Reviews and syntheses: measuring ecosystem nitrogen status – a comparison of proxies

There are many proxies used to measure nitrogen (N) availability in watersheds, but the degree to which they do (or do not) correlate within a watershed has not been systematically addressed. We surveyed the literature for intact forest or grassland watersheds globally, in which several metrics of n...

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Main Authors: M. Almaraz, S. Porder
Format: Article
Language:English
Published: Copernicus Publications 2016-09-01
Series:Biogeosciences
Online Access:http://www.biogeosciences.net/13/5395/2016/bg-13-5395-2016.pdf
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spelling doaj-12316172f987428fabce24f1b7fa52e42020-11-24T23:42:34ZengCopernicus PublicationsBiogeosciences1726-41701726-41892016-09-0113185395540310.5194/bg-13-5395-2016Reviews and syntheses: measuring ecosystem nitrogen status – a comparison of proxiesM. Almaraz0S. Porder1Department of Ecology and Evolutionary Biology, Brown University, Providence 02912, Rhode Island, USADepartment of Ecology and Evolutionary Biology, Brown University, Providence 02912, Rhode Island, USAThere are many proxies used to measure nitrogen (N) availability in watersheds, but the degree to which they do (or do not) correlate within a watershed has not been systematically addressed. We surveyed the literature for intact forest or grassland watersheds globally, in which several metrics of nitrogen availability have been measured. Our metrics included the following: foliar <i>δ</i><sup>15</sup>N, soil <i>δ</i><sup>15</sup>N, net nitrification, net N mineralization, and the ratio of dissolved inorganic to organic nitrogen (DIN : DON) in soil solution and streams. We were particularly interested in whether terrestrial and stream based proxies for N availability were correlated where they were measured in the same place. Not surprisingly, the strongest correlation (Kendall's <i>τ</i>) was between net nitrification and N mineralization (<i>τ</i>  =  0.71, <i>p</i> &lt; 0.0001). Net nitrification and N mineralization were each correlated with foliar and soil <i>δ</i><sup>15</sup>N (<i>p</i> &lt; 0.05). Foliar and soil <i>δ</i><sup>15</sup>N were more tightly correlated in tropical sites (<i>τ</i>  =  0.68, <i>p</i> &lt; 0.0001), than in temperate sites (<i>τ</i>  =  0.23, <i>p</i>  =  0.02). The only significant correlations between terrestrial- and water-based metrics were those of net nitrification (<i>τ</i>  =  0.48, <i>p</i>  =  0.01) and N mineralization (<i>τ</i>  =  0.69, <i>p</i>  =  0.0001) with stream DIN : DON. The relationship between stream DIN : DON with both net nitrification and N mineralization was significant only in temperate, but not tropical regions. To our surprise, we did not find a significant correlation between soil <i>δ</i><sup>15</sup>N and stream DIN : DON, despite the fact that both have been used to infer spatially or temporally integrated N status. Given that both soil <i>δ</i><sup>15</sup>N and stream DIN : DON are used to infer long-term N status, their lack of correlation in watersheds merits further investigation.http://www.biogeosciences.net/13/5395/2016/bg-13-5395-2016.pdf
collection DOAJ
language English
format Article
sources DOAJ
author M. Almaraz
S. Porder
spellingShingle M. Almaraz
S. Porder
Reviews and syntheses: measuring ecosystem nitrogen status – a comparison of proxies
Biogeosciences
author_facet M. Almaraz
S. Porder
author_sort M. Almaraz
title Reviews and syntheses: measuring ecosystem nitrogen status – a comparison of proxies
title_short Reviews and syntheses: measuring ecosystem nitrogen status – a comparison of proxies
title_full Reviews and syntheses: measuring ecosystem nitrogen status – a comparison of proxies
title_fullStr Reviews and syntheses: measuring ecosystem nitrogen status – a comparison of proxies
title_full_unstemmed Reviews and syntheses: measuring ecosystem nitrogen status – a comparison of proxies
title_sort reviews and syntheses: measuring ecosystem nitrogen status – a comparison of proxies
publisher Copernicus Publications
series Biogeosciences
issn 1726-4170
1726-4189
publishDate 2016-09-01
description There are many proxies used to measure nitrogen (N) availability in watersheds, but the degree to which they do (or do not) correlate within a watershed has not been systematically addressed. We surveyed the literature for intact forest or grassland watersheds globally, in which several metrics of nitrogen availability have been measured. Our metrics included the following: foliar <i>δ</i><sup>15</sup>N, soil <i>δ</i><sup>15</sup>N, net nitrification, net N mineralization, and the ratio of dissolved inorganic to organic nitrogen (DIN : DON) in soil solution and streams. We were particularly interested in whether terrestrial and stream based proxies for N availability were correlated where they were measured in the same place. Not surprisingly, the strongest correlation (Kendall's <i>τ</i>) was between net nitrification and N mineralization (<i>τ</i>  =  0.71, <i>p</i> &lt; 0.0001). Net nitrification and N mineralization were each correlated with foliar and soil <i>δ</i><sup>15</sup>N (<i>p</i> &lt; 0.05). Foliar and soil <i>δ</i><sup>15</sup>N were more tightly correlated in tropical sites (<i>τ</i>  =  0.68, <i>p</i> &lt; 0.0001), than in temperate sites (<i>τ</i>  =  0.23, <i>p</i>  =  0.02). The only significant correlations between terrestrial- and water-based metrics were those of net nitrification (<i>τ</i>  =  0.48, <i>p</i>  =  0.01) and N mineralization (<i>τ</i>  =  0.69, <i>p</i>  =  0.0001) with stream DIN : DON. The relationship between stream DIN : DON with both net nitrification and N mineralization was significant only in temperate, but not tropical regions. To our surprise, we did not find a significant correlation between soil <i>δ</i><sup>15</sup>N and stream DIN : DON, despite the fact that both have been used to infer spatially or temporally integrated N status. Given that both soil <i>δ</i><sup>15</sup>N and stream DIN : DON are used to infer long-term N status, their lack of correlation in watersheds merits further investigation.
url http://www.biogeosciences.net/13/5395/2016/bg-13-5395-2016.pdf
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