Back to Search
Start Over
Imbalanced nutrient recycling in a warmer ocean driven by differential response of extracellular enzymatic activities
- Source :
- Digital.CSIC. Repositorio Institucional del CSIC, instname
- Publication Year :
- 2017
- Publisher :
- Wiley, 2017.
-
Abstract
- 10 pages, 4 tables, supporting information https://dx.doi.org/10.1111/gcb.13779, database is available in https://doi.org/10.5281/zenodo.583989<br />Ocean oligotrophication concurrent with warming weakens the capacity of marine primary producers to support marine food webs and act as a CO sink, and is believed to result from reduced nutrient inputs associated to the stabilization of the thermocline. However, nutrient supply in the oligotrophic ocean is largely dependent on the recycling of organic matter. This involves hydrolytic processes catalyzed by extracellular enzymes released by bacteria, which temperature dependence has not yet been evaluated. Here, we report a global assessment of the temperature-sensitivity, as represented by the activation energies (E), of extracellular β-glucosidase (βG), leucine aminopeptidase (LAP) and alkaline phosphatase (AP) enzymatic activities, which enable the uptake by bacteria of substrates rich in carbon, nitrogen, and phosphorus, respectively. These E were calculated from two different approaches, temperature experimental manipulations and a space-for-time substitution approach, which generated congruent results. The three activities showed contrasting E in the subtropical and tropical ocean, with βG increasing the fastest with warming, followed by LAP, while AP showed the smallest increase. The estimated activation energies predict that the hydrolysis products under projected warming scenarios will have higher C:N, C:P and N:P molar ratios than those currently generated, and suggest that the warming of oceanic surface waters leads to a decline in the nutrient supply to the microbial heterotrophic community relative to that of carbon, particularly so for phosphorus, slowing down nutrient recycling and contributing to further ocean oligotrophication.<br />This is a contribution to the MALASPINA Expedition 2010 project, funded by the CONSOLIDER-Ingenio 2010 program from the Spanish Ministry of Economy and Competitiveness (Ref. CSD2008-00077). NA was supported by a grant from the Basque Government (Ref. BFI-2010-130)
- Subjects :
- 0106 biological sciences
Nutrient cycle
010504 meteorology & atmospheric sciences
Oceans and Seas
Heterotroph
chemistry.chemical_element
Biology
01 natural sciences
Leucine aminopeptidase
Nutrient
Alkaline phosphatase
Environmental Chemistry
Organic matter
0105 earth and related environmental sciences
General Environmental Science
chemistry.chemical_classification
Extracellular enzymatic activity
Temperature-sensitivity
Global and Planetary Change
Bacteria
Ecology
Primary producers
N:P molar ratio [C]
Global warming
010604 marine biology & hydrobiology
Temperature
Heterotrophic Processes
Phosphorus
Nitrogen
B-glucosidase
chemistry
Environmental chemistry
Subtropical and tropical ocean
C:N:P molar ratio
Water Microbiology
Thermocline
Subjects
Details
- ISSN :
- 13541013
- Volume :
- 23
- Database :
- OpenAIRE
- Journal :
- Global Change Biology
- Accession number :
- edsair.doi.dedup.....b09af34b27dc9a0226c4cef23f9d4999
- Full Text :
- https://doi.org/10.1111/gcb.13779