1989
DOI: 10.1016/0198-0149(89)90147-7
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Suspended particle and bacterial maxima in Peruvian coastal waters during a cold water anomaly

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Cited by 55 publications
(33 citation statements)
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“…Bulk seawater counts declined from~6 × 10 5 per ml in the primary chlorophyll maximum and upper oxycline to 1.3 × 10 5 at the oxic-nitrite interface (90 m), before increasing to a maximum of 1.4 × 10 6 at the OMZ core. This pattern agrees with trends from other OMZ sites, where particulate backscattering and bacterial load show local maxima in the photic zone and again in the OMZ (Spinrad et al, 1989;Naqvi et al, 1993;Whitmire et al, 2009). At all depths, gene numbers were substantially higher in the 0.2-1.6 μm (FL) fraction compared with the 1.6-30 μm (PA) fraction, with FL/PA ratios from 8 to 15 (Figure 1f).…”
Section: Oxygen and Nitrogensupporting
confidence: 78%
“…Bulk seawater counts declined from~6 × 10 5 per ml in the primary chlorophyll maximum and upper oxycline to 1.3 × 10 5 at the oxic-nitrite interface (90 m), before increasing to a maximum of 1.4 × 10 6 at the OMZ core. This pattern agrees with trends from other OMZ sites, where particulate backscattering and bacterial load show local maxima in the photic zone and again in the OMZ (Spinrad et al, 1989;Naqvi et al, 1993;Whitmire et al, 2009). At all depths, gene numbers were substantially higher in the 0.2-1.6 μm (FL) fraction compared with the 1.6-30 μm (PA) fraction, with FL/PA ratios from 8 to 15 (Figure 1f).…”
Section: Oxygen and Nitrogensupporting
confidence: 78%
“…There is only limited direct evidence bearing on this question. Recently, Spinrad et al (1989) found in mesocosm studies that changes in bacterial abundance could contribute significantly to the variability in the diffuse attenuation coefficient of seawater. Also, we note a striking similarity (Fig.…”
Section: Discussionmentioning
confidence: 99%
“…Because of these widespread suboxic and anoxic conditions, very high accumulations of nitrous oxide and hydrogen sulfide occur in this region (Naqvi et al 2000). Denitrifying zones in the subsurface hypoxic layers of the Eastern Tropical Pacific Ocean and the Arabian Sea are recognized by their secondary nitrite maxima (SNM), which also have high bacterial abundances (Spinrad et al 1989, Ward et al 1998. The depth of the SNM is highly correlated with the depth of the particle maxima in oxygen minimum zones of these regions (Naqvi et al 1993).…”
Section: Development Of Denitrification In the Study Areamentioning
confidence: 99%