Microbial nitrogen dynamics in organic and mineral soil horizons along a latitudinal transect in western Siberia
Soil N availability is constrained by the breakdown of N-containing polymers such as proteins to oligopeptides and amino acids that can be taken up by plants and microorganisms. Excess N is released from microbial cells as ammonium (N mineralization), which in turn can serve as substrate for nitrifi...
Published in: | Global Biogeochemical Cycles |
---|---|
Main Authors: | , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
2015
|
Subjects: | |
Online Access: | https://eprints.lancs.ac.uk/id/eprint/79564/ https://doi.org/10.1002/2015GB005084 |
id |
ftulancaster:oai:eprints.lancs.ac.uk:79564 |
---|---|
record_format |
openpolar |
spelling |
ftulancaster:oai:eprints.lancs.ac.uk:79564 2023-08-27T04:07:46+02:00 Microbial nitrogen dynamics in organic and mineral soil horizons along a latitudinal transect in western Siberia Wild, Birgit Schnecker, Jörg Knoltsch, Anna Takriti, Mounir Mooshammer, Maria Gentsch, Norman Mikutta, Robert Alves, Ricardo J Eloy Gittel, Antje Lashchinskiy, Nikolay Richter, Andreas 2015-05 https://eprints.lancs.ac.uk/id/eprint/79564/ https://doi.org/10.1002/2015GB005084 unknown Wild, Birgit and Schnecker, Jörg and Knoltsch, Anna and Takriti, Mounir and Mooshammer, Maria and Gentsch, Norman and Mikutta, Robert and Alves, Ricardo J Eloy and Gittel, Antje and Lashchinskiy, Nikolay and Richter, Andreas (2015) Microbial nitrogen dynamics in organic and mineral soil horizons along a latitudinal transect in western Siberia. Global Biogeochemical Cycles, 29 (5). pp. 567-582. ISSN 0886-6236 Journal Article PeerReviewed 2015 ftulancaster https://doi.org/10.1002/2015GB005084 2023-08-03T22:29:21Z Soil N availability is constrained by the breakdown of N-containing polymers such as proteins to oligopeptides and amino acids that can be taken up by plants and microorganisms. Excess N is released from microbial cells as ammonium (N mineralization), which in turn can serve as substrate for nitrification. According to stoichiometric theory, N mineralization and nitrification are expected to increase in relation to protein depolymerization with decreasing N limitation, and thus from higher to lower latitudes and from topsoils to subsoils. To test these hypotheses, we compared gross rates of protein depolymerization, N mineralization and nitrification (determined using (15)N pool dilution assays) in organic topsoil, mineral topsoil, and mineral subsoil of seven ecosystems along a latitudinal transect in western Siberia, from tundra (67°N) to steppe (54°N). The investigated ecosystems differed strongly in N transformation rates, with highest protein depolymerization and N mineralization rates in middle and southern taiga. All N transformation rates decreased with soil depth following the decrease in organic matter content. Related to protein depolymerization, N mineralization and nitrification were significantly higher in mineral than in organic horizons, supporting a decrease in microbial N limitation with depth. In contrast, we did not find indications for a decrease in microbial N limitation from arctic to temperate ecosystems along the transect. Our findings thus challenge the perception of ubiquitous N limitation at high latitudes, but suggest a transition from N to C limitation of microorganisms with soil depth, even in high-latitude systems such as tundra and boreal forest.\n\nKEY POINTS: We compared soil N dynamics of seven ecosystems along a latitudinal transectShifts in N dynamics suggest a decrease in microbial N limitation with depthWe found no decrease in microbial N limitation from arctic to temperate zones. Article in Journal/Newspaper Arctic taiga Tundra Siberia Lancaster University: Lancaster Eprints Arctic Global Biogeochemical Cycles 29 5 567 582 |
institution |
Open Polar |
collection |
Lancaster University: Lancaster Eprints |
op_collection_id |
ftulancaster |
language |
unknown |
description |
