scholarly journals Tracking redox reactions in Saanich Inlet from the water column to early diagenetic pyrite formation

2021 ◽  
Author(s):  
Maria Figueroa ◽  
Daniel Gregory ◽  
Ravi Kukkadapu ◽  
Timothy Lyons
2005 ◽  
Vol 2 (4) ◽  
pp. 331-362
Author(s):  
I. A. Seeberg-Elverfeldt ◽  
C. B. Lange ◽  
J. Pätzold ◽  
G. Kuhn

Abstract. Laminated sediments in the Shaban Deep, a brine-filled basin in the northern Red Sea, were analyzed with backscattered electron imagery. Here we present possible mechanisms involved in the formation of laminae of various types and homogenous intervals arising from the detailed investigation of multicore GeoB 7805-1 (26 13.9' N and 35 22.6' E; water depth 1447 m) and gravity core GeoB 5836-2 (26 12.61' N, 35 21.56' E; water depth 1475 m). Sediment makeup includes six types: a) a laminated structure with alternating light (mainly coccoliths) and dark (diatom frustules) layers, where the diatom component is indicative of the intra-annual variability between stratification and mixing events; b) a pocket-like structure attributed to the sinking of particles within fecal pellets and aggregates; c) a matrix of tightly packed diatoms that relates to extended stratification/mixing periods of the water column; d) homogenous intervals that result from turbidity deposition; e) silt accumulations which origin may lie in agglutinated foraminifers; and f) pyrite layers with pyrite formation initiated at the seawater-brine interface.


2017 ◽  
Vol 4 (1) ◽  
Author(s):  
Alyse K. Hawley ◽  
Mónica Torres-Beltrán ◽  
Elena Zaikova ◽  
David A. Walsh ◽  
Andreas Mueller ◽  
...  

2019 ◽  
Vol 6 (1) ◽  
Author(s):  
Mónica Torres-Beltrán ◽  
Alyse K. Hawley ◽  
David Capelle ◽  
Elena Zaikova ◽  
David A. Walsh ◽  
...  
Keyword(s):  

2019 ◽  
Vol 98 ◽  
pp. 11004
Author(s):  
Alfonso Menchén ◽  
Nicolas Valiente ◽  
Beatriz Toledo ◽  
Juan José Gómez-Alday

Biogeochemical cycling involves the exchange of electrons between chemical species through redox reactions. Microorganisms can utilize energy released by redox reactions for their metabolism following a thermodynamic sequence. Among these reactions, the dissimilatory reduction of sulfate (SO42−) to produce hydrogen sulfide (H2S) is one of the most important microbially-mediated pathways. The use of microelectrodes at the water-sediment interface provided a better understanding of sulfate reduction processes in the suboxic and anoxic zones. The goal of this study was to assess the microzonation of H2S and O2 under different conditions of light and oxygen in the water column. For this purpose, organic-rich lacustrine sediments from Pétrola Lake (SE Spain) were used. Sediment incubations were performed in mesocosm devices. The highest production of H2S (up to 0.36 nmol/cm-3s-1) was observed under anoxic and dark conditions. Production under those conditions was several orders of magnitude higher than those measured when oxygen was present in the water column. Furthermore, the absence of O2 in the water column significantly altered the microzonation of H2S in depth. The absence of light seems not to affect the dynamics of O2 and H2S in depth. The study contributes to our understanding of microzonation in organic-rich sediments.


2009 ◽  
Vol 4 (4) ◽  
pp. 558-566 ◽  
Author(s):  
Alexandra Demiri ◽  
Alexandra Meziti ◽  
Sokratis Papaspyrou ◽  
Maria Thessalou-Legaki ◽  
Konstantinos Kormas

AbstractWe investigated the diversity of the bacterial 16S rRNA genes occurring on the abdominal setal tufts and in the emptied midgut of the marine mudshrimp Pestarella tyrrhena (Decapoda: Thalassinidea). There were no dominant phylotypes on the setal tufts. The majority of the phylotypes belonged to the phylum Bacteroidetes, frequently occurring in the water column. The rest of the phylotypes were related to anoxygenic photosynthetic α-Proteobacteria and to Actinobacteria. This bacterial profile seems more of a marine assemblage rather than a specific one suggesting that no specific microbial process can be inferred on the setal tufts. In the emptied midgut, 64 clones were attributed to 16 unique phylotypes with the majority (40.6%) belonging to the γ-Proteobacteria, specifically to the genus Vibrio, a marine group with known symbionts of decapods. The next most abundant group was the ɛ-Proteobacteria (28.1%), with members as likely symbionts related to the processes involving redox reactions occurring in the midgut. In addition, phylotypes related to the Spirochaetes (10.9%) were also present, with relatives capable of symbiosis conducting a nitrite associated metabolism. Entomoplasmatales, Bacteroidetes and Actinobacteria related phylotypes were also found. These results indicate a specific bacterial community dominated by putative symbiotic Bacteria within the P. tyrrhena’s midgut.


Ocean Science ◽  
2005 ◽  
Vol 1 (2) ◽  
pp. 113-126 ◽  
Author(s):  
I. A. Seeberg-Elverfeldt ◽  
C. B. Lange ◽  
J. Pätzold ◽  
G. Kuhn

Abstract. Laminated sediments in the Shaban Deep, a brine-filled basin in the northern Red Sea, were analyzed with backscattered electron imagery. Here we present possible mechanisms involved in the formation of laminae of various types and homogenous intervals arising from the detailed investigation of multicore GeoB 7805-1 (26°13.9' N and 35°22.6' E; water depth 1447 m) and gravity core GeoB 5836-2 (26°12.61' N, 35°21.56' E; water depth 1475 m). Sediment makeup includes six types: a) a laminated structure with alternating light (mainly coccoliths) and dark (diatom frustules) layers, where the diatom component is indicative of the intra-annual variability between stratification and mixing events; b) a pocket-like structure attributed to the sinking of particles within fecal pellets and aggregates; c) a matrix of tightly packed diatoms that relates to extended stratification/mixing periods of the water column; d) homogenous intervals that result from turbidity deposition; e) silt accumulations which origin may lie in agglutinated foraminifers; and f) pyrite layers with pyrite formation initiated at the seawater-brine interface.


2017 ◽  
Vol 4 (1) ◽  
Author(s):  
Mónica Torres-Beltrán ◽  
Alyse K. Hawley ◽  
David Capelle ◽  
Elena Zaikova ◽  
David A. Walsh ◽  
...  
Keyword(s):  

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