Journal of Geophysical Research - Earth Surface, 2008-03, Vol.113 (F1), p.F01S21-n/a

2008

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Did Photosymbiont Bleaching Lead to the Demise of Planktic Foraminifer Morozovella at the Early Eocene Climatic Optimum?

Paleoceanography, 2017-11, Vol.32 (11), p.1115-1136

2017

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Bundled turbidite deposition in the central Pandora Trough (Gulf of Papua) since Last Glacial Maximum: Linking sediment nature and accumulation to sea level fluctuations at millennial timescale

Journal of Geophysical Research - Earth Surface, 2008-03, Vol.113 (F1), p.F01S19-n/a

2008

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Deep water geomorphology of the mixed siliciclastic-carbonate system, Gulf of Papua

Journal of Geophysical Research - Earth Surface, 2008-03, Vol.113 (F1), p.F01S16-n/a

2008

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Rhizon sampling of pore waters on scientific drilling expeditions : An example from the IODP expedition 302, arctic coring expedition (ACEX)

Scientific drilling (Hokkaido, Japan), 2007-03 (4), p.22-25

2007

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Methane hydrate stability in seawater

Geophysical research letters, 1994-09, Vol.21 (19), p.2115-2118

1994

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Major perturbations in the global carbon cycle and photosymbiont-bearing planktic foraminifera during the early Eocene

Climate of the past, 2016-01, Vol.12 (4), p.981-1007

2016

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An alternative model for CaCO3 over-shooting during the PETM: Biological carbonate compensation

Earth and planetary science letters, 2016-11, Vol.453, p.223-233

2016

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Pore water sulfate, alkalinity, and carbon isotope profiles in shallow sediment above marine gas hydrate systems: A numerical modeling perspective

Journal of Geophysical Research, 2011-09, Vol.116 (B9), p.n/a, Article B09103

2011

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Subtropical Arctic Ocean temperatures during the Palaeocene/Eocene thermal maximum

Nature, 2006-06, Vol.441 (7093), p.610-613

2006

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Einstellungen

Carbon dioxide forcing alone insufficient to explain Palaeocene-Eocene Thermal Maximum warming

Environmental precursors to rapid light carbon injection at the Palaeocene/Eocene boundary

Eocene (46–44 Ma) Onset of Australia‐Pacific Plate Motion in the Southwest Pacific Inferred From Stratigraphy in New Caledonia and New Zealand

The Cenozoic palaeoenvironment of the Arctic Ocean

Arctic hydrology during global warming at the Palaeocene/Eocene thermal maximum

Gas hydrate dissociation prolongs acidification of the Anthropocene oceans

Onset of carbon isotope excursion at the Paleocene-Eocene thermal maximum took millennia, not 13 years

Pore water geochemistry along continental slopes north of the East Siberian Sea: inference of low methane concentrations

Large-Amplitude Variations in Carbon Cycling and Terrestrial Weathering during the Latest Paleocene and Earliest Eocene: The Record at Mead Stream, New Zealand

The Source and Fate of Massive Carbon Input During the Latest Paleocene Thermal Maximum

Stable isotope and calcareous nannofossil assemblage record of the late Paleocene and early Eocene (Cicogna section)

Constraints on ocean acidification associated with rapid and massive carbon injections: The early Paleogene record at ocean drilling program site 1215, equatorial Pacific Ocean

A blast of gas in the latest Paleocene: simulating first-order effects of massive dissociation of oceanic methane hydrate

Sulfate-methane transition as a proxy for average methane hydrate saturation in marine sediments

The Apectodinium acme and terrestrial discharge during the Paleocene–Eocene thermal maximum: new palynological, geochemical and calcareous nannoplankton observations at Tawanui, New Zealand

Neogene evolution of the mixed carbonate-siliciclastic system in the Gulf of Papua, Papua New Guinea

Did Photosymbiont Bleaching Lead to the Demise of Planktic Foraminifer Morozovella at the Early Eocene Climatic Optimum?

Bundled turbidite deposition in the central Pandora Trough (Gulf of Papua) since Last Glacial Maximum: Linking sediment nature and accumulation to sea level fluctuations at millennial timescale

Deep water geomorphology of the mixed siliciclastic-carbonate system, Gulf of Papua

Rhizon sampling of pore waters on scientific drilling expeditions : An example from the IODP expedition 302, arctic coring expedition (ACEX)

Methane hydrate stability in seawater

Major perturbations in the global carbon cycle and photosymbiont-bearing planktic foraminifera during the early Eocene

An alternative model for CaCO3 over-shooting during the PETM: Biological carbonate compensation

Pore water sulfate, alkalinity, and carbon isotope profiles in shallow sediment above marine gas hydrate systems: A numerical modeling perspective

Subtropical Arctic Ocean temperatures during the Palaeocene/Eocene thermal maximum

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