1
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Duan X, Yin P, Tsona N, Cao K, Xie Y, He X, Chen B, Chen J, Gao F, Yang L, Lv S. Biogenic methane in coastal unconsolidated sediment systems: A review. ENVIRONMENTAL RESEARCH 2023; 227:115803. [PMID: 37003546 DOI: 10.1016/j.envres.2023.115803] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Received: 01/27/2023] [Revised: 03/20/2023] [Accepted: 03/29/2023] [Indexed: 05/08/2023]
Abstract
Marine sediments are the world's largest known reservoir of methane. In many coastal regions, methane is trapped in sediments buried at depths ranging from centimeters to hundreds of meters below the seafloor, in the forms of gas pockets, dispersed gas bubbles and dissolved gas, also known as shallow gas (methane-dominated gas mixture). The existence of shallow gas affects the engineering geological environment and threatens the safety of artificial facilities. The escape of shallow gas from sediments into the atmosphere can even threaten ecosystem security and affect global climate change. However, until now, shallow gas has remained a mystery to the scientific community. For example, how it is generated, how it distributes and migrates in sediments, and what are the factors that influence these processes that are still unclear. In the context of increasingly intense offshore development and global warming, there is a huge gap between existing scientific understanding of shallow gas and the need to develop scientific solutions for related problems. Based on this, this paper systematically collects the information on all aspects of shallow gas mentioned above, comprehensively summarizes the current scientific understanding, and analyzes the existing shortcomings, which will provide systematic references for the research on environmental disaster prevention, engineering technology, climate change, and other fields.
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Affiliation(s)
- Xiaoyong Duan
- Qingdao Institute of Marine Geology, China Geological Survey, Qingdao, 266237, China; Zhoushan Field Scientific Observation and Research Station for Marine Geo-hazards, China Geological Survey, Qingdao, 266237, China.
| | - Ping Yin
- Qingdao Institute of Marine Geology, China Geological Survey, Qingdao, 266237, China; Zhoushan Field Scientific Observation and Research Station for Marine Geo-hazards, China Geological Survey, Qingdao, 266237, China.
| | - Narcisse Tsona
- Environment Research Institute, Shandong University. Qingdao, 266237, China
| | - Ke Cao
- Qingdao Institute of Marine Geology, China Geological Survey, Qingdao, 266237, China; Zhoushan Field Scientific Observation and Research Station for Marine Geo-hazards, China Geological Survey, Qingdao, 266237, China
| | - Yongqing Xie
- Zhoushan Field Scientific Observation and Research Station for Marine Geo-hazards, China Geological Survey, Qingdao, 266237, China; Donghai Laboratory, Zhoushan, Zhejiang, 316021, China; Zhejiang Institute of Marine Geology Survey, Zhoushan, Zhejiang, 316021, China; Zhejiang Engineering Survey and Design Institute Group CO. LTD, Ningbo, Zhejiang, 315012, China
| | - Xingliang He
- Qingdao Institute of Marine Geology, China Geological Survey, Qingdao, 266237, China; Zhoushan Field Scientific Observation and Research Station for Marine Geo-hazards, China Geological Survey, Qingdao, 266237, China
| | - Bin Chen
- Qingdao Institute of Marine Geology, China Geological Survey, Qingdao, 266237, China; Zhoushan Field Scientific Observation and Research Station for Marine Geo-hazards, China Geological Survey, Qingdao, 266237, China
| | - Junbing Chen
- Zhoushan Field Scientific Observation and Research Station for Marine Geo-hazards, China Geological Survey, Qingdao, 266237, China; Zhejiang Institute of Hydrogeology and Engineering Geology, Ningbo, 315012, China
| | - Fei Gao
- Qingdao Institute of Marine Geology, China Geological Survey, Qingdao, 266237, China; Zhoushan Field Scientific Observation and Research Station for Marine Geo-hazards, China Geological Survey, Qingdao, 266237, China
| | - Lei Yang
- Zhoushan Field Scientific Observation and Research Station for Marine Geo-hazards, China Geological Survey, Qingdao, 266237, China; Donghai Laboratory, Zhoushan, Zhejiang, 316021, China; Zhejiang Institute of Marine Geology Survey, Zhoushan, Zhejiang, 316021, China; Zhejiang Engineering Survey and Design Institute Group CO. LTD, Ningbo, Zhejiang, 315012, China
| | - Shenghua Lv
- Qingdao Institute of Marine Geology, China Geological Survey, Qingdao, 266237, China; Zhoushan Field Scientific Observation and Research Station for Marine Geo-hazards, China Geological Survey, Qingdao, 266237, China
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2
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Assessing the Benthic Response to Climate-Driven Methane Hydrate Destabilisation: State of the Art and Future Modelling Perspectives. ENERGIES 2022. [DOI: 10.3390/en15093307] [Citation(s) in RCA: 2] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 01/25/2023]
Abstract
Modern observations and geological records suggest that anthropogenic ocean warming could destabilise marine methane hydrate, resulting in methane release from the seafloor to the ocean-atmosphere, and potentially triggering a positive feedback on global temperature. On the decadal to millennial timescales over which hydrate-sourced methane release is hypothesized to occur, several processes consuming methane below and above the seafloor have the potential to slow, reduce or even prevent such release. Yet, the modulating effect of these processes on seafloor methane emissions remains poorly quantified, and the full impact of benthic methane consumption on ocean carbon chemistry is still to be explored. In this review, we document the dynamic interplay between hydrate thermodynamics, benthic transport and biogeochemical reaction processes, that ultimately determines the impact of hydrate destabilisation on seafloor methane emissions and the ocean carbon cycle. Then, we provide an overview of how state-of-the-art numerical models treat such processes and examine their ability to quantify hydrate-sourced methane emissions from the seafloor, as well as their impact on benthic biogeochemical cycling. We discuss the limitations of current models in coupling the dynamic interplay between hydrate thermodynamics and the different reaction and transport processes that control the efficiency of the benthic sink, and highlight their shortcoming in assessing the full implication of methane release on ocean carbon cycling. Finally, we recommend that current Earth system models explicitly account for hydrate driven benthic-pelagic exchange fluxes to capture potential hydrate-carbon cycle-climate feed-backs.
