scholarly journals Bacterial and fungal colonization and decomposition of submerged plant litter: consequences for biogenic silica dissolution

2016 ◽  
Vol 92 (3) ◽  
pp. fiw011 ◽  
Author(s):  
Hanna Alfredsson ◽  
Wim Clymans ◽  
Johanna Stadmark ◽  
Daniel Conley ◽  
Johannes Rousk
2007 ◽  
Vol 106 (1-2) ◽  
pp. 223-238 ◽  
Author(s):  
K. Khalil ◽  
C. Rabouille ◽  
M. Gallinari ◽  
K. Soetaert ◽  
D.J. DeMaster ◽  
...  

2006 ◽  
Vol 72 (1) ◽  
pp. 596-605 ◽  
Author(s):  
Nanna Buesing ◽  
Mark O. Gessner

ABSTRACT Heterotrophic bacteria and fungi are widely recognized as crucial mediators of carbon, nutrient, and energy flow in ecosystems, yet information on their total annual production in benthic habitats is lacking. To assess the significance of annual microbial production in a structurally complex system, we measured production rates of bacteria and fungi over an annual cycle in four aerobic habitats of a littoral freshwater marsh. Production rates of fungi in plant litter were substantial (0.2 to 2.4 mg C g−1 C) but were clearly outweighed by those of bacteria (2.6 to 18.8 mg C g−1 C) throughout the year. This indicates that bacteria represent the most actively growing microorganisms on marsh plant litter in submerged conditions, a finding that contrasts strikingly with results from both standing dead shoots of marsh plants and submerged plant litter decaying in streams. Concomitant measurements of microbial respiration (1.5 to 15.3 mg C-CO2 g−1 of plant litter C day−1) point to high microbial growth efficiencies on the plant litter, averaging 45.5%. The submerged plant litter layer together with the thin aerobic sediment layer underneath (average depth of 5 mm) contributed the bulk of microbial production per square meter of marsh surface (99%), whereas bacterial production in the marsh water column and epiphytic biofilms was negligible. The magnitude of the combined production in these compartments (∼1,490 g C m−2 year−1) highlights the importance of carbon flows through microbial biomass, to the extent that even massive primary productivity of the marsh plants (603 g C m−2 year−1) and subsidiary carbon sources (∼330 g C m−2 year−1) were insufficient to meet the microbial carbon demand. These findings suggest that littoral freshwater marshes are genuine hot spots of aerobic microbial carbon transformations, which may act as net organic carbon importers from adjacent systems and, in turn, emit large amounts of CO2 (here, ∼870 g C m−2 year−1) into the atmosphere.


2007 ◽  
Vol 333 ◽  
pp. 129-142 ◽  
Author(s):  
B Moriceau ◽  
M Garvey ◽  
O Ragueneau ◽  
U Passow

2020 ◽  
Author(s):  
Shahab Varkouhi ◽  
Jonathan Wells

Abstract. This study calculated the dissolution rates of biogenic silica deposited on the seafloor and the silicic acid benthic flux for 22 Ocean Drilling Program sites. Simple models developed for two host sediment types – detrital and carbonate – were used to explain the variability of biogenic opal dissolution and recycling under present-day low (−0.3 to 2.14 °C) bottom-water temperatures. The kinetic constants describing silicic acid release and silica saturation concentration increased systematically with increasing bottom-water temperatures. When these temperature effects were incorporated into the diagenetic models, the prediction of dissolution rates and diffusive fluxes was more robust. This demonstrates that temperature acts as a primary control that decreases the relative degree of pore-water saturation with opal while increasing the silica concentration. The correlation between the dissolution rate and benthic flux with temperature was pronounced at sites where biogenic opal is accommodated in surficial sediments mostly comprised of biogenic carbonates. This is because the dissolution of carbonates provides the alkalinity necessary for both silica dissolution and clay formation; thus strongly reducing the retarding influence of clays on opal dissolution. Conversely, the silica exchange rates were modified by presence of aluminosilicates, which led to a higher burial efficiency for opal in detrital- than in carbonate-dominated benthic layers. Though model prediction of first-order silica early transformation suggests likely effects from surface temperatures (0–4 °C) on opal-CT precipitation over short geological times (


1992 ◽  
Vol 37 (3) ◽  
pp. 361-378 ◽  
Author(s):  
Jean-Jacques Pichon ◽  
Gilles Bareille ◽  
Monique Labracherie ◽  
Laurent D. Labeyrie ◽  
Annick Baudrimont ◽  
...  

AbstractA transfer function has been established to quantify the dissolution of diatom silica in Southern Ocean sediments. The relationship between the amount of silica dissolution and changes in diatom species distribution is built by controlled progressive dissolution of biogenic silica in five recent sediment samples from box-core tops, each representative of a modern diatom species sediment assemblage. The amount of dissolved silica was measured for each experiment. The resulting data set of species abundances (42 samples containing 32 diatom species and 2 silicoflagellate genera) was added to the modern data base of diatom species distributed over the Southern Ocean (124 core tops). Q-mode factor analysis individualizes four factors explaining 83% of the variance. The first three factors are controlled by surface water properties (mostly temperature). The fourth factor is the only one correlated with loss of silica in the reference samples (R = 0.900). We quantified the dissolution factor using this correlation: superficial sediments of the Southeast Indian Ocean are characterized, from low to high latitudes, by a decrease in silica loss by dissolution (from >50 to 10%) from the Subantarctic Zone (40°S) to around 55°S, followed by an increase of silica loss to values larger than 60% between 63° and 68°S. Application of the dissolution factor in two cores from the Southern Ocean (≈44° and 55°S) shows enhanced opal dissolution during the last glaciation, particularly during Emiliani's stage 3 (from 40,000 to 30,000 yr B.P.).


2015 ◽  
Vol 120 ◽  
pp. 169-177 ◽  
Author(s):  
Giuliano Bonanomi ◽  
Mauro Senatore ◽  
Antonello Migliozzi ◽  
Anna De Marco ◽  
Antonella Pintimalli ◽  
...  

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