Low particulate carbon to nitrogen ratios in marine surface waters of the Arctic

During the Canada Three Oceans and Joint Ocean Ice Study projects in the summers of 2007 and 2008, we measured particulate organic carbon to nitrogen ratios (POC:PON) throughout the euphotic zone in subarctic and arctic waters. Depth-integrated values averaged 2.65 (±0.19) in the Beaufort Sea and Ca...

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Autores principales: Crawford, David W., Wyatt, Shea N., Wrohan, Ian A., Cefarelli, Adrián Oscar, Giesbrecht, Karina E., Kelly, Brianne, Varela, Diana E.
Formato: Articulo
Lenguaje:Inglés
Publicado: 2015
Materias:
Acceso en línea:http://sedici.unlp.edu.ar/handle/10915/145939
Aporte de:
id I19-R120-10915-145939
record_format dspace
institution Universidad Nacional de La Plata
institution_str I-19
repository_str R-120
collection SEDICI (UNLP)
language Inglés
topic Biología
C:N ratios
Redfield ratios
Particulates
Uptake rates
Phytoplankton
Arctic
spellingShingle Biología
C:N ratios
Redfield ratios
Particulates
Uptake rates
Phytoplankton
Arctic
Crawford, David W.
Wyatt, Shea N.
Wrohan, Ian A.
Cefarelli, Adrián Oscar
Giesbrecht, Karina E.
Kelly, Brianne
Varela, Diana E.
Low particulate carbon to nitrogen ratios in marine surface waters of the Arctic
topic_facet Biología
C:N ratios
Redfield ratios
Particulates
Uptake rates
Phytoplankton
Arctic
description During the Canada Three Oceans and Joint Ocean Ice Study projects in the summers of 2007 and 2008, we measured particulate organic carbon to nitrogen ratios (POC:PON) throughout the euphotic zone in subarctic and arctic waters. Depth-integrated values averaged 2.65 (±0.19) in the Beaufort Sea and Canada Basin (BS-CB domain), and were much lower than both the Redfield ratio (6.6) and the average ratios (3.9 to 5.6) measured across other arctic-subarctic domains. Average uptake ratios of C and N (ρC:ρN) were also lower (0.87±0.14) in BS-CB than in the other four domains (2.10 to 3.51). Decreasing POC:PON ratios were associated with low concentrations of phytoplankton C, reduced abundance of biogenic silica (bSiO2), a smaller relative contribution of the >5 µm fraction to total chlorophyll a and a larger relative contribution of small flagellates (<8 µm) to phytoplankton C. In the subsurface chlorophyll a maximum (SCM) within the BS-CB domain, phytoplankton C represented only ~13% of POC, and therefore low POC:PON may be influenced by the presence of heterotrophic microbes. These ratios are supported by data obtained during other arctic programs in 2006, 2008 and 2009. Previous work has suggested a link between freshening of surface waters and increasing dominance of picophytoplankton and bacterioplankton in the Canada Basin, and the low POC:PON ratios measured during this study may be a consequence of this shift. Our results have ramifications for the conversion between C- and N-based estimates of primary productivity, and for biogeochemical modeling of marine arctic waters.
format Articulo
Articulo
author Crawford, David W.
Wyatt, Shea N.
Wrohan, Ian A.
Cefarelli, Adrián Oscar
Giesbrecht, Karina E.
Kelly, Brianne
Varela, Diana E.
author_facet Crawford, David W.
Wyatt, Shea N.
Wrohan, Ian A.
Cefarelli, Adrián Oscar
Giesbrecht, Karina E.
Kelly, Brianne
Varela, Diana E.
author_sort Crawford, David W.
title Low particulate carbon to nitrogen ratios in marine surface waters of the Arctic
title_short Low particulate carbon to nitrogen ratios in marine surface waters of the Arctic
title_full Low particulate carbon to nitrogen ratios in marine surface waters of the Arctic
title_fullStr Low particulate carbon to nitrogen ratios in marine surface waters of the Arctic
title_full_unstemmed Low particulate carbon to nitrogen ratios in marine surface waters of the Arctic
title_sort low particulate carbon to nitrogen ratios in marine surface waters of the arctic
publishDate 2015
url http://sedici.unlp.edu.ar/handle/10915/145939
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