Decline in Ecosystem δ¹³C and Mid-Successional Nitrogen Loss in a Two-Century Postglacial Chronosequence
Uncertainty about controls on long-term carbon (C) and nitrogen (N) balance, turnover, and isotopic composition currently limits our ability to predict ecosystem response to disturbance and landscape change. We used a two-century, postglacial chronosequence in Glacier Bay, Alaska, to explore the inf...
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ftleedsuniv:oai:eprints.whiterose.ac.uk:129135 2023-05-15T16:20:44+02:00 Decline in Ecosystem δ¹³C and Mid-Successional Nitrogen Loss in a Two-Century Postglacial Chronosequence Malone, ET Abbott, BW Klaar, MJ Kidd, C Sebilo, M Milner, AM Pinay, G 2018-12 text https://eprints.whiterose.ac.uk/129135/ https://eprints.whiterose.ac.uk/129135/24/noy020.pdf https://eprints.whiterose.ac.uk/129135/10/Malone%20et%20al%202018_Supplemental%20Info%20Final.pdf en eng Springer Nature https://eprints.whiterose.ac.uk/129135/24/noy020.pdf https://eprints.whiterose.ac.uk/129135/10/Malone%20et%20al%202018_Supplemental%20Info%20Final.pdf Malone, ET, Abbott, BW, Klaar, MJ et al. (4 more authors) (2018) Decline in Ecosystem δ¹³C and Mid-Successional Nitrogen Loss in a Two-Century Postglacial Chronosequence. Ecosystems, 21 (8). pp. 1659-1675. ISSN 1432-9840 cc_by_4 CC-BY Article NonPeerReviewed 2018 ftleedsuniv 2023-01-30T22:05:10Z Uncertainty about controls on long-term carbon (C) and nitrogen (N) balance, turnover, and isotopic composition currently limits our ability to predict ecosystem response to disturbance and landscape change. We used a two-century, postglacial chronosequence in Glacier Bay, Alaska, to explore the influence of C and N dynamics on soil and leaf stable isotopes. C dynamics were closely linked to soil hydrology, with increasing soil water retention during ecosystem development resulting in a linear decrease in foliar and soil δ¹³C, independent of shifts in vegetation cover and despite constant precipitation across sites. N dynamics responded to interactions among soil development, vegetation type, microbial activity, and topography. Contrary to the predictions of nutrient retention theory, potential nitrification and denitrification were high, relative to inorganic N stocks, from the beginning of the chronosequence, and gaseous and hydrological N losses were highest at mid-successional sites, 140–165 years since deglaciation. Though leaching of dissolved N is considered the predominant pathway of N loss at high latitudes, we found that gaseous N loss was more tightly correlated with δ¹⁵N enrichment. These results suggest that δ¹³C in leaves and soil can depend as much on soil development and associated water availability as on climate and that N availability and export depend on interactions between physical and biological state factors. Article in Journal/Newspaper glacier Alaska White Rose Research Online (Universities of Leeds, Sheffield & York) Glacier Bay |
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Open Polar |
collection |
White Rose Research Online (Universities of Leeds, Sheffield & York) |
op_collection_id |
ftleedsuniv |
language |
English |
description |
Uncertainty about controls on long-term carbon (C) and nitrogen (N) balance, turnover, and isotopic composition currently limits our ability to predict ecosystem response to disturbance and landscape change. We used a two-century, postglacial chronosequence in Glacier Bay, Alaska, to explore the influence of C and N dynamics on soil and leaf stable isotopes. C dynamics were closely linked to soil hydrology, with increasing soil water retention during ecosystem development resulting in a linear decrease in foliar and soil δ¹³C, independent of shifts in vegetation cover and despite constant precipitation across sites. N dynamics responded to interactions among soil development, vegetation type, microbial activity, and topography. Contrary to the predictions of nutrient retention theory, potential nitrification and denitrification were high, relative to inorganic N stocks, from the beginning of the chronosequence, and gaseous and hydrological N losses were highest at mid-successional sites, 140–165 years since deglaciation. Though leaching of dissolved N is considered the predominant pathway of N loss at high latitudes, we found that gaseous N loss was more tightly correlated with δ¹⁵N enrichment. These results suggest that δ¹³C in leaves and soil can depend as much on soil development and associated water availability as on climate and that N availability and export depend on interactions between physical and biological state factors. |
format |
Article in Journal/Newspaper |
author |
Malone, ET Abbott, BW Klaar, MJ Kidd, C Sebilo, M Milner, AM Pinay, G |
spellingShingle |
Malone, ET Abbott, BW Klaar, MJ Kidd, C Sebilo, M Milner, AM Pinay, G Decline in Ecosystem δ¹³C and Mid-Successional Nitrogen Loss in a Two-Century Postglacial Chronosequence |
author_facet |
Malone, ET Abbott, BW Klaar, MJ Kidd, C Sebilo, M Milner, AM Pinay, G |
author_sort |
Malone, ET |
title |
Decline in Ecosystem δ¹³C and Mid-Successional Nitrogen Loss in a Two-Century Postglacial Chronosequence |
title_short |
Decline in Ecosystem δ¹³C and Mid-Successional Nitrogen Loss in a Two-Century Postglacial Chronosequence |
title_full |
Decline in Ecosystem δ¹³C and Mid-Successional Nitrogen Loss in a Two-Century Postglacial Chronosequence |
title_fullStr |
Decline in Ecosystem δ¹³C and Mid-Successional Nitrogen Loss in a Two-Century Postglacial Chronosequence |
title_full_unstemmed |
Decline in Ecosystem δ¹³C and Mid-Successional Nitrogen Loss in a Two-Century Postglacial Chronosequence |
title_sort |
decline in ecosystem δ¹³c and mid-successional nitrogen loss in a two-century postglacial chronosequence |
publisher |
Springer Nature |
publishDate |
2018 |
url |
https://eprints.whiterose.ac.uk/129135/ https://eprints.whiterose.ac.uk/129135/24/noy020.pdf https://eprints.whiterose.ac.uk/129135/10/Malone%20et%20al%202018_Supplemental%20Info%20Final.pdf |
geographic |
Glacier Bay |
geographic_facet |
Glacier Bay |
genre |
glacier Alaska |
genre_facet |
glacier Alaska |
op_relation |
https://eprints.whiterose.ac.uk/129135/24/noy020.pdf https://eprints.whiterose.ac.uk/129135/10/Malone%20et%20al%202018_Supplemental%20Info%20Final.pdf Malone, ET, Abbott, BW, Klaar, MJ et al. (4 more authors) (2018) Decline in Ecosystem δ¹³C and Mid-Successional Nitrogen Loss in a Two-Century Postglacial Chronosequence. Ecosystems, 21 (8). pp. 1659-1675. ISSN 1432-9840 |
op_rights |
cc_by_4 |
op_rightsnorm |
CC-BY |
_version_ |
1766008699693826048 |