Imbalanced nutrient recycling in a warmer ocean driven by differential response of extracellular enzymatic activities

© 2017 John Wiley & Sons Ltd.

Bibliographische Detailangaben
Veröffentlicht in:Global change biology. - 1999. - 23(2017), 10 vom: 15. Okt., Seite 4084-4093
1. Verfasser: Ayo, Begoña (VerfasserIn)
Weitere Verfasser: Abad, Naiara, Artolozaga, Itxaso, Azua, Iñigo, Baña, Zuriñe, Unanue, Marian, Gasol, Josep M, Duarte, Carlos M, Iriberri, Juan
Format: Online-Aufsatz
Sprache:English
Veröffentlicht: 2017
Zugriff auf das übergeordnete Werk:Global change biology
Schlagworte:Journal Article C:N:P molar ratio alkaline phosphatase extracellular enzymatic activity global warming leucine aminopeptidase subtropical and tropical ocean temperature-sensitivity β-glucosidase Phosphorus 27YLU75U4W
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520 |a Ocean oligotrophication concurrent with warming weakens the capacity of marine primary producers to support marine food webs and act as a CO2 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 (Ea ), 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 Ea 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 Ea 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 
650 4 |a Journal Article 
650 4 |a C:N:P molar ratio 
650 4 |a alkaline phosphatase 
650 4 |a extracellular enzymatic activity 
650 4 |a global warming 
650 4 |a leucine aminopeptidase 
650 4 |a subtropical and tropical ocean 
650 4 |a temperature-sensitivity 
650 4 |a β-glucosidase 
650 7 |a Phosphorus  |2 NLM 
650 7 |a 27YLU75U4W  |2 NLM 
700 1 |a Abad, Naiara  |e verfasserin  |4 aut 
700 1 |a Artolozaga, Itxaso  |e verfasserin  |4 aut 
700 1 |a Azua, Iñigo  |e verfasserin  |4 aut 
700 1 |a Baña, Zuriñe  |e verfasserin  |4 aut 
700 1 |a Unanue, Marian  |e verfasserin  |4 aut 
700 1 |a Gasol, Josep M  |e verfasserin  |4 aut 
700 1 |a Duarte, Carlos M  |e verfasserin  |4 aut 
700 1 |a Iriberri, Juan  |e verfasserin  |4 aut 
773 0 8 |i Enthalten in  |t Global change biology  |d 1999  |g 23(2017), 10 vom: 15. Okt., Seite 4084-4093  |w (DE-627)NLM098239996  |x 1365-2486  |7 nnns 
773 1 8 |g volume:23  |g year:2017  |g number:10  |g day:15  |g month:10  |g pages:4084-4093 
856 4 0 |u http://dx.doi.org/10.1111/gcb.13779  |3 Volltext 
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