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  • 92-597B; 92-597C; Aluminium oxide; Atomic emission spectroscopy (AES); Barium; Boron; Calcium oxide; Chromium; Cobalt; Copper; Deep Sea Drilling Project; Description; DRILL; Drilling/drill rig; DSDP; Event label; Gallium; Glomar Challenger; Iron oxide, Fe2O3; Leg92; Lithium; Magnesium oxide; Manganese oxide; Nickel; Phosphorus pentoxide; Potassium oxide; Rubidium; Sample code/label; Scandium; Silicon dioxide; Sodium oxide; South Pacific; Spectrophotometry; Strontium; Titanium dioxide; Total; Vanadium; Yttrium; Zinc  (1)
  • Hydrothermal vents  (1)
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Keywords
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Years
  • 1
    Publication Date: 2023-06-27
    Keywords: 92-597B; 92-597C; Aluminium oxide; Atomic emission spectroscopy (AES); Barium; Boron; Calcium oxide; Chromium; Cobalt; Copper; Deep Sea Drilling Project; Description; DRILL; Drilling/drill rig; DSDP; Event label; Gallium; Glomar Challenger; Iron oxide, Fe2O3; Leg92; Lithium; Magnesium oxide; Manganese oxide; Nickel; Phosphorus pentoxide; Potassium oxide; Rubidium; Sample code/label; Scandium; Silicon dioxide; Sodium oxide; South Pacific; Spectrophotometry; Strontium; Titanium dioxide; Total; Vanadium; Yttrium; Zinc
    Type: Dataset
    Format: text/tab-separated-values, 353 data points
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2022-05-25
    Description: © The Author(s), 2015. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Frontiers in Microbiology 6 (2015): 901, doi:10.3389/fmicb.2015.00901.
    Description: Many deep-sea hydrothermal vent systems are regularly impacted by volcanic eruptions, leaving fresh basalt where abundant animal and microbial communities once thrived. After an eruption, microbial biofilms are often the first visible evidence of biotic re-colonization. The present study is the first to investigate microbial colonization of newly exposed basalt surfaces in the context of vent fluid chemistry over an extended period of time (4–293 days) by deploying basalt blocks within an established diffuse-flow vent at the 9°50′ N vent field on the East Pacific Rise. Additionally, samples obtained after a recent eruption at the same vent field allowed for comparison between experimental results and those from natural microbial re-colonization. Over 9 months, the community changed from being composed almost exclusively of Epsilonproteobacteria to a more diverse assemblage, corresponding with a potential expansion of metabolic capabilities. The process of biofilm formation appears to generate similar surface-associated communities within and across sites by selecting for a subset of fluid-associated microbes, via species sorting. Furthermore, the high incidence of shared operational taxonomic units over time and across different vent sites suggests that the microbial communities colonizing new surfaces at diffuse-flow vent sites might follow a predictable successional pattern.
    Description: This work was partly supported by grants from the US National Science Foundation to SS (OCE-0452333, 1136727), to TS (OCE-0117117, 0525907, 0961186, 1043064, 0327261, 1131620), to WS and KD (1434798), as well as a grant by the WHOI Deep Ocean Exploration Institute to SB, TS, and SS.
    Keywords: Hydrothermal vents ; Colonization ; Species sorting ; Settlement ; Volcanic eruption ; 16S rRNA ; Epsilonproteobacteria ; Disturbance
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
    Location Call Number Limitation Availability
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