The transformation and fate of sub-Arctic microphytobenthos carbon revealed through 13C-labeling

Microphytobenthos (MPB) at higher latitudes has been poorly studied. This study used pulse-chase 13C-labeling to investigate the production, processing, and fate of MPB-derived carbon (MPB-C) in sub-Arctic intertidal sediments over 31 d. Gross primary production (2.1 mmol C m−2 h−1 ± 0.4 mmol C m−2...

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Published in:Limnology and Oceanography
Main Authors: Oakes, Joanne M, Rysgaard, Soren, Glud, Ronnie N, Eyre, Bradley D
Format: Article in Journal/Newspaper
Language:unknown
Published: ePublications@SCU 2016
Subjects:
Online Access:https://epubs.scu.edu.au/esm_pubs/3116
https://doi.org/10.1002/lno.10377
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spelling ftsoutherncu:oai:epubs.scu.edu.au:esm_pubs-4144 2023-05-15T14:51:52+02:00 The transformation and fate of sub-Arctic microphytobenthos carbon revealed through 13C-labeling Oakes, Joanne M Rysgaard, Soren Glud, Ronnie N Eyre, Bradley D 2016-01-01T08:00:00Z https://epubs.scu.edu.au/esm_pubs/3116 https://doi.org/10.1002/lno.10377 unknown ePublications@SCU School of Environment, Science and Engineering Papers Environmental Sciences article 2016 ftsoutherncu https://doi.org/10.1002/lno.10377 2019-08-06T13:10:59Z Microphytobenthos (MPB) at higher latitudes has been poorly studied. This study used pulse-chase 13C-labeling to investigate the production, processing, and fate of MPB-derived carbon (MPB-C) in sub-Arctic intertidal sediments over 31 d. Gross primary production (2.1 mmol C m−2 h−1 ± 0.4 mmol C m−2 h−1) was comparable to that reported for temperate regions. Some of the 13C fixed by sub-Arctic MPB was rapidly (within 0.5 d) transferred to deeper sediments (below 2 cm), but most was retained within surface sediments (>70.2% of the 13C present at any time during the study). At any time, MPB accounted for ≥ 49.8% of this 13C. The 13C content of sediment organic carbon declined over time, but > 31% of the 13C fixed within the first tidal cycle remained after 31 d, suggesting that sub-Arctic MPB may contribute to coastal carbon retention during the productive season. Over 21 d, 10.6% of the fixed 13C was removed via DIC fluxes and 0.3% via DOC fluxes from inundated sediment, and 0.6% as CO2 from exposed sediment. The greatest loss of 13C (38.2%) was via unmeasured pathways, including resuspension and/or removal by mobile consumers. The rates of MPB-C production and the relative importance of the pathways for MPB-C loss were similar to that observed for comparable lower latitude sediments, demonstrating that MPB at higher latitudes are not necessarily distinct from MPB at lower latitudes and probably play a similarly important role in ecosystem functioning. Apparently, local environmental conditions are more important than climate differences for determining the processing and fate of MPB-C. Article in Journal/Newspaper Arctic Southern Cross University: epublications@SCU Arctic Limnology and Oceanography 61 6 2296 2308
institution Open Polar
collection Southern Cross University: epublications@SCU
op_collection_id ftsoutherncu
language unknown
topic Environmental Sciences
spellingShingle Environmental Sciences
Oakes, Joanne M
Rysgaard, Soren
Glud, Ronnie N
Eyre, Bradley D
The transformation and fate of sub-Arctic microphytobenthos carbon revealed through 13C-labeling
topic_facet Environmental Sciences
description Microphytobenthos (MPB) at higher latitudes has been poorly studied. This study used pulse-chase 13C-labeling to investigate the production, processing, and fate of MPB-derived carbon (MPB-C) in sub-Arctic intertidal sediments over 31 d. Gross primary production (2.1 mmol C m−2 h−1 ± 0.4 mmol C m−2 h−1) was comparable to that reported for temperate regions. Some of the 13C fixed by sub-Arctic MPB was rapidly (within 0.5 d) transferred to deeper sediments (below 2 cm), but most was retained within surface sediments (>70.2% of the 13C present at any time during the study). At any time, MPB accounted for ≥ 49.8% of this 13C. The 13C content of sediment organic carbon declined over time, but > 31% of the 13C fixed within the first tidal cycle remained after 31 d, suggesting that sub-Arctic MPB may contribute to coastal carbon retention during the productive season. Over 21 d, 10.6% of the fixed 13C was removed via DIC fluxes and 0.3% via DOC fluxes from inundated sediment, and 0.6% as CO2 from exposed sediment. The greatest loss of 13C (38.2%) was via unmeasured pathways, including resuspension and/or removal by mobile consumers. The rates of MPB-C production and the relative importance of the pathways for MPB-C loss were similar to that observed for comparable lower latitude sediments, demonstrating that MPB at higher latitudes are not necessarily distinct from MPB at lower latitudes and probably play a similarly important role in ecosystem functioning. Apparently, local environmental conditions are more important than climate differences for determining the processing and fate of MPB-C.
format Article in Journal/Newspaper
author Oakes, Joanne M
Rysgaard, Soren
Glud, Ronnie N
Eyre, Bradley D
author_facet Oakes, Joanne M
Rysgaard, Soren
Glud, Ronnie N
Eyre, Bradley D
author_sort Oakes, Joanne M
title The transformation and fate of sub-Arctic microphytobenthos carbon revealed through 13C-labeling
title_short The transformation and fate of sub-Arctic microphytobenthos carbon revealed through 13C-labeling
title_full The transformation and fate of sub-Arctic microphytobenthos carbon revealed through 13C-labeling
title_fullStr The transformation and fate of sub-Arctic microphytobenthos carbon revealed through 13C-labeling
title_full_unstemmed The transformation and fate of sub-Arctic microphytobenthos carbon revealed through 13C-labeling
title_sort transformation and fate of sub-arctic microphytobenthos carbon revealed through 13c-labeling
publisher ePublications@SCU
publishDate 2016
url https://epubs.scu.edu.au/esm_pubs/3116
https://doi.org/10.1002/lno.10377
geographic Arctic
geographic_facet Arctic
genre Arctic
genre_facet Arctic
op_source School of Environment, Science and Engineering Papers
op_doi https://doi.org/10.1002/lno.10377
container_title Limnology and Oceanography
container_volume 61
container_issue 6
container_start_page 2296
op_container_end_page 2308
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