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3
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Using the BFAST Algorithm and Multitemporal AIRS Data to Investigate Variation of Atmospheric Methane Concentration over Zoige Wetland of China. REMOTE SENSING 2020. [DOI: 10.3390/rs12193199] [Citation(s) in RCA: 3] [Impact Index Per Article: 0.8] [Reference Citation Analysis] [Abstract] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 11/17/2022]
Abstract
The monitoring of wetland methane (CH4) emission is essential in the context of global CH4 emission and climate change. The remotely sensed multitemporal Atmospheric Infrared Sounder (AIRS) CH4 data and the Breaks for Additive Season and Trend (BFAST) algorithm were used to detect atmospheric CH4 dynamics in the Zoige wetland, China between 2002 and 2018. The overall atmospheric CH4 concentration increased steadily with a rate of 5.7 ± 0.3 ppb/year. After decomposing the time-series of CH4 data using the BFAST algorithm, we found no anomalies in the seasonal and error components. The trend component increased with time, and a total of seven breaks were detected within four cells. Six were well-explained by the air temperature anomalies primarily, but one break was not. The effect of parameter h on decomposition outcomes was studied because it could influence the number of breaks in the trend component. As h increased, the number of breaks decreased. The interplays of the observations of interest, break numbers, and statistical significance should determine the h value.
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4
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Dyonisius MN, Petrenko VV, Smith AM, Hua Q, Yang B, Schmitt J, Beck J, Seth B, Bock M, Hmiel B, Vimont I, Menking JA, Shackleton SA, Baggenstos D, Bauska TK, Rhodes RH, Sperlich P, Beaudette R, Harth C, Kalk M, Brook EJ, Fischer H, Severinghaus JP, Weiss RF. Old carbon reservoirs were not important in the deglacial methane budget. Science 2020; 367:907-910. [PMID: 32079770 DOI: 10.1126/science.aax0504] [Citation(s) in RCA: 34] [Impact Index Per Article: 8.5] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 02/19/2019] [Accepted: 01/06/2020] [Indexed: 11/02/2022]
Abstract
Permafrost and methane hydrates are large, climate-sensitive old carbon reservoirs that have the potential to emit large quantities of methane, a potent greenhouse gas, as the Earth continues to warm. We present ice core isotopic measurements of methane (Δ14C, δ13C, and δD) from the last deglaciation, which is a partial analog for modern warming. Our results show that methane emissions from old carbon reservoirs in response to deglacial warming were small (<19 teragrams of methane per year, 95% confidence interval) and argue against similar methane emissions in response to future warming. Our results also indicate that methane emissions from biomass burning in the pre-Industrial Holocene were 22 to 56 teragrams of methane per year (95% confidence interval), which is comparable to today.
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Affiliation(s)
- M N Dyonisius
- Department of Earth and Environmental Sciences, University of Rochester, Rochester, NY 14627, USA.
| | - V V Petrenko
- Department of Earth and Environmental Sciences, University of Rochester, Rochester, NY 14627, USA
| | - A M Smith
- Australian Nuclear Science and Technology Organisation (ANSTO), Lucas Heights, NSW 2234, Australia
| | - Q Hua
- Australian Nuclear Science and Technology Organisation (ANSTO), Lucas Heights, NSW 2234, Australia
| | - B Yang
- Australian Nuclear Science and Technology Organisation (ANSTO), Lucas Heights, NSW 2234, Australia
| | - J Schmitt
- Climate and Environmental Physics, Physics Institute and Oeschger Centre for Climate Change Research, University of Bern, CH-3012 Bern, Switzerland
| | - J Beck
- Climate and Environmental Physics, Physics Institute and Oeschger Centre for Climate Change Research, University of Bern, CH-3012 Bern, Switzerland
| | - B Seth
- Climate and Environmental Physics, Physics Institute and Oeschger Centre for Climate Change Research, University of Bern, CH-3012 Bern, Switzerland
| | - M Bock
- Climate and Environmental Physics, Physics Institute and Oeschger Centre for Climate Change Research, University of Bern, CH-3012 Bern, Switzerland
| | - B Hmiel
- Department of Earth and Environmental Sciences, University of Rochester, Rochester, NY 14627, USA
| | - I Vimont
- Institute of Arctic and Alpine Research, University of Colorado Boulder, Boulder, CO 80303, USA
| | - J A Menking
- College of Earth, Ocean and Atmospheric Sciences, Oregon State University, Corvallis, OR 97331, USA
| | - S A Shackleton
- Scripps Institution of Oceanography (SIO), University of California, San Diego, La Jolla, CA 92037, USA
| | - D Baggenstos
- Climate and Environmental Physics, Physics Institute and Oeschger Centre for Climate Change Research, University of Bern, CH-3012 Bern, Switzerland.,Scripps Institution of Oceanography (SIO), University of California, San Diego, La Jolla, CA 92037, USA
| | - T K Bauska
- College of Earth, Ocean and Atmospheric Sciences, Oregon State University, Corvallis, OR 97331, USA.,British Antarctic Survey High Cross, Cambridge CB3 0ET, UK
| | - R H Rhodes
- College of Earth, Ocean and Atmospheric Sciences, Oregon State University, Corvallis, OR 97331, USA.,Department of Earth Sciences, University of Cambridge, Cambridge CB2 3EQ, UK
| | - P Sperlich
- National Institute of Water and Atmospheric Research (NIWA), 6021 Wellington, New Zealand
| | - R Beaudette
- Scripps Institution of Oceanography (SIO), University of California, San Diego, La Jolla, CA 92037, USA
| | - C Harth
- Scripps Institution of Oceanography (SIO), University of California, San Diego, La Jolla, CA 92037, USA
| | - M Kalk
- College of Earth, Ocean and Atmospheric Sciences, Oregon State University, Corvallis, OR 97331, USA
| | - E J Brook
- College of Earth, Ocean and Atmospheric Sciences, Oregon State University, Corvallis, OR 97331, USA
| | - H Fischer
- Climate and Environmental Physics, Physics Institute and Oeschger Centre for Climate Change Research, University of Bern, CH-3012 Bern, Switzerland
| | - J P Severinghaus
- Scripps Institution of Oceanography (SIO), University of California, San Diego, La Jolla, CA 92037, USA
| | - R F Weiss
- Scripps Institution of Oceanography (SIO), University of California, San Diego, La Jolla, CA 92037, USA
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5
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Preindustrial 14CH 4 indicates greater anthropogenic fossil CH 4 emissions. Nature 2020; 578:409-412. [PMID: 32076219 DOI: 10.1038/s41586-020-1991-8] [Citation(s) in RCA: 110] [Impact Index Per Article: 27.5] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 05/27/2019] [Accepted: 11/27/2019] [Indexed: 11/08/2022]
Abstract
