GLORIA

GEOMAR Library Ocean Research Information Access

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
  • Other types  (2)
  • 2020-2022  (2)
Document type
Source
Language
Years
Year
  • 1
    Publication Date: 2021-09-29
    Description: Microbial degradation of dissolved organic matter (DOM) contributes to the formation and preservation of oxygen minimum zones (OMZs) in the ocean, but information on the spatial distribution and molecular composition of DOM in OMZ regions is scarce. We quantified molecular components of DOM that is, dissolved amino acids (DAA) and dissolved combined carbohydrates (DCCHO), in the upwelling region off Peru. We found the highest concentrations of DCCHO in fully oxygenated surface waters steeply declining at shallow depth. The highest DAA concentrations were observed close to the surface also, but attenuation of DAA concentration over depth was less pronounced. Compositional changes of DCCHO were strongest within more oxygenated waters. Compositional changes of DAA were also evident under suboxic conditions (〈5 µmol O2 kg−1) and indicated bacterial peptide degradation. Moreover, specific free amino acids (alanine and threonine) were enhanced within suboxic waters, pointing to a potential production of dissolved organic nitrogen under suboxic conditions. Our results therewith suggest that deoxygenation supports a spatial decoupling of DCCHO and DAA production and degradation dynamics and give new insights to carbon and nitrogen cycling in the OMZ off Peru.
    Description: Plain Language Summary: The molecular composition of dissolved organic matter (DOM) in seawater mainly depends on production and consumption processes by plankton organisms. The biological consumption of DOM reduces the amount of oxygen in seawater, but little is known about the composition of DOM in so‐called oxygen minimum zones (OMZs). We studied the distribution of DOM, specifically of dissolved sugars and amino acids in the OMZ off Peru. We observed that the reworking and degradation of sugars and amino acids differed between more and less oxygenated waters. We also found indications for the production of specific amino acids within the OMZ. Our study therewith suggests, that oxygen concentrations affect dissolved amino acid and sugar dynamics and may help to better understand carbon and nitrogen cycling within OMZs.
    Description: Key Points: Decoupling of dissolved combined carbohydrates and dissolved amino acids dynamics, in the oxygen minimum zone off Peru. Free amino acids indicate production of dissolved organic nitrogen within suboxic waters.
    Description: Hemholtz Association
    Description: German Science Foundation
    Keywords: 551.46 ; amino acids ; bacteria ; carbohydrates ; dissolved organic carbon ; oxygen minimum zone ; Pacific Ocean
    Type: map
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 2
    Publication Date: 2021-12-01
    Description: The duration and magnitude of the North Atlantic spring bloom impacts both higher trophic levels and oceanic carbon sequestration. Nutrient exhaustion offers a general explanation for bloom termination, but detail on which nutrients and their relative influence on phytoplankton productivity, community structure, and physiology is lacking. Here, we address this using nutrient addition bioassay experiments conducted across the midlatitude North Atlantic in June 2017 (late spring). In four out of six experiments, phytoplankton accumulated over 48–72 h following individual additions of either iron (Fe) or nitrogen (N). In the remaining two experiments, Fe and N were serially limiting, that is, their combined addition sequentially enhanced phytoplankton accumulation. Silicic acid (Si) added in combination with N + Fe led to further chlorophyll a (Chl a) enhancement at two sites. Conversely, addition of zinc, manganese, cobalt, vitamin B12, or phosphate in combination with N + Fe did not. At two sites, the simultaneous supply of all six nutrients, in combination with N + Fe, also led to no further Chl a enhancement, but did result in an additional 30–60% particulate carbon accumulation. This particulate carbon accumulation was not matched by a Redfield equivalent of particulate N, characteristic of high C:N organic exudates that enhance cell aggregation and sinking. Our results suggest that growth rates of larger phytoplankton were primarily limited by Fe and/or N, making the availability of these nutrients the main bottom-up factors contributing to spring bloom termination. In addition, the simultaneous availability of other nutrients could modify bloom characteristics and carbon export efficiency.
    Keywords: 577.7 ; mid-latitude North Atlantic ; phytoplankton ; diatom blooming ; experiments
    Language: English
    Type: map
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...