Icelandic grasslands as long-term C sinks under elevated N inputs

About 10 % of the anthropogenic CO 2 emissions have been absorbed by northern terrestrial ecosystems during the past decades. It has been hypothesized that part of this increasing carbon (C) sink is caused by the alleviation of nitrogen (N) limitation by increasing anthropogenic N inputs. However, l...

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Main Authors: Leblans, Niki I. W., Sigurdsson, Bjarni D., Aerts, Rien, Vicca, Sara, Magnússon, Borgthór, Janssens, Ivan A.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/bg-2016-111
https://www.biogeosciences-discuss.net/bg-2016-111/
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spelling ftcopernicus:oai:publications.copernicus.org:bgd50526 2023-05-15T18:42:46+02:00 Icelandic grasslands as long-term C sinks under elevated N inputs Leblans, Niki I. W. Sigurdsson, Bjarni D. Aerts, Rien Vicca, Sara Magnússon, Borgthór Janssens, Ivan A. 2018-09-26 application/pdf https://doi.org/10.5194/bg-2016-111 https://www.biogeosciences-discuss.net/bg-2016-111/ eng eng doi:10.5194/bg-2016-111 https://www.biogeosciences-discuss.net/bg-2016-111/ eISSN: 1726-4189 Text 2018 ftcopernicus https://doi.org/10.5194/bg-2016-111 2019-12-24T09:52:39Z About 10 % of the anthropogenic CO 2 emissions have been absorbed by northern terrestrial ecosystems during the past decades. It has been hypothesized that part of this increasing carbon (C) sink is caused by the alleviation of nitrogen (N) limitation by increasing anthropogenic N inputs. However, little is known about this N-dependent C sink. Here, we studied the effect of chronic seabird-derived N inputs (47–67 kg N ha −1 yr −1 ) on the net soil organic C (SOC) storage rate of unmanaged Icelandic grasslands on the volcanic Vestmannaeyjar archipelago by using a stock change approach in combination with soil dating. We studied both early developmental soils (50 years) and mature soils (1,600 years), and for the latter we separated between decadal (topsoil) and millennial (total soil profile) responses, where the SOC stocks in the topsoil accorded to 40–50 years of net SOC storage and those in the total soil to 1,600 years of net SOC storage. We found that enhanced N availability – either from accumulation over time, or seabird derived – increased the net SOC storage rate. Under low N inputs, the early developmental soils were weak decadal C sinks (0.018 ton SOC ha −1 yr −1 ), but this increased quickly under elevated N inputs to 0.29 ton SOC ha −1 yr −1 , thereby equaling the decadal SOC storage rate of the unfertilized mature site. Furthermore, at the mature site, chronic N inputs not only stimulated the decadal SOC storage rate, but also the millennial SOC storage was consistently higher at the high N input site. Hence, our study suggests that Icelandic grasslands, if not disturbed, can remain C sinks for many centuries under current climatic conditions and that chronically elevated N inputs can induce a permanent strengthening of this sink. Text Vestmannaeyjar Copernicus Publications: E-Journals Vestmannaeyjar ENVELOPE(-20.391,-20.391,63.362,63.362)
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description About 10 % of the anthropogenic CO 2 emissions have been absorbed by northern terrestrial ecosystems during the past decades. It has been hypothesized that part of this increasing carbon (C) sink is caused by the alleviation of nitrogen (N) limitation by increasing anthropogenic N inputs. However, little is known about this N-dependent C sink. Here, we studied the effect of chronic seabird-derived N inputs (47–67 kg N ha −1 yr −1 ) on the net soil organic C (SOC) storage rate of unmanaged Icelandic grasslands on the volcanic Vestmannaeyjar archipelago by using a stock change approach in combination with soil dating. We studied both early developmental soils (50 years) and mature soils (1,600 years), and for the latter we separated between decadal (topsoil) and millennial (total soil profile) responses, where the SOC stocks in the topsoil accorded to 40–50 years of net SOC storage and those in the total soil to 1,600 years of net SOC storage. We found that enhanced N availability – either from accumulation over time, or seabird derived – increased the net SOC storage rate. Under low N inputs, the early developmental soils were weak decadal C sinks (0.018 ton SOC ha −1 yr −1 ), but this increased quickly under elevated N inputs to 0.29 ton SOC ha −1 yr −1 , thereby equaling the decadal SOC storage rate of the unfertilized mature site. Furthermore, at the mature site, chronic N inputs not only stimulated the decadal SOC storage rate, but also the millennial SOC storage was consistently higher at the high N input site. Hence, our study suggests that Icelandic grasslands, if not disturbed, can remain C sinks for many centuries under current climatic conditions and that chronically elevated N inputs can induce a permanent strengthening of this sink.
format Text
author Leblans, Niki I. W.
Sigurdsson, Bjarni D.
Aerts, Rien
Vicca, Sara
Magnússon, Borgthór
Janssens, Ivan A.
spellingShingle Leblans, Niki I. W.
Sigurdsson, Bjarni D.
Aerts, Rien
Vicca, Sara
Magnússon, Borgthór
Janssens, Ivan A.
Icelandic grasslands as long-term C sinks under elevated N inputs
author_facet Leblans, Niki I. W.
Sigurdsson, Bjarni D.
Aerts, Rien
Vicca, Sara
Magnússon, Borgthór
Janssens, Ivan A.
author_sort Leblans, Niki I. W.
title Icelandic grasslands as long-term C sinks under elevated N inputs
title_short Icelandic grasslands as long-term C sinks under elevated N inputs
title_full Icelandic grasslands as long-term C sinks under elevated N inputs
title_fullStr Icelandic grasslands as long-term C sinks under elevated N inputs
title_full_unstemmed Icelandic grasslands as long-term C sinks under elevated N inputs
title_sort icelandic grasslands as long-term c sinks under elevated n inputs
publishDate 2018
url https://doi.org/10.5194/bg-2016-111
https://www.biogeosciences-discuss.net/bg-2016-111/
long_lat ENVELOPE(-20.391,-20.391,63.362,63.362)
geographic Vestmannaeyjar
geographic_facet Vestmannaeyjar
genre Vestmannaeyjar
genre_facet Vestmannaeyjar
op_source eISSN: 1726-4189
op_relation doi:10.5194/bg-2016-111
https://www.biogeosciences-discuss.net/bg-2016-111/
op_doi https://doi.org/10.5194/bg-2016-111
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