Atmospheric methane (CH4) is a potent greenhouse gas, and its mole fraction has more than doubled since the preindustrial era1. Fossil fuel extraction and use are among the largest anthropogenic sources of CH4 emissions, but the precise magnitude of these contributions is a subject of debate2,3. Carbon-14 in CH4 (14CH4) can be used to distinguish between fossil (14C-free) CH4 emissions and contemporaneous biogenic sources; however, poorly constrained direct 14CH4 emissions from nuclear reactors have complicated this approach since the middle of the 20th century4,5. Moreover, the partitioning of total fossil CH4 emissions (presently 172 to 195 teragrams CH4 per year)2,3 between anthropogenic and natural geological sources (such as seeps and mud volcanoes) is under debate; emission inventories suggest that the latter account for about 40 to 60 teragrams CH4 per year6,7. Geological emissions were less than 15.4 teragrams CH4 per year at the end of the Pleistocene, about 11,600 years ago8, but that period is an imperfect analogue for present-day emissions owing to the large terrestrial ice sheet cover, lower sea level and extensive permafrost. Here we use preindustrial-era ice core 14CH4 measurements to show that natural geological CH4 emissions to the atmosphere were about 1.6 teragrams CH4 per year, with a maximum of 5.4 teragrams CH4 per year (95 per cent confidence limit)-an order of magnitude lower than the currently used estimates. This result indicates that anthropogenic fossil CH4 emissions are underestimated by about 38 to 58 teragrams CH4 per year, or about 25 to 40 per cent of recent estimates. Our record highlights the human impact on the atmosphere and climate, provides a firm target for inventories of the global CH4 budget, and will help to inform strategies for targeted emission reductions9,10.
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6
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Minimal geological methane emissions during the Younger Dryas–Preboreal abrupt warming event. Nature 2017; 548:443-446. [DOI: 10.1038/nature23316] [Citation(s) in RCA: 62] [Impact Index Per Article: 8.9] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 09/28/2016] [Accepted: 06/21/2017] [Indexed: 11/08/2022]
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7
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Affiliation(s)
- Peter Hopcroft
- School of Geographical Sciences, University of Bristol, Bristol BS8 1SS, UK
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8
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Bock M, Schmitt J, Beck J, Seth B, Chappellaz J, Fischer H. Glacial/interglacial wetland, biomass burning, and geologic methane emissions constrained by dual stable isotopic CH 4 ice core records. Proc Natl Acad Sci U S A 2017; 114:E5778-E5786. [PMID: 28673973 PMCID: PMC5530640 DOI: 10.1073/pnas.1613883114] [Citation(s) in RCA: 40] [Impact Index Per Article: 5.7] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/18/2022] Open
Abstract
Atmospheric methane (CH4) records reconstructed from polar ice cores represent an integrated view on processes predominantly taking place in the terrestrial biogeosphere. Here, we present dual stable isotopic methane records [δ13CH4 and δD(CH4)] from four Antarctic ice cores, which provide improved constraints on past changes in natural methane sources. Our isotope data show that tropical wetlands and seasonally inundated floodplains are most likely the controlling sources of atmospheric methane variations for the current and two older interglacials and their preceding glacial maxima. The changes in these sources are steered by variations in temperature, precipitation, and the water table as modulated by insolation, (local) sea level, and monsoon intensity. Based on our δD(CH4) constraint, it seems that geologic emissions of methane may play a steady but only minor role in atmospheric CH4 changes and that the glacial budget is not dominated by these sources. Superimposed on the glacial/interglacial variations is a marked difference in both isotope records, with systematically higher values during the last 25,000 y compared with older time periods. This shift cannot be explained by climatic changes. Rather, our isotopic methane budget points to a marked increase in fire activity, possibly caused by biome changes and accumulation of fuel related to the late Pleistocene megafauna extinction, which took place in the course of the last glacial.
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Affiliation(s)
- Michael Bock
- Climate and Environmental Physics, Physics Institute, University of Bern, 3012 Bern, Switzerland;
- Oeschger Centre for Climate Change Research, University of Bern, 3012 Bern, Switzerland
| | - Jochen Schmitt
- Climate and Environmental Physics, Physics Institute, University of Bern, 3012 Bern, Switzerland
- Oeschger Centre for Climate Change Research, University of Bern, 3012 Bern, Switzerland
| | - Jonas Beck
- Climate and Environmental Physics, Physics Institute, University of Bern, 3012 Bern, Switzerland
- Oeschger Centre for Climate Change Research, University of Bern, 3012 Bern, Switzerland
| | - Barbara Seth
- Climate and Environmental Physics, Physics Institute, University of Bern, 3012 Bern, Switzerland
- Oeschger Centre for Climate Change Research, University of Bern, 3012 Bern, Switzerland
| | - Jérôme Chappellaz
- CNRS, IGE (Institut des Géosciences de l'Environnement), F-38000 Grenoble, France
- University of Grenoble Alpes, IGE, F-38000 Grenoble, France
- IRD (Institut de Recherche pour le Développement), IGE, F-38000 Grenoble, France
- Grenoble INP (Institut National Polytechnique), IGE, F-38000 Grenoble, France
| | - Hubertus Fischer
- Climate and Environmental Physics, Physics Institute, University of Bern, 3012 Bern, Switzerland;
- Oeschger Centre for Climate Change Research, University of Bern, 3012 Bern, Switzerland
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9
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Pandey S, Houweling S, Krol M, Aben I, Monteil G, Nechita-Banda N, Dlugokencky EJ, Detmers R, Hasekamp O, Xu X, Riley WJ, Poulter B, Zhang Z, McDonald KC, White JWC, Bousquet P, Röckmann T. Enhanced methane emissions from tropical wetlands during the 2011 La Niña. Sci Rep 2017; 7:45759. [PMID: 28393869 PMCID: PMC5385533 DOI: 10.1038/srep45759] [Citation(s) in RCA: 36] [Impact Index Per Article: 5.1] [Reference Citation Analysis] [Abstract] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 10/18/2016] [Accepted: 03/03/2017] [Indexed: 11/25/2022] Open
Abstract
Year-to-year variations in the atmospheric methane (CH4) growth rate show significant correlation with climatic drivers. The second half of 2010 and the first half of 2011 experienced the strongest La Niña since the early 1980s, when global surface networks started monitoring atmospheric CH4 mole fractions. We use these surface measurements, retrievals of column-averaged CH4 mole fractions from GOSAT, new wetland inundation estimates, and atmospheric δ13C-CH4 measurements to estimate the impact of this strong La Niña on the global atmospheric CH4 budget. By performing atmospheric inversions, we find evidence of an increase in tropical CH4 emissions of ∼6–9 TgCH4 yr−1 during this event. Stable isotope data suggest that biogenic sources are the cause of this emission increase. We find a simultaneous expansion of wetland area, driven by the excess precipitation over the Tropical continents during the La Niña. Two process-based wetland models predict increases in wetland area consistent with observationally-constrained values, but substantially smaller per-area CH4 emissions, highlighting the need for improvements in such models. Overall, tropical wetland emissions during the strong La Niña were at least by 5% larger than the long-term mean.
