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Sufficient oxygen for animal respiration 1,400 million years ago

Proceedings of the National Academy of Sciences - PNAS, 2016-02, Vol.113 (7), p.1731-1736

2016

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Towards a quantitative understanding of the late Neoproterozoic carbon cycle

Proceedings of the National Academy of Sciences - PNAS, 2011-04, Vol.108 (14), p.5542-5547

2011

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Orbital forcing of climate 1.4 billion years ago

Proceedings of the National Academy of Sciences - PNAS, 2015-03, Vol.112 (12), p.E1406-E1413

2015

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Cold spells in the Nordic Seas during the early Eocene Greenhouse

Nature communications, 2020-09, Vol.11 (1), p.4713-4713, Article 4713

2020

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A sulfidic driver for the end-Ordovician mass extinction

Earth and planetary science letters, 2012-05, Vol.331-332, p.128-139

2012

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Development of Iron Speciation Reference Materials for Palaeoredox Analysis

Geostandards and geoanalytical research, 2020-09, Vol.44 (3), p.581-591

2020

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Tracing euxinia by molybdenum concentrations in sediments using handheld X-ray fluorescence spectroscopy (HHXRF)

Chemical geology, 2013-12, Vol.360-361, p.241-251

2013

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Ocean productivity before about 1.9 Gyr ago limited by phosphorus adsorption onto iron oxides

Nature (London), 2002-05, Vol.417 (6885), p.159-162

2002

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Constructing a model including the cryptic sulfur cycle in Chesapeake Bay requires judicious choices for key processes and parameters

MethodsX, 2023-12, Vol.11 (C), p.102253-102253, Article 102253

2023

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Massive dissociation of gas hydrate during a Jurassic oceanic anoxic event

Nature (London), 2000-07, Vol.406 (6794), p.392-395

2000

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Quantifying early marine diagenesis in shallow-water carbonate sediments

Geochimica et cosmochimica acta, 2018-09, Vol.236, p.140-159

2018

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Petrographic carbon in ancient sediments constrains Proterozoic Era atmospheric oxygen levels

Proceedings of the National Academy of Sciences - PNAS, 2021-06, Vol.118 (23)

2021

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Minimum levels of atmospheric oxygen from fossil tree roots imply new plant−oxygen feedback

Geobiology, 2021-05, Vol.19 (3), p.250-260

2021

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Reply to Planavsky et al.: Strong evidence for high atmospheric oxygen levels 1,400 million years ago

Proceedings of the National Academy of Sciences - PNAS, 2016-05, Vol.113 (19), p.E2552-E2553

2016

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A Mesoproterozoic iron formation

Proceedings of the National Academy of Sciences - PNAS, 2018-04, Vol.115 (17), p.E3895-E3904

2018

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Ocean subsurface warming as a mechanism for coupling Dansgaard-Oeschger climate cycles and ice-rafting events

Geophysical research letters, 2004-12, Vol.31 (24), p.L24202-n/a

2004

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No climate paradox under the faint early Sun

Nature (London), 2010-04, Vol.464 (7289), p.744-747

2010

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A new correlation of Triassic–Jurassic boundary successions in NW Europe, Nevada and Peru, and the Central Atlantic Magmatic Province: A time-line for the end-Triassic mass extinction

Palaeogeography, palaeoclimatology, palaeoecology, 2017-07, Vol.478, p.80-102

2017

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New insights into the burial history of organic carbon on the early Earth

Geochemistry, geophysics, geosystems : G3, 2004-08, Vol.5 (8), p.Q08001-n/a

2004

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Paleoenvironmental proxies and what the Xiamaling Formation tells us about the mid‐Proterozoic ocean

Geobiology, 2019-05, Vol.17 (3), p.225-246

2019

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Widespread seafloor anoxia during generation of the Ediacaran Shuram carbon isotope excursion

Geobiology, 2023-09, Vol.21 (5), p.556-570

2023

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Vulnerability of climate on Earth to sudden changes in insolation

Geophysical research letters, 2002-08, Vol.29 (15), p.1-1-1-4

2002

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Rosing, Bird, Sleep & Bjerrum reply

Nature (London), 2011-06, Vol.474 (7349), p.E4-E1

2011

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A model-based insight into the coupling of nitrogen and sulfur cycles in a coastal upwelling system

Journal of geophysical research. Biogeosciences, 2014-03, Vol.119 (3), p.264-285

2014

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Combined cadmium and chromium isotopes record a collapse of bioproductivity across the Cretaceous—Paleogene boundary in the Danish basin

Chemical geology, 2024-06, Vol.654, p.122058, Article 122058

2024

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Sufficient oxygen for animal respiration 1,400 million years ago

Towards a quantitative understanding of the late Neoproterozoic carbon cycle

Orbital forcing of climate 1.4 billion years ago

Cold spells in the Nordic Seas during the early Eocene Greenhouse

A sulfidic driver for the end-Ordovician mass extinction

Development of Iron Speciation Reference Materials for Palaeoredox Analysis

Tracing euxinia by molybdenum concentrations in sediments using handheld X-ray fluorescence spectroscopy (HHXRF)

Ocean productivity before about 1.9 Gyr ago limited by phosphorus adsorption onto iron oxides

Constructing a model including the cryptic sulfur cycle in Chesapeake Bay requires judicious choices for key processes and parameters

Massive dissociation of gas hydrate during a Jurassic oceanic anoxic event

Quantifying early marine diagenesis in shallow-water carbonate sediments

Petrographic carbon in ancient sediments constrains Proterozoic Era atmospheric oxygen levels

Minimum levels of atmospheric oxygen from fossil tree roots imply new plant−oxygen feedback

Reply to Planavsky et al.: Strong evidence for high atmospheric oxygen levels 1,400 million years ago

A Mesoproterozoic iron formation

Ocean subsurface warming as a mechanism for coupling Dansgaard-Oeschger climate cycles and ice-rafting events

No climate paradox under the faint early Sun

A new correlation of Triassic–Jurassic boundary successions in NW Europe, Nevada and Peru, and the Central Atlantic Magmatic Province: A time-line for the end-Triassic mass extinction

New insights into the burial history of organic carbon on the early Earth

Paleoenvironmental proxies and what the Xiamaling Formation tells us about the mid‐Proterozoic ocean

Widespread seafloor anoxia during generation of the Ediacaran Shuram carbon isotope excursion

Vulnerability of climate on Earth to sudden changes in insolation

Rosing, Bird, Sleep & Bjerrum reply

A model-based insight into the coupling of nitrogen and sulfur cycles in a coastal upwelling system

Combined cadmium and chromium isotopes record a collapse of bioproductivity across the Cretaceous—Paleogene boundary in the Danish basin

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