Changes in carbon storage since the pre-industrial era

A national scale analysis

Bibliographic Data

ID5253200
AuthorsVictoria Janes-Bassett, Victoria Janes‐bassett (0000-0002-4882-6202, Lancaster University, corresponding author), Raewyn Bassett (0000-0002-5334-7951, Lancaster University), E C Rowe (0000-0003-4784-7236, UK Centre for Ecology & Hydrology), E Tipping (0000-0001-6618-6512, UK Centre for Ecology & Hydrology), Dmitry Yumashev (0000-0003-1355-2827, Lancaster University), Jessica Davies (0000-0001-9832-7412, Lancaster University)
Year2021
Volume34
Pages100289
Publication date2021-06-01
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueAnthropocene (JOURNAL)
Journal identifiersISSN: 2213-3054
PublisherElsevier BV (PUBLISHER)
DOI10.1016/j.ancene.2021.100289
OpenAlexW3147064372
LanguageEN
Citations received3
References cited43

Carbon stores in the terrestrial biosphere globally represent over 50% of present-day organic carbon reservoirs and have significantly altered over the last three centuries owing to anthropogenic disturbances. Conversion of natural land to agricultural uses often results in a loss of soil carbon, whilst atmospheric deposition of pollutants such as nitrogen has increased carbon storage in both soil and biomass. Terrestrial carbon storage underpins a range of ecosystem services, including climate regulation, food production, and water services. This storage is crucial for sustainable land management. Quantification of terrestrial carbon cycling at regional and national scales, and understanding how human-induced drivers have impacted present-day carbon stores is therefore required to inform sustainable land use policy. This study applies the N14CP model, an integrated soil-plant biogeochemistry carbon-nitrogen-phosphorus model, across the United Kingdom to simulate changes in terrestrial carbon storage from 1700 to 2020. The analysis shows that change in anthropogenic terrestrial carbon storage is a complex picture comprising of gains in natural areas due to nitrogen deposition and afforestation, and losses in arable areas. We observed an overall net increase in total terrestrial carbon storage of 6.9%. We note, however, that continued increases in carbon storage cannot be assumed due to (i) reduced influence of future nitrogen deposition as these systems become limited by other nutrients, (ii) the need to continue enhanced nitrogen inputs to maintain carbon sequestered, and (iii) carbon declines in arable areas continuing alongside diminishing gains in other land use types. This research provides a full picture of anthropogenic impacts on terrestrial organic carbon storage, accounting for changing nutrient cycles at a national scale

Agriculture · Arable land · Bio-energy with carbon capture and storage · Biogeochemistry · Biology · Biomass (ecology · Carbon cycle · Carbon dioxide · Carbon fibers · Carbon sequestration · Deposition (geology · Ecosystem · Environmental protection · Soil carbon · Soil water · Terrestrial ecosystem · Environmental Science · Peatlands and Wetlands Ecology · Soil and Water Nutrient Dynamics · Soil Carbon and Nitrogen Dynamics · Ecology · Geology · Soil Science

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