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Affiliation(s)
- Sudhanshu Pandey
- Institute of Marine and Atmospheric Research Utrecht (IMAU), Utrecht, The Netherlands.,SRON Netherlands institute for Space Research, Utrecht, The Netherlands
| | - Sander Houweling
- Institute of Marine and Atmospheric Research Utrecht (IMAU), Utrecht, The Netherlands.,SRON Netherlands institute for Space Research, Utrecht, The Netherlands
| | - Maarten Krol
- Institute of Marine and Atmospheric Research Utrecht (IMAU), Utrecht, The Netherlands.,SRON Netherlands institute for Space Research, Utrecht, The Netherlands.,Department of Meteorology and Air Quality (MAQ), Wageningen University and Research Centre, WageningenThe Netherlands
| | - Ilse Aben
- SRON Netherlands institute for Space Research, Utrecht, The Netherlands
| | - Guillaume Monteil
- Department of Physical Geography and Ecosystem Science, Lund University, Lund, Sweden
| | | | | | - Rob Detmers
- SRON Netherlands institute for Space Research, Utrecht, The Netherlands
| | - Otto Hasekamp
- SRON Netherlands institute for Space Research, Utrecht, The Netherlands
| | - Xiyan Xu
- Earth Sciences Division, Lawrence Berkeley National Laboratory, Berkeley, California, USA.,CAS Key Laboratory of Regional Climate-Environment for Temperate East Asia, Institute of Atmospheric Physics, Beijing, China
| | - William J Riley
- Earth Sciences Division, Lawrence Berkeley National Laboratory, Berkeley, California, USA
| | - Benjamin Poulter
- Institute on Ecosystems and Department of Ecology, Montana State University, Bozeman, USA
| | - Zhen Zhang
- Swiss Federal Research Institute WSL, Birmensdorf, Switzerland
| | - Kyle C McDonald
- City College of New York, City University of New York, New York, NY, USA
| | | | - Philippe Bousquet
- Laboratoire des Sciences du Climatet de l'Environnement (LSCE), Gif-sur-Yvette, France
| | - Thomas Röckmann
- Institute of Marine and Atmospheric Research Utrecht (IMAU), Utrecht, The Netherlands
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10
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Massive remobilization of permafrost carbon during post-glacial warming. Nat Commun 2016; 7:13653. [PMID: 27897191 PMCID: PMC5141343 DOI: 10.1038/ncomms13653] [Citation(s) in RCA: 19] [Impact Index Per Article: 2.4] [Reference Citation Analysis] [Abstract] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 02/13/2016] [Accepted: 10/19/2016] [Indexed: 11/25/2022] Open
Abstract
Recent hypotheses, based on atmospheric records and models, suggest that permafrost carbon (PF-C) accumulated during the last glaciation may have been an important source for the atmospheric CO2 rise during post-glacial warming. However, direct physical indications for such PF-C release have so far been absent. Here we use the Laptev Sea (Arctic Ocean) as an archive to investigate PF-C destabilization during the last glacial–interglacial period. Our results show evidence for massive supply of PF-C from Siberian soils as a result of severe active layer deepening in response to the warming. Thawing of PF-C must also have brought about an enhanced organic matter respiration and, thus, these findings suggest that PF-C may indeed have been an important source of CO2 across the extensive permafrost domain. The results challenge current paradigms on the post-glacial CO2 rise and, at the same time, serve as a harbinger for possible consequences of the present-day warming of PF-C soils. Atmospheric CO2 increases during the last deglaciation have been linked to the destabilisation of permafrost carbon reservoirs. Here, using a sediment core from the Laptev Sea, Tesi et al. indicate a massive supply of permafrost carbon was released from Siberia following active layer deepening.
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11
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Timescales of methane seepage on the Norwegian margin following collapse of the Scandinavian Ice Sheet. Nat Commun 2016; 7:11509. [PMID: 27167635 PMCID: PMC4865861 DOI: 10.1038/ncomms11509] [Citation(s) in RCA: 101] [Impact Index Per Article: 12.6] [Reference Citation Analysis] [Abstract] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 10/16/2015] [Accepted: 04/05/2016] [Indexed: 11/19/2022] Open
Abstract
Gas hydrates stored on continental shelves are susceptible to dissociation triggered by environmental changes. Knowledge of the timescales of gas hydrate dissociation and subsequent methane release are critical in understanding the impact of marine gas hydrates on the ocean–atmosphere system. Here we report a methane efflux chronology from five sites, at depths of 220–400 m, in the southwest Barents and Norwegian seas where grounded ice sheets led to thickening of the gas hydrate stability zone during the last glaciation. The onset of methane release was coincident with deglaciation-induced pressure release and thinning of the hydrate stability zone. Methane efflux continued for 7–10 kyr, tracking hydrate stability changes controlled by relative sea-level rise, bottom water warming and fluid pathway evolution in response to changing stress fields. The protracted nature of seafloor methane emissions probably attenuated the impact of hydrate dissociation on the climate system. Understanding the timescales of gas hydrate dissociation and methane release are critical to gauge the potential climate impact. Here, the authors report a methane efflux chronology from five sites in Barents and Norwegian seas and show methane release coincident with the release of ice sheet-induced pressure.
