Application of the isotope pairing technique in sediments : Use, challenges, and new directions
(2019) In Limnology and Oceanography: Methods 17(2). p.112-136- Abstract
Determining accurate rates of benthic nitrogen (N) removal and retention pathways from diverse environments is critical to our understanding of process distribution and constructing reliable N budgets and models. The whole-core 15N isotope pairing technique (IPT) is one of the most widely used methods to determine rates of benthic nitrate-reducing processes and has provided valuable information on processes and factors controlling N removal and retention in aquatic systems. While the whole core IPT has been employed in a range of environments, a number of methodological and environmental factors may lead to the generation of inaccurate data and are important to acknowledge for those applying the method. In this review, we... (More)
Determining accurate rates of benthic nitrogen (N) removal and retention pathways from diverse environments is critical to our understanding of process distribution and constructing reliable N budgets and models. The whole-core 15N isotope pairing technique (IPT) is one of the most widely used methods to determine rates of benthic nitrate-reducing processes and has provided valuable information on processes and factors controlling N removal and retention in aquatic systems. While the whole core IPT has been employed in a range of environments, a number of methodological and environmental factors may lead to the generation of inaccurate data and are important to acknowledge for those applying the method. In this review, we summarize the current state of the whole core IPT and highlight some of the important steps and considerations when employing the technique. We discuss environmental parameters which can pose issues to the application of the IPT and may lead to experimental artifacts, several of which are of particular importance in environments heavily impacted by eutrophication. Finally, we highlight the advances in the use of the whole-core IPT in combination with other methods, discuss new potential areas of consideration and encourage careful and considered use of the whole-core IPT. With the recognition of potential issues and proper use, the whole-core IPT will undoubtedly continue to develop, improve our understanding of benthic N cycling and allow more reliable budgets and predictions to be made.
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- author
- Robertson, Elizabeth K. LU ; Bartoli, Marco ; Brüchert, Volker ; Dalsgaard, Tage ; Hall, Per O.J. ; Hellemann, Dana ; Hietanen, Susanna ; Zilius, Mindaugas and Conley, Daniel J. LU
- organization
- publishing date
- 2019-01-13
- type
- Contribution to journal
- publication status
- published
- subject
- in
- Limnology and Oceanography: Methods
- volume
- 17
- issue
- 2
- pages
- 112 - 136
- publisher
- Wiley-Blackwell
- external identifiers
-
- scopus:85059943720
- ISSN
- 1541-5856
- DOI
- 10.1002/lom3.10303
- language
- English
- LU publication?
- yes
- id
- 255f23f7-3af3-413b-9a89-f729e16f031a
- date added to LUP
- 2019-01-24 13:17:51
- date last changed
- 2022-04-25 20:22:56
@article{255f23f7-3af3-413b-9a89-f729e16f031a,
abstract = {{<p>Determining accurate rates of benthic nitrogen (N) removal and retention pathways from diverse environments is critical to our understanding of process distribution and constructing reliable N budgets and models. The whole-core <sup>15</sup>N isotope pairing technique (IPT) is one of the most widely used methods to determine rates of benthic nitrate-reducing processes and has provided valuable information on processes and factors controlling N removal and retention in aquatic systems. While the whole core IPT has been employed in a range of environments, a number of methodological and environmental factors may lead to the generation of inaccurate data and are important to acknowledge for those applying the method. In this review, we summarize the current state of the whole core IPT and highlight some of the important steps and considerations when employing the technique. We discuss environmental parameters which can pose issues to the application of the IPT and may lead to experimental artifacts, several of which are of particular importance in environments heavily impacted by eutrophication. Finally, we highlight the advances in the use of the whole-core IPT in combination with other methods, discuss new potential areas of consideration and encourage careful and considered use of the whole-core IPT. With the recognition of potential issues and proper use, the whole-core IPT will undoubtedly continue to develop, improve our understanding of benthic N cycling and allow more reliable budgets and predictions to be made.</p>}},
author = {{Robertson, Elizabeth K. and Bartoli, Marco and Brüchert, Volker and Dalsgaard, Tage and Hall, Per O.J. and Hellemann, Dana and Hietanen, Susanna and Zilius, Mindaugas and Conley, Daniel J.}},
issn = {{1541-5856}},
language = {{eng}},
month = {{01}},
number = {{2}},
pages = {{112--136}},
publisher = {{Wiley-Blackwell}},
series = {{Limnology and Oceanography: Methods}},
title = {{Application of the isotope pairing technique in sediments : Use, challenges, and new directions}},
url = {{http://dx.doi.org/10.1002/lom3.10303}},
doi = {{10.1002/lom3.10303}},
volume = {{17}},
year = {{2019}},
}