Carbon sequestration is not inhibited by livestock grazing in Danish salt marshes

2022 ◽  
Author(s):  
Anna Elizabeth Løvgren Graversen ◽  
Gary T. Banta ◽  
Pere Masque ◽  
Dorte Krause‐Jensen
2017 ◽  
Vol 11 (2) ◽  
pp. 152-161 ◽  
Author(s):  
Corinna Rickert ◽  
Andreas Fichtner ◽  
Roel van Klink

2013 ◽  
Vol 135 ◽  
pp. 296-305 ◽  
Author(s):  
Stefanie Nolte ◽  
Frauke Müller ◽  
Mark Schuerch ◽  
Antonia Wanner ◽  
Peter Esselink ◽  
...  

2020 ◽  
Author(s):  
Oksana Rybchak ◽  
Justin du Toit ◽  
Jean-Pierre Delorme ◽  
Jens-Kristian Jüdt ◽  
Kanisios Mukwashi ◽  
...  

Abstract. Climatic and land management factors, such as water availability and grazing intensity, play an important role in seasonal and annual variability of the ecosystem–atmosphere exchange of CO2 in semi-arid ecosystems. However, the semi-arid South African ecosystems have been poorly studied. Four years of measurements (November 2015–October 2019) were collected and analysed from two eddy covariance towers near Middelburg in the Karoo, Eastern Cape, South Africa. We studied the impact of grazing intensity on the CO2 exchange by comparing seasonal and interannual CO2 fluxes for two sites with almost identical climatic conditions but different intensity of current and historical livestock grazing. The first site represents lenient grazing (LG) and the vegetation comprises a diverse balance of dwarf shrubs and grasses, while the second site has been degraded through heavy grazing (HG) in the past but then rested for the past 10 years and mainly consists of unpalatable grasses and ephemeral species. Over the observation period, we found that the LG site was a considerable carbon source (82.11 g C m−2), while the HG site was a slight carbon sink (−36.43 g C m−2). The annual carbon budgets ranged from −90 ± 51 g C m−2 yr−1 to 84 ± 43 g C m−2 yr−1 for the LG site and from −92 ± 66 g C m−2 yr−1 to 59 ± 46 g C m−2 yr−1 for the heavily grazed site over the four years of eddy covariance measurements. The significant variation in carbon sequestration rates between the last two years of measurement was explained by water availability (25 % of the precipitation deficit in 2019 compared to the long-term mean precipitation). This indicates that studied ecosystems can quickly switch from a considerable carbon sink to a considerable carbon source ecosystem. Our study shows that the CO2 dynamics in the Karoo are largely driven by water availability and the current and historical effects of livestock grazing intensity on aboveground biomass (AGB). The higher carbon uptake at the HG site indicates that resting period after overgrazing, together with the transition to unpalatable drought-tolerant grass species, creates conditions that are favourable for carbon sequestration in the Karoo ecosystems, but unproductive as Dorper sheep pasture. Furthermore, we observed a slight decrease in carbon uptake peaks at the HG site in response to resuming continuous grazing (July 2017).


2017 ◽  
Vol 54 (5) ◽  
pp. 1395-1405 ◽  
Author(s):  
Kate E. Davidson ◽  
Mike S. Fowler ◽  
Martin W. Skov ◽  
Stefan H. Doerr ◽  
Nicola Beaumont ◽  
...  

2005 ◽  
Vol 13 (1) ◽  
pp. 1-15 ◽  
Author(s):  
Daan Bos ◽  
Maarten J.J.E. Loonen ◽  
Martin Stock ◽  
Frank Hofeditz ◽  
Alexandra J. van der Graaf ◽  
...  

2016 ◽  
Vol 3 ◽  
Author(s):  
Paulina Martinetto ◽  
Diana I. Montemayor ◽  
Juan Alberti ◽  
César S. B. Costa ◽  
Oscar Iribarne

Author(s):  
Christine Bertram ◽  
Martin Quaas ◽  
Thorsten B. H. Reusch ◽  
Athanasios T. Vafeidis ◽  
Claudia Wolff ◽  
...  

AbstractCarbon sequestration and storage in mangroves, salt marshes and seagrass meadows is an essential coastal ‘blue carbon’ ecosystem service for climate change mitigation. Here we offer a comprehensive, global and spatially explicit economic assessment of carbon sequestration and storage in three coastal ecosystem types at the global and national levels. We propose a new approach based on the country-specific social cost of carbon that allows us to calculate each country’s contribution to, and redistribution of, global blue carbon wealth. Globally, coastal ecosystems contribute a mean ± s.e.m. of US$190.67 ± 30 bn yr−1 to blue carbon wealth. The three countries generating the largest positive net blue wealth contribution for other countries are Australia, Indonesia and Cuba, with Australia alone generating a positive net benefit of US$22.8 ± 3.8 bn yr−1 for the rest of the world through coastal ecosystem carbon sequestration and storage in its territory.


Ecosphere ◽  
2019 ◽  
Vol 10 (1) ◽  
Author(s):  
Peter Mueller ◽  
Nils Ladiges ◽  
Alexander Jack ◽  
Gerhard Schmiedl ◽  
Lars Kutzbach ◽  
...  

2015 ◽  
Vol 56 (4) ◽  
pp. 998-1008 ◽  
Author(s):  
Katherine Drake ◽  
Holly Halifax ◽  
Susan C. Adamowicz ◽  
Christopher Craft

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