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12
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Permafrost thawing as a possible source of abrupt carbon release at the onset of the Bølling/Allerød. Nat Commun 2014; 5:5520. [PMID: 25409739 PMCID: PMC4263146 DOI: 10.1038/ncomms6520] [Citation(s) in RCA: 47] [Impact Index Per Article: 4.7] [Reference Citation Analysis] [Abstract] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 04/07/2014] [Accepted: 10/09/2014] [Indexed: 11/09/2022] Open
Abstract
One of the most abrupt and yet unexplained past rises in atmospheric CO2 (>10 p.p.m.v. in two centuries) occurred in quasi-synchrony with abrupt northern hemispheric warming into the Bølling/Allerød, ~14,600 years ago. Here we use a U/Th-dated record of atmospheric Δ14C from Tahiti corals to provide an independent and precise age control for this CO2 rise. We also use model simulations to show that the release of old (nearly 14C-free) carbon can explain these changes in CO2 and Δ14C. The Δ14C record provides an independent constraint on the amount of carbon released (~125 Pg C). We suggest, in line with observations of atmospheric CH4 and terrigenous biomarkers, that thawing permafrost in high northern latitudes could have been the source of carbon, possibly with contribution from flooding of the Siberian continental shelf during meltwater pulse 1A. Our findings highlight the potential of the permafrost carbon reservoir to modulate abrupt climate changes via greenhouse-gas feedbacks. Ice core records show evidence for an abrupt, and thus far unexplained, increase in atmospheric CO2 levels ~14,600 years ago. Here, the authors combine ice core data, a precisely dated decline in atmospheric 14C and numerical simulations, and propose thawing permafrost as a possible source of this event.
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13
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Anthony KMW, Zimov SA, Grosse G, Jones MC, Anthony PM, Chapin FS, Finlay JC, Mack MC, Davydov S, Frenzel P, Frolking S. A shift of thermokarst lakes from carbon sources to sinks during the Holocene epoch. Nature 2014; 511:452-6. [PMID: 25043014 DOI: 10.1038/nature13560] [Citation(s) in RCA: 55] [Impact Index Per Article: 5.5] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 07/13/2013] [Accepted: 06/02/2014] [Indexed: 11/09/2022]
Abstract
Thermokarst lakes formed across vast regions of Siberia and Alaska during the last deglaciation and are thought to be a net source of atmospheric methane and carbon dioxide during the Holocene epoch. However, the same thermokarst lakes can also sequester carbon, and it remains uncertain whether carbon uptake by thermokarst lakes can offset their greenhouse gas emissions. Here we use field observations of Siberian permafrost exposures, radiocarbon dating and spatial analyses to quantify Holocene carbon stocks and fluxes in lake sediments overlying thawed Pleistocene-aged permafrost. We find that carbon accumulation in deep thermokarst-lake sediments since the last deglaciation is about 1.6 times larger than the mass of Pleistocene-aged permafrost carbon released as greenhouse gases when the lakes first formed. Although methane and carbon dioxide emissions following thaw lead to immediate radiative warming, carbon uptake in peat-rich sediments occurs over millennial timescales. We assess thermokarst-lake carbon feedbacks to climate with an atmospheric perturbation model and find that thermokarst basins switched from a net radiative warming to a net cooling climate effect about 5,000 years ago. High rates of Holocene carbon accumulation in 20 lake sediments (47 ± 10 grams of carbon per square metre per year; mean ± standard error) were driven by thermokarst erosion and deposition of terrestrial organic matter, by nutrient release from thawing permafrost that stimulated lake productivity and by slow decomposition in cold, anoxic lake bottoms. When lakes eventually drained, permafrost formation rapidly sequestered sediment carbon. Our estimate of about 160 petagrams of Holocene organic carbon in deep lake basins of Siberia and Alaska increases the circumpolar peat carbon pool estimate for permafrost regions by over 50 per cent (ref. 6). The carbon in perennially frozen drained lake sediments may become vulnerable to mineralization as permafrost disappears, potentially negating the climate stabilization provided by thermokarst lakes during the late Holocene.
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Affiliation(s)
- K M Walter Anthony
- Water and Environmental Research Center, University of Alaska, Fairbanks, Alaska 99775-5860, USA
| | - S A Zimov
- Northeast Scientific Station, Pacific Institute for Geography, Far-East Branch, Russian Academy of Sciences, Cherskii 678830, Russia
| | - G Grosse
- 1] Geophysical Institute, University of Alaska, Fairbanks, Alaska 99775-7320, USA [2] Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Potsdam 14473, Germany
| | - M C Jones
- 1] Water and Environmental Research Center, University of Alaska, Fairbanks, Alaska 99775-5860, USA [2] US Geological Survey, Reston, Virginia 20192, USA
| | - P M Anthony
- Water and Environmental Research Center, University of Alaska, Fairbanks, Alaska 99775-5860, USA
| | - F S Chapin
- Institute of Arctic Biology, University of Alaska, Fairbanks, Alaska 99775-7000, USA
| | - J C Finlay
- Department of Ecology, Evolution and Behavior, University of Minnesota, Saint Paul, Minnesota 55108, USA
| | - M C Mack
- Department of Biology, University of Florida, Gainesville, Florida 32611, USA
| | - S Davydov
- Northeast Scientific Station, Pacific Institute for Geography, Far-East Branch, Russian Academy of Sciences, Cherskii 678830, Russia
| | - P Frenzel
- Max Planck Institute for Terrestrial Microbiology, Marburg 35043, Germany
| | - S Frolking
- Institute for the Study of Earth, Oceans, and Space, University of New Hampshire, Durham, New Hampshire 03824-3525, USA
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14
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Radiometric 81Kr dating identifies 120,000-year-old ice at Taylor Glacier, Antarctica. Proc Natl Acad Sci U S A 2014; 111:6876-81. [PMID: 24753606 DOI: 10.1073/pnas.1320329111] [Citation(s) in RCA: 51] [Impact Index Per Article: 5.1] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/18/2022] Open
Abstract
We present successful (81)Kr-Kr radiometric dating of ancient polar ice. Krypton was extracted from the air bubbles in four ∼350-kg polar ice samples from Taylor Glacier in the McMurdo Dry Valleys, Antarctica, and dated using Atom Trap Trace Analysis (ATTA). The (81)Kr radiometric ages agree with independent age estimates obtained from stratigraphic dating techniques with a mean absolute age offset of 6 ± 2.5 ka. Our experimental methods and sampling strategy are validated by (i) (85)Kr and (39)Ar analyses that show the samples to be free of modern air contamination and (ii) air content measurements that show the ice did not experience gas loss. We estimate the error in the (81)Kr ages due to past geomagnetic variability to be below 3 ka. We show that ice from the previous interglacial period (Marine Isotope Stage 5e, 130-115 ka before present) can be found in abundance near the surface of Taylor Glacier. Our study paves the way for reliable radiometric dating of ancient ice in blue ice areas and margin sites where large samples are available, greatly enhancing their scientific value as archives of old ice and meteorites. At present, ATTA (81)Kr analysis requires a 40-80-kg ice sample; as sample requirements continue to decrease, (81)Kr dating of ice cores is a future possibility.
