Loading…
The suspended small-particle layer in the oxygen-poor Black Sea: a proxy for delineating the effective N 2 -yielding section
The shallower oxygen-poor water masses of the ocean confine a majority of the microbial communities that can produce up to 90 % of oceanic N2. This effective N2-yielding section encloses a suspended small-particle layer, inferred from particle backscattering (bbp) measurements. It is thus hypothesiz...
Saved in:
Published in: | Biogeosciences 2020-12, Vol.17 (24), p.6491-6505 |
---|---|
Main Authors: | , , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Get full text |
Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
Summary: | The shallower oxygen-poor water masses of the ocean confine a majority of the microbial communities that can produce up to 90 % of
oceanic N2. This effective N2-yielding section encloses a
suspended small-particle layer, inferred from particle backscattering
(bbp) measurements. It is thus hypothesized that this layer (hereafter,
the bbp-layer) is linked to microbial communities involved in
N2 yielding such as nitrate-reducing SAR11 as well as sulfur-oxidizing, anammox, and denitrifying bacteria – a hypothesis yet to be evaluated. Here, data collected by three BGC-Argo floats deployed in the Black Sea are used to investigate the origin of this bbp-layer. To this end,
we evaluate how the key drivers of N2-yielding bacteria dynamics impact
the vertical distribution of bbp and the thickness of the bbp-layer. In conjunction with published data on N2 excess, our results
suggest that the bbp-layer is at least partially composed of the bacteria
driving N2 yielding for three main reasons: (1) strong correlations are
recorded between bbp and nitrate; (2) the top location of the
bbp-layer is driven by the ventilation of oxygen-rich subsurface waters, while
its thickness is modulated by the amount of nitrate available to produce
N2; and (3) the maxima of both bbp and N2 excess coincide at the same isopycnals where bacteria involved in N2 yielding coexist. We thus
advance that bbp and O2 can be exploited as a combined proxy to
delineate the N2-yielding section of the Black Sea. This proxy can
potentially contribute to refining delineation of the effective
N2-yielding section of oxygen-deficient zones via data from the growing
BGC-Argo float network. |
---|---|
ISSN: | 1726-4189 1726-4170 1726-4189 |
DOI: | 10.5194/bg-17-6491-2020 |