FN Archimer Export Format
PT J
TI Seasonal patterns in Arctic planktonic metabolism (Fram Strait - Svalbard region)
BT 
AF VAQUER-SUNYER, R.
   DUARTE, C. M.
   REGAUDIE-DE-GIOUX, Aurore
   HOLDING, J.
   GARCIA-CORRAL, L. S.
   REIGSTAD, M.
   WASSMANN, P.
AS 1:1;2:2,3,4;3:2;4:2;5:2;6:5;7:5;
FF 1:;2:;3:;4:;5:;6:;7:;
C1 Lund Univ, Dept Geol, S-22362 Lund, Sweden.
   IMEDEA CSIC UIB Inst Mediterani Estudis Avancats, Dept Global Change Res, Esporles 07190, Mallorca, Spain.
   Univ Western Australia, UWA Oceans Inst, Crawle, Australia.
   Univ Western Australia, Sch Plant Biol, Crawle, Australia.
   Univ Tromso, Fac Biosci Fisheries & Econ, N-9037 Tromso, Norway.
C2 UNIV LUND, SWEDEN
   CSIC, SPAIN
   UNIV WESTERN AUSTRALIA, AUSTRALIA
   UNIV WESTERN AUSTRALIA, AUSTRALIA
   UNIV TROMSO, NORWAY
IN DOAJ
IF 3.753
TC 28
UR https://archimer.ifremer.fr/doc/00419/53077/54027.pdf
   https://archimer.ifremer.fr/doc/00419/53077/54028.pdf
   https://archimer.ifremer.fr/doc/00419/53077/54029.pdf
LA English
DT Article
AB The metabolism of the Arctic Ocean is marked by extremely pronounced seasonality and spatial heterogeneity associated with light conditions, ice cover, water masses and nutrient availability. Here we report the marine planktonic metabolic rates (net community production, gross primary production and community respiration) along three different seasons of the year, for a total of eight cruises along the western sector of the European Arctic (Fram Strait - Svalbard region) in the Arctic Ocean margin: one at the end of 2006 (fall/winter), two in 2007 (early spring and summer), two in 2008 (early spring and summer), one in 2009 (late spring-early summer), one in 2010 (spring) and one in 2011 (spring). The results show that the metabolism of the western sector of the European Arctic varies throughout the year, depending mostly on the stage of bloom and water temperature. Here we report metabolic rates for the different periods, including the spring bloom, summer and the dark period, increasing considerably the empirical basis of metabolic rates in the Arctic Ocean, and especially in the European Arctic corridor. Additionally, a rough annual metabolic estimate for this area of the Arctic Ocean was calculated, resulting in a net community production of 108 g C m(-2) yr(-1). 
PY 2013
SO Biogeosciences
SN 1726-4170
PU Copernicus Gesellschaft Mbh
VL 10
IS 3
UT 000317010600016
BP 1451
EP 1469
DI 10.5194/bg-10-1451-2013
ID 53077
ER

EF