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15
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Zimov S, Zimov N. Role of megafauna and frozen soil in the atmospheric CH4 dynamics. PLoS One 2014; 9:e93331. [PMID: 24695117 PMCID: PMC3973675 DOI: 10.1371/journal.pone.0093331] [Citation(s) in RCA: 10] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 11/10/2012] [Accepted: 03/05/2014] [Indexed: 11/19/2022] Open
Abstract
Modern wetlands are the world’s strongest methane source. But what was the role of this source in the past? An analysis of global 14C data for basal peat combined with modelling of wetland succession allowed us to reconstruct the dynamics of global wetland methane emission through time. These data show that the rise of atmospheric methane concentrations during the Pleistocene-Holocene transition was not connected with wetland expansion, but rather started substantially later, only 9 thousand years ago. Additionally, wetland expansion took place against the background of a decline in atmospheric methane concentration. The isotopic composition of methane varies according to source. Owing to ice sheet drilling programs past dynamics of atmospheric methane isotopic composition is now known. For example over the course of Pleistocene-Holocene transition atmospheric methane became depleted in the deuterium isotope, which indicated that the rise in methane concentrations was not connected with activation of the deuterium-rich gas clathrates. Modelling of the budget of the atmospheric methane and its isotopic composition allowed us to reconstruct the dynamics of all main methane sources. For the late Pleistocene, the largest methane source was megaherbivores, whose total biomass is estimated to have exceeded that of present-day humans and domestic animals. This corresponds with our independent estimates of herbivore density on the pastures of the late Pleistocene based on herbivore skeleton density in the permafrost. During deglaciation, the largest methane emissions originated from degrading frozen soils of the mammoth steppe biome. Methane from this source is unique, as it is depleted of all isotopes. We estimated that over the entire course of deglaciation (15,000 to 6,000 year before present), soils of the mammoth steppe released 300–550 Pg (1015 g) of methane. From current study we conclude that the Late Quaternary Extinction significantly affected the global methane cycle.
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Affiliation(s)
- Sergey Zimov
- Northeast Science Station, Pacific Institute for Geography, Russian Academy of Sciences, Cherskii, Russia
- * E-mail:
| | - Nikita Zimov
- Northeast Science Station, Pacific Institute for Geography, Russian Academy of Sciences, Cherskii, Russia
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16
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Nitrogen trifluoride global emissions estimated from updated atmospheric measurements. Proc Natl Acad Sci U S A 2013; 110:2029-34. [PMID: 23341630 DOI: 10.1073/pnas.1212346110] [Citation(s) in RCA: 34] [Impact Index Per Article: 3.1] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/18/2022] Open
Abstract
Nitrogen trifluoride (NF(3)) has potential to make a growing contribution to the Earth's radiative budget; however, our understanding of its atmospheric burden and emission rates has been limited. Based on a revision of our previous calibration and using an expanded set of atmospheric measurements together with an atmospheric model and inverse method, we estimate that the global emissions of NF(3) in 2011 were 1.18 ± 0.21 Gg⋅y(-1), or ∼20 Tg CO(2)-eq⋅y(-1) (carbon dioxide equivalent emissions based on a 100-y global warming potential of 16,600 for NF(3)). The 2011 global mean tropospheric dry air mole fraction was 0.86 ± 0.04 parts per trillion, resulting from an average emissions growth rate of 0.09 Gg⋅y(-2) over the prior decade. In terms of CO(2) equivalents, current NF(3) emissions represent between 17% and 36% of the emissions of other long-lived fluorinated compounds from electronics manufacture. We also estimate that the emissions benefit of using NF(3) over hexafluoroethane (C(2)F(6)) in electronics manufacture is significant-emissions of between 53 and 220 Tg CO(2)-eq⋅y(-1) were avoided during 2011. Despite these savings, total NF(3) emissions, currently ∼10% of production, are still significantly larger than expected assuming global implementation of ideal industrial practices. As such, there is a continuing need for improvements in NF(3) emissions reduction strategies to keep pace with its increasing use and to slow its rising contribution to anthropogenic climate forcing.
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17
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Brosius LS, Walter Anthony KM, Grosse G, Chanton JP, Farquharson LM, Overduin PP, Meyer H. Using the deuterium isotope composition of permafrost meltwater to constrain thermokarst lake contributions to atmospheric CH4during the last deglaciation. ACTA ACUST UNITED AC 2012. [DOI: 10.1029/2011jg001810] [Citation(s) in RCA: 62] [Impact Index Per Article: 5.2] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/10/2022]
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18
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Abstract
Earth's climate is warming as a result of anthropogenic emissions of greenhouse gases, particularly carbon dioxide (CO(2)) from fossil fuel combustion. Anthropogenic emissions of non-CO(2) greenhouse gases, such as methane, nitrous oxide and ozone-depleting substances (largely from sources other than fossil fuels), also contribute significantly to warming. Some non-CO(2) greenhouse gases have much shorter lifetimes than CO(2), so reducing their emissions offers an additional opportunity to lessen future climate change. Although it is clear that sustainably reducing the warming influence of greenhouse gases will be possible only with substantial cuts in emissions of CO(2), reducing non-CO(2) greenhouse gas emissions would be a relatively quick way of contributing to this goal.
