Sie befinden Sich nicht im Netzwerk der Universität Paderborn. Der Zugriff auf elektronische Ressourcen ist gegebenenfalls nur via VPN oder Shibboleth (DFN-AAI) möglich. mehr Informationen...
Potential bioavailability of organic matter from atmospheric particles to marine heterotrophic bacteria
Ist Teil von
Biogeosciences, 2020-12, Vol.17 (24), p.6271-6285
Ort / Verlag
Katlenburg-Lindau: Copernicus GmbH
Erscheinungsjahr
2020
Quelle
EZB Electronic Journals Library
Beschreibungen/Notizen
The surface ocean receives important amounts of organic carbon
from atmospheric deposition. The degree of bioavailability of this source of
organic carbon will determine its impact on the marine carbon cycle. In this
study, the potential availability of dissolved organic carbon (DOC) leached
from both desert dust and anthropogenic aerosols to marine heterotrophic
bacteria was investigated. The experimental design was based on 16 d
incubations, in the dark, of a marine bacterial inoculum into artificial
seawater amended with water-soluble Saharan dust (D treatment) and
anthropogenic (A treatment) aerosols, so that the initial DOC concentration
was similar between treatments. Glucose-amended (G) and non-amended
(control) treatments were run in parallel. Over the incubation period, an
increase in bacterial abundance (BA) and bacterial production (BP) was
observed first in the G treatment, followed then by the D and finally A
treatments, with bacterial growth rates significantly higher in the G and D
treatments than the A treatment. Following this growth, maxima of BP reached
were similar in the D (879 ± 64 ng C L−1 h−1; n=3) and G (648 ± 156 ng C L−1 h−1; n=3) treatments and were significantly
higher than in the A treatment (124 ng C L−1 h−1; n=2). The DOC
consumed over the incubation period was similar in the A (9 µM;
n=2) and D (9 ± 2 µM; n=3) treatments and was significantly
lower than in the G treatment (22 ± 3 µM; n=3). Nevertheless,
the bacterial growth efficiency (BGE) in the D treatment (14.2 ± 5.5 %; n=3) compared well with the G treatment (7.6 ± 2 %;
n=3), suggesting that the metabolic use of the labile DOC fraction in both
conditions was energetically equivalent. In contrast, the BGE in the A treatment was lower (1.7 %; n=2), suggesting that most of the used labile
DOC was catabolized. The results obtained in this study highlight the
potential of aerosol organic matter to sustain the metabolism of marine
heterotrophs and stress the need to include this external source of organic
carbon in biogeochemical models for a better constraining of the carbon
budget.