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  • Hydrothermal vents  (1)
  • Molecular iodine  (1)
  • 1
    Publication Date: 2022-05-25
    Description: Author Posting. © National Shellfisheries Association, 2008. This article is posted here by permission of National Shellfisheries Association for personal use, not for redistribution. The definitive version was published in Journal of Shellfish Research 27 (2008): 177-190, doi:10.2983/0730-8000(2008)27[177:IBVFCT]2.0.CO;2.
    Description: In April 1991, submarine volcanic eruptions initiated the formation of numerous hydrothermal vents between 9°45′ and 9°52′N along the crest of the East Pacific Rise (EPR). Dramatic changes in biological community structure and vent fluid chemistry have been documented throughout this region since the eruptive event. By April 2004, mussels (Bathymodiolus thermophilus) dominated the faunal assemblages at several of the vent sites formed during of after the 1991 eruptions, whereas other habitats within the region were dominated by the vestimentiferan Riftia pachyptila. In the present paper, we build upon the extensive data sets obtained at these sites over the past decade and describe a manipulative experiment (conducted at 9°49.94′N; 104°14.43′W on the EPR) designed to assess interrelationships between vent fluid chemistry, temperature, biological community structure, and seismic activity. To this end, in situ voltammetric systems and thermal probes were used to measure H2S/HS− and temperature over time in a denuded region of an extensive mussel bed in which an exclusion cage was placed to inhibit the subsequent migration of mussels into the denuded area. Fluid samples were taken from the same locations to characterize the associated microbial constituents. Basalt blocks, which were placed in the cage in April 2004 and subsequently recovered in April 2005, were colonized by more than 25 different species of invertebrates, including numerous vestimentiferans and remarkably few mussels. Recorded temporal changes in vent fluid chemistry and temperature regimes, when coupled with microbiological characterization of the vent fluids and seismic activity data obtained from ocean bottom seismometers, shed considerable light on factors controlling biological community structure in these hydrothermal ecosystems.
    Description: Supported by NSF Grants OCE-9529819, ESI-0087679 (RAL), OCE-0327353 (RAL and CV), OCE-0327261, OCE-0451983 (TS), MCB-0456676, CHE-0221978 (CV), OCE-0326434 (GWL), and OCE-0327283 (MT), the Deep Ocean Exploration Institute at the Woods Hole Oceanographic Institution, and the New Jersey Agricultural Experiment Station at Rutgers University.
    Keywords: Hydrothermal vents ; Seismicity ; Voltammetry ; Vent chemistry ; Mussels
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
    Location Call Number Limitation Availability
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  • 2
    Electronic Resource
    Electronic Resource
    Springer
    Aquatic geochemistry 1 (1995), S. 89-104 
    ISSN: 1573-1421
    Keywords: Molecular iodine ; iodination kinetics ; iodine speciation ; organic iodine
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Geosciences
    Notes: Abstract The reactivity of 2 µM molecular iodine in seawater toward various organic compounds containing aromatic, α-keto, amino, olefinic and sugar functional groups was investigated. More detailed studies have been made of the reduction kinetics with salicylic acid, α-ketoglutaric acid and the polypeptide oxidized glutathione, particularly to establish whether variation over the pH range 4–9 would provide a similar reduction reactivity or “fingerprint” to that of molecular iodine added to natural seawater. The data indicates that compounds with only one functional group react with first order kinetics whereas compounds with multiple functional groups show more complex behaviour. Kinetic and thermodynamic modelling indicates that HOI is the main iodine species reacting with organic matter at seawater pH of 8.2. Based on the pH “fingerprints”, peptides and compounds containing carbonyl or α-keto groups are the key reductants of molecular iodine added to seawater. These compounds form C-I and N-I bonds which can allow for a rich organic iodine chemistry in seawater. The model compound results are discussed in relation to oceanic processes.
    Type of Medium: Electronic Resource
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