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Temperature control on CO2 emissions from the weathering of sedimentary rocks

Nature geoscience, 2021-09, Vol.14 (9), p.665-671

2021

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Deep instability of deforested tropical peatlands revealed by fluvial organic carbon fluxes

Nature (London), 2013-01, Vol.493 (7434), p.660-663

2013

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East Siberian Arctic inland waters emit mostly contemporary carbon

Nature communications, 2020-04, Vol.11 (1), p.1627-1627, Article 1627

2020

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UK peatland streams release old carbon dioxide to the atmosphere and young dissolved organic carbon to rivers

Geophysical research letters, 2007-12, Vol.34 (23), p.L23401-n/a

2007

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A Previously Undescribed Helotialean Fungus That Is Superabundant in Soil Under Maritime Antarctic Higher Plants

Frontiers in microbiology, 2020-12, Vol.11, p.615608-615608

2020

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The Potential Hidden Age of Dissolved Organic Carbon Exported by Peatland Streams

Journal of geophysical research. Biogeosciences, 2019-02, Vol.124 (2), p.328-341

2019

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Publisher Correction: East Siberian Arctic inland waters emit mostly contemporary carbon

Nature communications, 2020-04, Vol.11 (1), p.2048-2048, Article 2048

2020

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Assessing the Potential for Mobilization of Old Soil Carbon After Permafrost Thaw: A Synthesis of 14C Measurements From the Northern Permafrost Region

Global biogeochemical cycles, 2020-09, Vol.34 (9), p.n/a

2020

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Blue carbon additionality: New insights from the radiocarbon content of saltmarsh soils and their respired CO2

Limnology and oceanography, 2024-03, Vol.69 (3), p.548-561

2024

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Heterotrophic microbial communities use ancient carbon following glacial retreat

Biology letters (2005), 2007-10, Vol.3 (5), p.487-490

2007

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No evidence for increased loss of old carbon in a temperate organic soil after 13 years of simulated climatic warming despite increased CO 2 emissions

Global change biology, 2021-05, Vol.27 (9), p.1836-1847

2021

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Vascular plants promote ancient peatland carbon loss with climate warming

Global change biology, 2016-05, Vol.22 (5), p.1880-1889

2016

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Plant carbon allocation drives turnover of old soil organic matter in permafrost tundra soils

Global change biology, 2020-08, Vol.26 (8), p.4559-4571

2020

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Vascular plant‐mediated controls on atmospheric carbon assimilation and peat carbon decomposition under climate change

Global change biology, 2018-09, Vol.24 (9), p.3911-3921

2018

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Discrete taxa of saprotrophic fungi respire different ages of carbon from Antarctic soils

Scientific reports, 2018-05, Vol.8 (1), p.7866-10, Article 7866

2018

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Sources and controls of greenhouse gases and heavy metals in mine water: A continuing climate legacy

The Science of the total environment, 2024-01, Vol.906, p.167371-167371, Article 167371

2024

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No evidence for increased loss of old carbon in a temperate organic soil after 13 years of simulated climatic warming despite increased CO2 emissions

Global change biology, 2021-05, Vol.27 (9), p.1836-1847

2021

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Tropical forest soil carbon stocks do not increase despite 15 years of doubled litter inputs

Scientific reports, 2019-12, Vol.9 (1), p.18030-18030, Article 18030

2019

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Aquatic export of young dissolved and gaseous carbon from a pristine boreal fen: Implications for peat carbon stock stability

Global change biology, 2017-12, Vol.23 (12), p.5523-5536

2017

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Invertebrates increase the sensitivity of non-labile soil carbon to climate change

Soil biology & biochemistry, 2007-03, Vol.39 (3), p.816-818

2007

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Radiocarbon analysis reveals that vegetation facilitates the release of old methane in a temperate raised bog

Biogeochemistry, 2020-03, Vol.148 (1), p.1-17

2020

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A potential loss of carbon associated with greater plant growth in the European Arctic

Nature climate change, 2012-12, Vol.2 (12), p.875-879

2012

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Limited contribution of permafrost carbon to methane release from thawing peatlands

Nature climate change, 2017-07, Vol.7 (7), p.507-511

2017

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C mobilisation in disturbed tropical peat swamps: old DOC can fuel the fluvial efflux of old carbon dioxide, but site recovery can occur

Scientific reports, 2019-08, Vol.9 (1), p.11429-12, Article 11429

2019

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Soil microbial respiration in arctic soil does not acclimate to temperature

Ecology letters, 2008-10, Vol.11 (10), p.1092-1100

2008

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Temperature control on CO2 emissions from the weathering of sedimentary rocks

Deep instability of deforested tropical peatlands revealed by fluvial organic carbon fluxes

East Siberian Arctic inland waters emit mostly contemporary carbon

UK peatland streams release old carbon dioxide to the atmosphere and young dissolved organic carbon to rivers

A Previously Undescribed Helotialean Fungus That Is Superabundant in Soil Under Maritime Antarctic Higher Plants

The Potential Hidden Age of Dissolved Organic Carbon Exported by Peatland Streams

Publisher Correction: East Siberian Arctic inland waters emit mostly contemporary carbon

Assessing the Potential for Mobilization of Old Soil Carbon After Permafrost Thaw: A Synthesis of 14C Measurements From the Northern Permafrost Region

Blue carbon additionality: New insights from the radiocarbon content of saltmarsh soils and their respired CO2

Heterotrophic microbial communities use ancient carbon following glacial retreat

No evidence for increased loss of old carbon in a temperate organic soil after 13 years of simulated climatic warming despite increased CO 2 emissions

Vascular plants promote ancient peatland carbon loss with climate warming

Plant carbon allocation drives turnover of old soil organic matter in permafrost tundra soils

Vascular plant‐mediated controls on atmospheric carbon assimilation and peat carbon decomposition under climate change

Discrete taxa of saprotrophic fungi respire different ages of carbon from Antarctic soils

Sources and controls of greenhouse gases and heavy metals in mine water: A continuing climate legacy

No evidence for increased loss of old carbon in a temperate organic soil after 13 years of simulated climatic warming despite increased CO2 emissions

Tropical forest soil carbon stocks do not increase despite 15 years of doubled litter inputs

Aquatic export of young dissolved and gaseous carbon from a pristine boreal fen: Implications for peat carbon stock stability

Invertebrates increase the sensitivity of non-labile soil carbon to climate change

Radiocarbon analysis reveals that vegetation facilitates the release of old methane in a temperate raised bog

A potential loss of carbon associated with greater plant growth in the European Arctic

Limited contribution of permafrost carbon to methane release from thawing peatlands

C mobilisation in disturbed tropical peat swamps: old DOC can fuel the fluvial efflux of old carbon dioxide, but site recovery can occur

Soil microbial respiration in arctic soil does not acclimate to temperature

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