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Affiliation(s)
- S A Montzka
- National Oceanic and Atmospheric Administration, Boulder, Colorado 80305, USA.
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19
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Dlugokencky EJ, Nisbet EG, Fisher R, Lowry D. Global atmospheric methane: budget, changes and dangers. PHILOSOPHICAL TRANSACTIONS. SERIES A, MATHEMATICAL, PHYSICAL, AND ENGINEERING SCIENCES 2011; 369:2058-2072. [PMID: 21502176 DOI: 10.1098/rsta.2010.0341] [Citation(s) in RCA: 153] [Impact Index Per Article: 11.8] [Reference Citation Analysis] [Abstract] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/30/2023]
Abstract
A factor of 2.5 increase in the global abundance of atmospheric methane (CH(4)) since 1750 contributes 0.5 Wm(-2) to total direct radiative forcing by long-lived greenhouse gases (2.77 Wm(-2) in 2009), while its role in atmospheric chemistry adds another approximately 0.2 Wm(-2) of indirect forcing. Since CH(4) has a relatively short lifetime and it is very close to a steady state, reductions in its emissions would quickly benefit climate. Sensible emission mitigation strategies require quantitative understanding of CH(4)'s budget of emissions and sinks. Atmospheric observations of CH(4) abundance and its rate of increase, combined with an estimate of the CH(4) lifetime, constrain total global CH(4) emissions to between 500 and 600 Tg CH(4) yr(-1). While total global emissions are constrained reasonably well, estimates of emissions by source sector vary by up to a factor of 2. Current observation networks are suitable to constrain emissions at large scales (e.g. global) but not at the regional to national scales necessary to verify emission reductions under emissions trading schemes. Improved constraints on the global CH(4) budget and its break down of emissions by source sector and country will come from an enhanced observation network for CH(4) abundance and its isotopic composition (δ(13)C, δD(D=(2)H) and δ(14)C). Isotopic measurements are a valuable tool in distinguishing among various sources that contribute emissions to an air parcel, once fractionation by loss processes is accounted for. Isotopic measurements are especially useful at regional scales where signals are larger. Reducing emissions from many anthropogenic source sectors is cost-effective, but these gains may be cancelled, in part, by increasing emissions related to economic development in many parts of the world. An observation network that can quantitatively assess these changing emissions, both positive and negative, is required, especially in the context of emissions trading schemes.
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Affiliation(s)
- Edward J Dlugokencky
- US National Oceanic and Atmospheric Administration, Earth System Research Laboratory, 325 Broadway, Boulder, CO 80305, USA.
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20
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Wolff EW. Greenhouse gases in the Earth system: a palaeoclimate perspective. PHILOSOPHICAL TRANSACTIONS. SERIES A, MATHEMATICAL, PHYSICAL, AND ENGINEERING SCIENCES 2011; 369:2133-2147. [PMID: 21502180 DOI: 10.1098/rsta.2010.0225] [Citation(s) in RCA: 7] [Impact Index Per Article: 0.5] [Reference Citation Analysis] [Abstract] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/30/2023]
Abstract
While the trends in greenhouse gas concentrations in recent decades are clear, their significance is only revealed when viewed in the context of a longer time period. Fortunately, the air bubbles in polar ice cores provide an unusually direct method of determining the concentrations of stable gases over a period of (so far) 800,000 years. Measurements on different cores with varying characteristics, as well as an overlap of ice-core and atmospheric measurements covering the same time period, show that the ice-core record provides a faithful record of changing atmospheric composition. The mixing ratio of CO(2) is now 30 per cent higher than any value observed in the ice-core record, while methane is more than double any observed value; the rate of change also appears extraordinary compared with natural changes. Before the period when anthropogenic changes have dominated, there are very interesting natural changes in concentration, particularly across glacial/interglacial cycles, and these can be used to understand feedbacks in the Earth system. The phasing of changes in temperature and CO(2) across glacial/interglacial transitions is consistent with the idea that CO(2) acts as an important amplifier of climate changes in the natural system. Even larger changes are inferred to have occurred in periods earlier than the ice cores cover, and these events might be used to constrain assessments of the way the Earth could respond to higher than present concentrations of CO(2), and to a large release of carbon: however, more certainty about CO(2) concentrations beyond the time period covered by ice cores is needed before such constraints can be fully realized.
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Affiliation(s)
- Eric W Wolff
- British Antarctic Survey, High Cross, Madingley Road, Cambridge CB3 0ET, UK.
