2013
DOI: 10.1007/s00027-013-0301-z
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Viriobenthos in aquatic sediments: variability in abundance and production and impact on the C-cycle

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Cited by 16 publications
(18 citation statements)
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“…In these environments, viral abundances have previously been reported to range from 10 7 to 10 10 VLP g −1 of dry sediment, being 10-1000 times higher than viral abundances in the water column (Danovaro et al, 2008a). Viral numbers in sediments, with pore water included, between 10 4 and 10 11 VLP ml −1 have been reported (Duhamel & Jacquet, 2006;Pinto et al, 2013). Similar general trends as in water columns can also be observed in the viriobenthos.…”
Section: (A) Benthossupporting
confidence: 72%
See 1 more Smart Citation
“…In these environments, viral abundances have previously been reported to range from 10 7 to 10 10 VLP g −1 of dry sediment, being 10-1000 times higher than viral abundances in the water column (Danovaro et al, 2008a). Viral numbers in sediments, with pore water included, between 10 4 and 10 11 VLP ml −1 have been reported (Duhamel & Jacquet, 2006;Pinto et al, 2013). Similar general trends as in water columns can also be observed in the viriobenthos.…”
Section: (A) Benthossupporting
confidence: 72%
“…Consequently, it has been posited that declines in VBR are due to viral loss, for example by non-specific adsorption to particles (Maranger & Bird, 1995) or degradation after adsorption to humic substances (Anesio et al, 2004). Inversely, high VBR values have been attributed to high viral production Kellogg, 2010;Yoshida-Takashima et al, 2012;Pinto, Larsen & Casper, 2013;Engelhardt et al, 2014;Parvathi et al, 2014) or low viral decay (Mei & Danovaro, 2004;Danovaro et al, 2005;Williamson et al, 2007;Winter, Kerros & Weinbauer, 2009;Maurice et al, 2010;De Corte et al, 2012), which in some cases (e.g. in soil and sediments) could be an artifact of extraction procedures (Middelboe, Glud & Finster, 2003;Williamson, Radosevich & Wommack, 2005;Kimura et al, 2008;Williamson, 2011).…”
Section: Introduction: the Virus-to-prokaryote Ratio -Definition Amentioning
confidence: 97%
“…In shallow estuarine ecosystems, hydrodynamics (tide, waves, wind) induce erosion of particulate material from the sediments into the overlying water column and at the sedimentwater interface, the gradients in organic and inorganic nutrients may structure the composition of the microbial communities and their activities (Seymour et al, 2007). Differences in grain size distribution may explain the distribution of dissolved and particulate matter according to the porosity and permeability of the sediment (Pinto et al, 2013). The smaller pore size and higher surface area in clays and silts compared to sand may infer a higher dissolved nutrients in clayed sediment and a higher desorption of organic particles in sandy sediment (Wainright, 1987).…”
Section: Introductionmentioning
confidence: 99%
“…Across six studies in benthic sediments, for example, virus‐caused mortality of prokaryotes released between 0.1% and 10% of the organic carbon supporting heterotrophic bacteria (Pinto et al. ). Pathogenic carbon consumption by the fungus Rhytisma polare reduced ecosystem carbon by 20% in Arctic tundra (Masumoto et al.…”
Section: Introductionmentioning
confidence: 99%