Sulfide production and consumption in degrading wood in the marine environment

2013-01-01
Yücel, Mustafa
Fagervold, Sonja K.
CONTREİRA-PEREİRA, Leonardo
LE BRİS, Nadine
Woody debris is known to be transported to the seas and accumulate on the seafloor, however, little is known on the consequences of its degradation in the marine environment. In this study we monitored the degradation product sulfide with Au/Hg voltammetric microelectrodes on the surface and interior of an experimentally immersed wood for 200 d. After 5 weeks of immersion, the interior became sulfidic, and steady-state conditions were established after 13 weeks with sulfide concentration reaching about 300 mu M. Although sulfide was briefly detected at the surface of wood, its concentration remained lower than 20 mu M, indicating that this compound was effectively oxidized within the substrate. Fitting these data to a kinetic model lead to an estimated microbial sulfide production rate in the range of 19-28 mu M d(-1) at steady state. As much as 24 mu M d(-1) nitrate could be consumed by this process in the steady-state period. Before the establishment of the steady state conditions, steep fluctuations in sulfide concentration (between 1 mM and several mu M) were observed in the wood interior. This study is the first to document the temporal dynamics of this unsteady process, characterized by fast sulfide fluctuation and consumption. Our results point to the complex mechanisms driving the dynamics of wood biogeochemical transformations, and reveal the capacity of woody debris to generate sulfidic conditions and act as a possible sink for oxygen and nitrate in the marine environment.

Suggestions

Sulfide Oxidation across Diffuse Flow Zones of Hydrothermal Vents
Gartman, Amy; Yücel, Mustafa; Madison, Andrew S.; Chu, David W.; MA, Shufen; Janzen, Christopher P.; Becker, Erin L.; Beinart, Roxanne A.; Girguis, Peter R.; Luther, George W. (2011-09-01)
The sulfide (H(2)S/HS(-)) that is emitted from hydrothermal vents begins to oxidize abiotically with oxygen upon contact with ambient bottom water, but the reaction kinetics are slow. Here, using in situ voltammetry, we report detection of the intermediate sulfur oxidation products polysulfides [S(x)(2-)] and thiosulfate [S(2)O(3)(2-)], along with contextual data on sulfide, oxygen, and temperature. At Lau Basin in 2006, thiosulfate was identified in less than one percent of approximately 10,500 scans and n...
Microbial Sulfide Filter along a Benthic Redox Gradient in the Eastern Gotland Basin, Baltic Sea
Yücel, Mustafa; Dale, Andrew W.; PFANNKUCHE, Olaf (2017-02-09)
The sediment-water interface is an important site for material exchange in marine systems and harbor unique microbial habitats. The flux of nutrients, metals, and greenhouse gases at this interface may be severely dampened by the activity of microorganisms and abiotic redox processes, leading to the "benthic filter" concept. In this study, we investigate the spatial variability, mechanisms and quantitative importance of a microbially-dominated benthic filter for dissolved sulfide in the Eastern Gotland Basi...
Heavy Metal Contamination Analysis of Bottom Sediments of Köycegiz Lake and Fethiye-Göcek Bay, SW Turkey
Gülşen Rothmund, Halil; Avşar, Özgür; Avşar, Ulaş; Kurtuluş, Bedri; Tunca, Evren (null; 2018-04-13)
In this study, the heavy metal contamination in the base sediments of Köyceğiz Lake and Fethiye-Göcek Bay in Muğla, Turkey was assessed. The focus lies mainly on Mo, Cu, Pb, Zn, Ni, Co, Mn, Fe, As, Cr and Al metals. The applied analysis methods on the data set of 150 sediment samples (81 samples in Köyceğiz Lake and 69 samples in Fethiye-Göcek Bay) are the following: contamination analyses (contamination factor, contamination degree, modified contamination degree, enrichment factor, geo-accumulation index, ...
Lİthofacies and biofacies characteristics of Lower Carboniferous carbonates in Central Taurides, TURKEY
Özdemir, Ayşe; Altıner, Demir; Altıner, Sevinç (2019-09-09)
The studied successions in the Central Taurides were mainly deposited in a shallow marine environment during the Early Carboniferous time. Conodonts are one of the most important microfossil groups for the Lower Carboniferous biostratigraphy. The measured sections are not rich in conodonts but important species including those of the Lower Carboniferous boundary conodonts. The conodont elements recorded in this study include Gnathodus cuneiformis, Gnathodus girtyi girtyi, Gnathodus girtyi simplex, Kladognat...
Spatial and temporal variability in the chemical properties of the oxic and suboxic layers of the Black Sea
Tuğrul, Süleyman; Murray, James W.; Friederich, Gernot E.; Salihoglu, Ilkay (Elsevier BV, 2014-07-01)
The Black Sea, a land-locked deep basin with sulfide bearing waters below 150-200 m, has been subject to anthropogenic pressures since the 1970s. Large inputs of nutrients (nitrate - N, phosphate - P, silicate - Si) with high N/P but low Si/N ratios and subsequent development of intensive eutrophication over the basin have changed vertical distributions and inventories of nutrients and redox-sensitive metals in the oxic, suboxic and anoxic layers. Chemical data sets obtained between 1988 and 2010, and older...
Citation Formats
M. Yücel, S. K. Fagervold, L. CONTREİRA-PEREİRA, and N. LE BRİS, “Sulfide production and consumption in degrading wood in the marine environment,” CHEMOSPHERE, pp. 403–409, 2013, Accessed: 00, 2020. [Online]. Available: https://hdl.handle.net/11511/32160.