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21
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22
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Affiliation(s)
- Natalia Shakhova
- International Arctic Research Center, University of Alaska, Fairbanks, AK 99775, USA
- Russian Academy of Sciences, Far Eastern Branch, Pacific Oceanological Institute, Vladivostok, Russia
| | - Igor Semiletov
- International Arctic Research Center, University of Alaska, Fairbanks, AK 99775, USA
- Russian Academy of Sciences, Far Eastern Branch, Pacific Oceanological Institute, Vladivostok, Russia
| | - Örjan Gustafsson
- Department of Applied Environmental Science and Bert Bolin Centre for Climate Research, Stockholm University, Stockholm, Sweden
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23
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Petrenko VV, Etheridge DM, Weiss RF, Brook EJ, Schaefer H, Severinghaus JP, Smith AM, Lowe D, Hua Q, Riedel K. Methane from the East Siberian Arctic Shelf. Science 2010; 329:1146-7; author reply 1147-8. [DOI: 10.1126/science.329.5996.1146-b] [Citation(s) in RCA: 5] [Impact Index Per Article: 0.4] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/02/2022]
Affiliation(s)
- Vasilii V. Petrenko
- Institute of Arctic and Alpine Research, University of Colorado, Boulder, CO 80309, USA
| | - David M. Etheridge
- Centre for Australian Weather and Climate Research, CSIRO Marine and Atmospheric Research, Aspendale, VIC 3195, Australia
| | - Ray F. Weiss
- Scripps Institution of Oceanography, University of California, San Diego, La Jolla, CA 92093, USA
| | - Edward J. Brook
- Department of Geosciences, Oregon State University, Corvallis, OR 97331, USA
| | - Hinrich Schaefer
- National Institute of Water and Atmospheric Research, Kilbirnie, Wellington, New Zealand
| | - Jeffrey P. Severinghaus
- Scripps Institution of Oceanography, University of California, San Diego, La Jolla, CA 92093, USA
| | - Andrew M. Smith
- Australian Nuclear Science and Technology Organisation, PMB 1, Menai, NSW 2234, Australia
| | - Dave Lowe
- Antarctic Research Centre, Victoria University of Wellington, Wellington, New Zealand
- Lowe NZ, Climate Change Education and Renewable Energy, Plimmerton–Porirua 5026, New Zealand
| | - Quan Hua
- Australian Nuclear Science and Technology Organisation, PMB 1, Menai, NSW 2234, Australia
| | - Katja Riedel
- National Institute of Water and Atmospheric Research, Kilbirnie, Wellington, New Zealand
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Abstract
Northern peatlands represent one of the largest biospheric carbon (C) reservoirs; however, the role of peatlands in the global carbon cycle remains intensely debated, owing in part to the paucity of detailed regional datasets and the complexity of the role of climate, ecosystem processes, and environmental factors in controlling peatland C dynamics. Here we used detailed C accumulation data from four peatlands and a compilation of peatland initiation ages across Alaska to examine Holocene peatland dynamics and climate sensitivity. We find that 75% of dated peatlands in Alaska initiated before 8,600 years ago and that early Holocene C accumulation rates were four times higher than the rest of the Holocene. Similar rapid peatland expansion occurred in West Siberia during the Holocene thermal maximum (HTM). Our results suggest that high summer temperature and strong seasonality during the HTM in Alaska might have played a major role in causing the highest rates of C accumulation and peatland expansion. The rapid peatland expansion and C accumulation in these vast regions contributed significantly to the peak of atmospheric methane concentrations in the early Holocene. Furthermore, we find that Alaskan peatlands began expanding much earlier than peatlands in other regions, indicating an important contribution of these peatlands to the pre-Holocene increase in atmospheric methane concentrations.
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Affiliation(s)
- Miriam C Jones
- Department of Earth and Environmental Sciences, Lehigh University, Bethlehem, PA 18015, USA.
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25
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Shakhova N, Semiletov I, Salyuk A, Yusupov V, Kosmach D, Gustafsson O. Extensive methane venting to the atmosphere from sediments of the East Siberian Arctic Shelf. Science 2010; 327:1246-50. [PMID: 20203047 DOI: 10.1126/science.1182221] [Citation(s) in RCA: 418] [Impact Index Per Article: 29.9] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/02/2022]
Abstract
Remobilization to the atmosphere of only a small fraction of the methane held in East Siberian Arctic Shelf (ESAS) sediments could trigger abrupt climate warming, yet it is believed that sub-sea permafrost acts as a lid to keep this shallow methane reservoir in place. Here, we show that more than 5000 at-sea observations of dissolved methane demonstrates that greater than 80% of ESAS bottom waters and greater than 50% of surface waters are supersaturated with methane regarding to the atmosphere. The current atmospheric venting flux, which is composed of a diffusive component and a gradual ebullition component, is on par with previous estimates of methane venting from the entire World Ocean. Leakage of methane through shallow ESAS waters needs to be considered in interactions between the biogeosphere and a warming Arctic climate.
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Affiliation(s)
- Natalia Shakhova
- International Arctic Research Centre, University of Alaska, Fairbanks, AK 99709, USA.
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26
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Bock M, Schmitt J, Behrens M, Möller L, Schneider R, Sapart C, Fischer H. A gas chromatography/pyrolysis/isotope ratio mass spectrometry system for high-precision deltaD measurements of atmospheric methane extracted from ice cores. RAPID COMMUNICATIONS IN MASS SPECTROMETRY : RCM 2010; 24:621-633. [PMID: 20155754 DOI: 10.1002/rcm.4429] [Citation(s) in RCA: 5] [Impact Index Per Article: 0.4] [Reference Citation Analysis] [Abstract] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/28/2023]
Abstract
Air enclosures in polar ice cores represent the only direct paleoatmospheric archive. Analysis of the entrapped air provides clues to the climate system of the past in decadal to centennial resolution. A wealth of information has been gained from measurements of concentrations of greenhouse gases; however, little is known about their isotopic composition. In particular, stable isotopologues (deltaD and delta(13)C) of methane (CH(4)) record valuable information on its global cycle as the different sources exhibit distinct carbon and hydrogen isotopic composition. However, CH(4) isotope analysis is limited by the large sample size required and the demanding analysis as high precision is required. Here we present a highly automated, high-precision online gas chromatography/pyrolysis/isotope ratio monitoring mass spectrometry (GC/P/irmMS) technique for the analysis of deltaD(CH(4)). It includes gas extraction from ice, preconcentration, gas chromatographic separation and pyrolysis of CH(4) from roughly 500 g of ice with CH(4) concentrations as low as 350 ppbv. Ice samples with approximately 40 mL air and only approximately 1 nmol CH(4) can be measured with a precision of 3.4 per thousand. The precision for 65 mL air samples with recent atmospheric concentration is 1.5 per thousand. The CH(4) concentration can be obtained along with isotope data which is crucial for reporting ice core data on matched time scales and enables us to detect flaws in the measurement procedure. Custom-made script-based processing of MS raw and peak data enhance the system's performance with respect to stability, peak size dependency, hence precision and accuracy and last but not least time requirement.
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Affiliation(s)
- Michael Bock
- Climate and Environmental Physics and Oeschger Centre for Climate Change Research, University of Bern, Switzerland.
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27
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Affiliation(s)
- James J. McCarthy
- James J. McCarthy is the Alexander Agassiz Professor of Biological Oceanography at Harvard University. He has served as president of the AAAS from February 2009 to February 2010. This essay is adapted from the Presidential Address he delivered at the AAAS Annual Meeting in Chicago on 12 February 2009
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28
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Affiliation(s)
- E. G. Nisbet
- Department of Earth Sciences, Royal Holloway, University of London, Egham TW20 0EX, UK
| | - J. Chappellaz
- Laboratoire de Glaciologie et Géophysique de l'Environnement, CNRS, University of Grenoble, BP 96, 38402 St. Martin d'Hères, France
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