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Application of the isotope pairing technique in sediments: Use, challenges, and new directions

Publikation: Bidrag til tidsskrift/Konferencebidrag i tidsskrift /Bidrag til avisReviewForskningpeer review

Standard

Application of the isotope pairing technique in sediments : Use, challenges, and new directions. / Robertson, Elizabeth K.; Bartoli, Marco; Brüchert, Volker; Dalsgaard, Tage; Hall, Per O.J.; Hellemann, Dana; Hietanen, Susanna; Zilius, Mindaugas; Conley, Daniel J.

I: Limnology and Oceanography: Methods, Bind 17, Nr. 2, 02.2019, s. 112-136.

Publikation: Bidrag til tidsskrift/Konferencebidrag i tidsskrift /Bidrag til avisReviewForskningpeer review

Harvard

Robertson, EK, Bartoli, M, Brüchert, V, Dalsgaard, T, Hall, POJ, Hellemann, D, Hietanen, S, Zilius, M & Conley, DJ 2019, 'Application of the isotope pairing technique in sediments: Use, challenges, and new directions', Limnology and Oceanography: Methods, bind 17, nr. 2, s. 112-136. https://doi.org/10.1002/lom3.10303

APA

Robertson, E. K., Bartoli, M., Brüchert, V., Dalsgaard, T., Hall, P. O. J., Hellemann, D., ... Conley, D. J. (2019). Application of the isotope pairing technique in sediments: Use, challenges, and new directions. Limnology and Oceanography: Methods, 17(2), 112-136. https://doi.org/10.1002/lom3.10303

CBE

Robertson EK, Bartoli M, Brüchert V, Dalsgaard T, Hall POJ, Hellemann D, Hietanen S, Zilius M, Conley DJ. 2019. Application of the isotope pairing technique in sediments: Use, challenges, and new directions. Limnology and Oceanography: Methods. 17(2):112-136. https://doi.org/10.1002/lom3.10303

MLA

Robertson, Elizabeth K. o.a.. "Application of the isotope pairing technique in sediments: Use, challenges, and new directions". Limnology and Oceanography: Methods. 2019, 17(2). 112-136. https://doi.org/10.1002/lom3.10303

Vancouver

Robertson EK, Bartoli M, Brüchert V, Dalsgaard T, Hall POJ, Hellemann D o.a. Application of the isotope pairing technique in sediments: Use, challenges, and new directions. Limnology and Oceanography: Methods. 2019 feb;17(2):112-136. https://doi.org/10.1002/lom3.10303

Author

Robertson, Elizabeth K. ; Bartoli, Marco ; Brüchert, Volker ; Dalsgaard, Tage ; Hall, Per O.J. ; Hellemann, Dana ; Hietanen, Susanna ; Zilius, Mindaugas ; Conley, Daniel J. / Application of the isotope pairing technique in sediments : Use, challenges, and new directions. I: Limnology and Oceanography: Methods. 2019 ; Bind 17, Nr. 2. s. 112-136.

Bibtex

@article{3ad811a03dfa4a5781917fd01cce4b7e,
title = "Application of the isotope pairing technique in sediments: Use, challenges, and new directions",
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 15 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.",
author = "Robertson, {Elizabeth K.} and Marco Bartoli and Volker Br{\"u}chert and Tage Dalsgaard and Hall, {Per O.J.} and Dana Hellemann and Susanna Hietanen and Mindaugas Zilius and Conley, {Daniel J.}",
year = "2019",
month = "2",
doi = "10.1002/lom3.10303",
language = "English",
volume = "17",
pages = "112--136",
journal = "Limnology and Oceanography: Methods",
issn = "1541-5856",
publisher = "John Wiley & Sons, Inc.",
number = "2",

}

RIS

TY - JOUR

T1 - Application of the isotope pairing technique in sediments

T2 - Use, challenges, and new directions

AU - Robertson, Elizabeth K.

AU - Bartoli, Marco

AU - Brüchert, Volker

AU - Dalsgaard, Tage

AU - Hall, Per O.J.

AU - Hellemann, Dana

AU - Hietanen, Susanna

AU - Zilius, Mindaugas

AU - Conley, Daniel J.

PY - 2019/2

Y1 - 2019/2

N2 - 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 15 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.

AB - 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 15 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.

UR - http://www.scopus.com/inward/record.url?scp=85059943720&partnerID=8YFLogxK

U2 - 10.1002/lom3.10303

DO - 10.1002/lom3.10303

M3 - Review

VL - 17

SP - 112

EP - 136

JO - Limnology and Oceanography: Methods

JF - Limnology and Oceanography: Methods

SN - 1541-5856

IS - 2

ER -