Production, partitioning and stoichiometry of organic matter under variable nutrient supply during mesocosm experiments in the tropical Pacific and Atlantic Ocean

Franz, Jasmin, Hauss, Helena, Sommer, Ulrich, Dittmar, T. and Riebesell, Ulf (2012) Production, partitioning and stoichiometry of organic matter under variable nutrient supply during mesocosm experiments in the tropical Pacific and Atlantic Ocean Biogeosciences (BG), 9 (11). pp. 4629-4643. DOI 10.5194/bg-9-4629-2012.

[img]
Preview
Text
bg-9-4629-2012.pdf - Published Version
Available under License Creative Commons Attribution.

Download (2937Kb) | Preview

Supplementary data:

Abstract

Oxygen-deficient waters in the ocean, generally referred to as oxygen minimum zones (OMZ), are expected to expand as a consequence of global climate change. Poor oxygenation is promoting microbial loss of inorganic nitrogen (N) and increasing release of sediment-bound phosphate (P) into the water column. These intermediate water masses, nutrient-loaded but with an N deficit relative to the canonical N:P Redfield ratio of 16:1, are transported via coastal upwelling into the euphotic zone. To test the impact of nutrient supply and nutrient stoichiometry on production, partitioning and elemental composition of dissolved (DOC, DON, DOP) and particulate (POC, PON, POP) organic matter, three nutrient enrichment experiments were conducted with natural microbial communities in shipboard mesocosms, during research cruises in the tropical waters of the southeast Pacific and the northeast Atlantic. Maximum accumulation of POC and PON was observed under high N supply conditions, indicating that primary production was controlled by N availability. The stoichiometry of microbial biomass was unaffected by nutrient N:P supply during exponential growth under nutrient saturation, while it was highly variable under conditions of nutrient limitation and closely correlated to the N:P supply ratio, although PON:POP of accumulated biomass generally exceeded the supply ratio. Microbial N:P composition was constrained by a general lower limit of 5:1. Channelling of assimilated P into DOP appears to be the mechanism responsible for the consistent offset of cellular stoichiometry relative to inorganic nutrient supply and nutrient drawdown, as DOP build-up was observed to intensify under decreasing N:P supply. Low nutrient N:P conditions in coastal upwelling areas overlying O2-deficient waters seem to represent a net source for DOP, which may stimulate growth of diazotrophic phytoplankton. These results demonstrate that microbial nutrient assimilation and partitioning of organic matter between the particulate and the dissolved phase are controlled by the N:P ratio of upwelled nutrients, implying substantial consequences for nutrient cycling and organic matter pools in the course of decreasing nutrient N:P stoichiometry.

Document Type: Article
Additional Information: WOS:000312667300032
Keywords: Pacific Ocean; Atlantic Ocean; ANAEROBIC AMMONIUM OXIDATION; ENRICHMENT EXPERIMENTS; ELEMENTAL COMPOSITION; PHOSPHORUS-COMPOUNDS; MARINE-SEDIMENTS; NORTH-ATLANTIC; LONG-TERM; N-P; PHYTOPLANKTON; LIMITATION
Research affiliation: OceanRep > GEOMAR > FB3 Marine Ecology > FB3-EOE-N Experimental Ecology - Food Webs
OceanRep > SFB 754 > B2
OceanRep > SFB 754
OceanRep > GEOMAR > FB2 Marine Biogeochemistry > FB2-BI Biological Oceanography
OceanRep > SFB 754 > B8
OceanRep > The Future Ocean - Cluster of Excellence
Refereed: Yes
DOI etc.: 10.5194/bg-9-4629-2012
ISSN: 1726-4170
Projects: SFB754, Future Ocean
Expeditions/Models:
Date Deposited: 22 Nov 2012 12:16
Last Modified: 11 Aug 2014 10:39
URI: http://eprints.uni-kiel.de/id/eprint/19248

Actions (login required)

View Item View Item

Document Downloads

More statistics for this item...