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Marine CDOM accumulation during a coastal Arctic mesocosm experiment: No response to elevated pCO 2 levels
Author(s) -
Pavlov Alexey K.,
Silyakova Anna,
Granskog Mats A.,
Bellerby Richard G.J.,
Engel Anja,
Schulz Kai G.,
Brussaard Corina P.D.
Publication year - 2014
Publication title -
journal of geophysical research: biogeosciences
Language(s) - English
Resource type - Journals
eISSN - 2169-8961
pISSN - 2169-8953
DOI - 10.1002/2013jg002587
Subject(s) - colored dissolved organic matter , mesocosm , biogeochemical cycle , environmental science , arctic , spectral slope , dissolved organic carbon , phytoplankton , dimethylsulfoniopropionate , oceanography , environmental chemistry , photosynthetically active radiation , zooplankton , ecosystem , chemistry , photosynthesis , ecology , biology , nutrient , botany , physics , geology , astronomy , spectral line
Abstract A large‐scale multidisciplinary mesocosm experiment in an Arctic fjord (Kongsfjorden, Svalbard; 78°56.2′N) was used to study Arctic marine food webs and biogeochemical elements cycling at natural and elevated future carbon dioxide (CO 2 ) levels. At the start of the experiment, marine‐derived chromophoric dissolved organic matter (CDOM) dominated the CDOM pool. Thus, this experiment constituted a convenient case to study production of autochthonous CDOM, which is typically masked by high levels of CDOM of terrestrial origin in the Arctic Ocean proper. CDOM accumulated during the experiment in line with an increase in bacterial abundance; however, no response was observed to increased pCO 2 levels. Changes in CDOM absorption spectral slopes indicate that bacteria were most likely responsible for the observed CDOM dynamics. Distinct absorption peaks (at ~ 330 and ~ 360 nm) were likely associated with mycosporine‐like amino acids (MAAs). Due to the experimental setup, MAAs were produced in absence of ultraviolet exposure providing evidence for MAAs to be considered as multipurpose metabolites rather than simple photoprotective compounds. We showed that a small increase in CDOM during the experiment made it a major contributor to total absorption in a range of photosynthetically active radiation (PAR, 400–700 nm) and, therefore, is important for spectral light availability and may be important for photosynthesis and phytoplankton groups composition in a rapidly changing Arctic marine ecosystem.