GLORIA

GEOMAR Library Ocean Research Information Access

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
  • Adaptive divergence  (1)
  • DERIDGE; From Mantle to Ocean: Energy-, Material- and Life-cycles at Spreading Axes; M64/1; M64/1-114-ROV; M64/1-123-ROV; M64/1-124-GTV; M64/1-125-ROV; M64/1-130-ROV; M64/1-139-GTV; M64/1-141-ROV; M64/1-146-ROV; M68/1; M68/1-03-ROV; M68/1-07-ROV; M68/1-12-ROV; M68/1-20-ROV; MARSUED2; MARSUED3; Mephisto; Meteor (1986); Mid-Atlantic Ridge at 4-11°S; MULT; Multiple investigations; Remote operated vehicle; ROV; Shrimp_Farm; Sister_Peak; Tannenbaum; Television-Grab; TVG; Two_Boats  (1)
Document type
Keywords
Publisher
Years
  • 1
    Publication Date: 2024-02-02
    Description: The effect of volcanic activity on submarine hydrothermal systems has been well documented along fast- and intermediate-spreading centers but not from slow-spreading ridges. Indeed, volcanic eruptions are expected to be rare on slow-spreading axes. Here we report the presence of hydrothermal venting associated with extremely fresh lava flows at an elevated, apparently magmatically robust segment center on the slow-spreading southern Mid-Atlantic Ridge near 5°S. Three high-temperature vent fields have been recognized so far over a strike length of less than 2 km with two fields venting phase-separated, vapor-type fluids. Exit temperatures at one of the fields reach up to 407°C, at conditions of the critical point of seawater, the highest temperatures ever recorded from the seafloor. Fluid and vent field characteristics show a large variability between the vent fields, a variation that is not expected within such a limited area. We conclude from mineralogical investigations of hydrothermal precipitates that vent-fluid compositions have evolved recently from relatively oxidizing to more reducing conditions, a shift that could also be related to renewed magmatic activity in the area. Current high exit temperatures, reducing conditions, low silica contents, and high hydrogen contents in the fluids of two vent sites are consistent with a shallow magmatic source, probably related to a young volcanic eruption event nearby, in which basaltic magma is actively crystallizing. This is the first reported evidence for direct magmatic-hydrothermal interaction on a slow-spreading mid-ocean ridge.
    Keywords: DERIDGE; From Mantle to Ocean: Energy-, Material- and Life-cycles at Spreading Axes; M64/1; M64/1-114-ROV; M64/1-123-ROV; M64/1-124-GTV; M64/1-125-ROV; M64/1-130-ROV; M64/1-139-GTV; M64/1-141-ROV; M64/1-146-ROV; M68/1; M68/1-03-ROV; M68/1-07-ROV; M68/1-12-ROV; M68/1-20-ROV; MARSUED2; MARSUED3; Mephisto; Meteor (1986); Mid-Atlantic Ridge at 4-11°S; MULT; Multiple investigations; Remote operated vehicle; ROV; Shrimp_Farm; Sister_Peak; Tannenbaum; Television-Grab; TVG; Two_Boats
    Type: Dataset
    Format: application/zip, 3 datasets
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 2
    Publication Date: 2022-05-26
    Description: Author Posting. © The Author(s), 2015. This is the author's version of the work. It is posted here by permission of The Royal Society for personal use, not for redistribution. The definitive version was published in Proceedings of the Royal Society B: Biological Sciences 282 (2015): 20150008, doi:10.1098/rspb.2015.0008.
    Description: The depth-differentiation hypothesis proposes that the bathyal region is a source of genetic diversity and an area where there is a high rate of species formation. Genetic differentiation should thus occur over relatively small vertical distances, particularly along the upper continental slope (200-1000 m) where oceanography varies greatly over small differences in depth. To test whether genetic differentiation within deepwater octocorals is greater over vertical rather than geographic distances, Callogorgia delta was targeted. This species commonly occurs throughout the northern Gulf of Mexico at depths ranging from 400-900 m. We found significant genetic differentiation (FST=0.042) across seven sites spanning 400 km of distance and 400 m of depth. A pattern of isolation by depth emerged, but geographic distance between sites may further limit gene flow. Water mass boundaries may serve to isolate populations across depth; however, adaptive divergence with depth is also a possible scenario. Microsatellite markers also revealed significant genetic differentiation (FST=0.434) between C. delta and a closely-related species, C. americana, demonstrating the utility of microsatellites in species delimitation of octocorals. Results provided support for the depth-differentiation hypothesis, strengthening the notion that factors co-varying with depth serve as isolation mechanisms in deep-sea populations.
    Description: Funding was provided by BOEM and NOAA-OER (BOEM contract #M08PC20038) for the Lophelia II project led by TDI-Brooks International. AMQ was funded by the Dr. Nancy Foster Scholarship program, Temple University Dissertation Completion Grant, and the Lerner-Gray grant for marine research.
    Description: 2016-04-22
    Keywords: Deep sea ; Population genetics ; Connectivity ; Adaptive divergence ; Octocoral ; Gulf of Mexico
    Repository Name: Woods Hole Open Access Server
    Type: Preprint
    Format: application/pdf
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...