Soil N availability is constrained by the breakdown of N-containing polymers such as proteins to oligopeptides and amino acids that can be taken up by plants and microorganisms. Excess N is released from microbial cells as ammonium (N mineralization), which in turn can serve as substrate for nitrification. According to stoichiometric theory, N mineralization and nitrification are expected to increase in relation to protein depolymerization with decreasing N limitation, and thus from higher to lower latitudes and from topsoils to subsoils. To test these hypotheses, we compared gross rates of protein depolymerization, N mineralization and nitrification (determined using (15)N pool dilution assays) in organic topsoil, mineral topsoil, and mineral subsoil of seven ecosystems along a latitudinal transect in western Siberia, from tundra (67°N) to steppe (54°N). The investigated ecosystems differed strongly in N transformation rates, with highest protein depolymerization and N mineralization rates in middle and southern taiga. All N transformation rates decreased with soil depth following the decrease in organic matter content. Related to protein depolymerization, N mineralization and nitrification were significantly higher in mineral than in organic horizons, supporting a decrease in microbial N limitation with depth. In contrast, we did not find indications for a decrease in microbial N limitation from arctic to temperate ecosystems along the transect. Our findings thus challenge the perception of ubiquitous N limitation at high latitudes, but suggest a transition from N to C limitation of microorganisms with soil depth, even in high-latitude systems such as tundra and boreal forest.\n\nKEY POINTS: We compared soil N dynamics of seven ecosystems along a latitudinal transectShifts in N dynamics suggest a decrease in microbial N limitation with depthWe found no decrease in microbial N limitation from arctic to temperate zones. |
format |
Article in Journal/Newspaper |
author |
Wild, Birgit Schnecker, Jörg Knoltsch, Anna Takriti, Mounir Mooshammer, Maria Gentsch, Norman Mikutta, Robert Alves, Ricardo J Eloy Gittel, Antje Lashchinskiy, Nikolay Richter, Andreas |
spellingShingle |
Wild, Birgit Schnecker, Jörg Knoltsch, Anna Takriti, Mounir Mooshammer, Maria Gentsch, Norman Mikutta, Robert Alves, Ricardo J Eloy Gittel, Antje Lashchinskiy, Nikolay Richter, Andreas Microbial nitrogen dynamics in organic and mineral soil horizons along a latitudinal transect in western Siberia |
author_facet |
Wild, Birgit Schnecker, Jörg Knoltsch, Anna Takriti, Mounir Mooshammer, Maria Gentsch, Norman Mikutta, Robert Alves, Ricardo J Eloy Gittel, Antje Lashchinskiy, Nikolay Richter, Andreas |
author_sort |
Wild, Birgit |
title |
Microbial nitrogen dynamics in organic and mineral soil horizons along a latitudinal transect in western Siberia |
title_short |
Microbial nitrogen dynamics in organic and mineral soil horizons along a latitudinal transect in western Siberia |
title_full |
Microbial nitrogen dynamics in organic and mineral soil horizons along a latitudinal transect in western Siberia |
title_fullStr |
Microbial nitrogen dynamics in organic and mineral soil horizons along a latitudinal transect in western Siberia |
title_full_unstemmed |
Microbial nitrogen dynamics in organic and mineral soil horizons along a latitudinal transect in western Siberia |
title_sort |
microbial nitrogen dynamics in organic and mineral soil horizons along a latitudinal transect in western siberia |
publishDate |
2015 |
url |
https://eprints.lancs.ac.uk/id/eprint/79564/ https://doi.org/10.1002/2015GB005084 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic taiga Tundra Siberia |
genre_facet |
Arctic taiga Tundra Siberia |
op_relation |
Wild, Birgit and Schnecker, Jörg and Knoltsch, Anna and Takriti, Mounir and Mooshammer, Maria and Gentsch, Norman and Mikutta, Robert and Alves, Ricardo J Eloy and Gittel, Antje and Lashchinskiy, Nikolay and Richter, Andreas (2015) Microbial nitrogen dynamics in organic and mineral soil horizons along a latitudinal transect in western Siberia. Global Biogeochemical Cycles, 29 (5). pp. 567-582. ISSN 0886-6236 |
op_doi |
https://doi.org/10.1002/2015GB005084 |
container_title |
Global Biogeochemical Cycles |
container_volume |
29 |
container_issue |
5 |
container_start_page |
567 |
op_container_end_page |
582 |
_version_ |
1775348490883301376 |