Metal Concentrations in Deep-Sea Mussels from a Hydrothermal Vent and Cold Seep
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Hydrothermal Vents. Teacher's Notes
Hydrothermal Vents Hydrothermal Vents. Teacher’s notes. A hydrothermal vent is a fissure in a planet's surface from which geothermally heated water issues. They are usually volcanically active. Seawater penetrates into fissures of the volcanic bed and interacts with the hot, newly formed rock in the volcanic crust. This heated seawater (350-450°) dissolves large amounts of minerals. The resulting acidic solution, containing metals (Fe, Mn, Zn, Cu) and large amounts of reduced sulfur and compounds such as sulfides and H2S, percolates up through the sea floor where it mixes with the cold surrounding ocean water (2-4°) forming mineral deposits and different types of vents. In the resulting temperature gradient, these minerals provide a source of energy and nutrients to chemoautotrophic organisms that are, thus, able to live in these extreme conditions. This is an extreme environment with high pressure, steep temperature gradients, and high concentrations of toxic elements such as sulfides and heavy metals. Black and white smokers Some hydrothermal vents form a chimney like structure that can be as 60m tall. They are formed when the minerals that are dissolved in the fluid precipitates out when the super-heated water comes into contact with the freezing seawater. The minerals become particles with high sulphur content that form the stack. Black smokers are very acidic typically with a ph. of 2 (around that of vinegar). A black smoker is a type of vent found at depths typically below 3000m that emit a cloud or black material high in sulphates. White smokers are formed in a similar way but they emit lighter-hued minerals, for example barium, calcium and silicon. -
Cold Seep Benthic Communities in Japan Subduction Zones: Spatial Organization, Trophic Strategies and Evidence for Temporal Evolution*
MARINE ECOLOGY - PROGRESS SERIES Vol. 40: 115-126. 1987 Published October 7 Mar. Ecol. Prog. Ser. Cold seep benthic communities in Japan subduction zones: spatial organization, trophic strategies and evidence for temporal evolution* S. Kim Juniper", Myriam Sibuet IFREMER, Centre de Brest. BP 337. F-29273 Brest Cedex. France ABSTRACT: Submersible exploration of the Japan subduction zones has revealed benthic communities dominated by clams (Calyptogena spp.) around sed~mentporewater seeps at depths from 3850 to 6000 m. Photographic and video records were used to produce microcartographlc reconstructions of 3 contrasting cold seep sites. Spatial and abundance relations of megafauna lead us to propose several hypotheses regard~ngthe ecological functioning of these cold seep communities. We dlst~nguish between the likely direct use of reducing substances in venting fluids by Calyptogena-bacteria symbioses and indirect usage by accompanying abyssal species not known to harbour symbionts. Microdistribution and known or presumed feedmg modes of the accompanying species indicate 2 different sources of organic matter enrichment within cold seep sites: organic debris originating from bivalve colonies, and enrichment of extensive areas of surrounding surface sediments where weaker, more hffuse porewater seepage may support chemosynthetic production by free-living bacteria. The occurrence of colony-like groupings of empty Calyptogena valves indicates that cold seeps are ephemeral, with groups of living clams, mixed living and dead clams, and empty dissolving shells marlung the course of a cycle of porewater venting and offering clues to the recent history of cold seep activity. INTRODUCTION al. 1985). One of the bivalve species from this area has been shown to harbour symbiotic bacteria in its gill The discovery of deep-sea hydrothermal vents has tissue and to oxidise methane (Childress et al. -
Biodiversity and Trophic Ecology of Hydrothermal Vent Fauna Associated with Tubeworm Assemblages on the Juan De Fuca Ridge
Biogeosciences, 15, 2629–2647, 2018 https://doi.org/10.5194/bg-15-2629-2018 © Author(s) 2018. This work is distributed under the Creative Commons Attribution 4.0 License. Biodiversity and trophic ecology of hydrothermal vent fauna associated with tubeworm assemblages on the Juan de Fuca Ridge Yann Lelièvre1,2, Jozée Sarrazin1, Julien Marticorena1, Gauthier Schaal3, Thomas Day1, Pierre Legendre2, Stéphane Hourdez4,5, and Marjolaine Matabos1 1Ifremer, Centre de Bretagne, REM/EEP, Laboratoire Environnement Profond, 29280 Plouzané, France 2Département de sciences biologiques, Université de Montréal, C.P. 6128, succursale Centre-ville, Montréal, Québec, H3C 3J7, Canada 3Laboratoire des Sciences de l’Environnement Marin (LEMAR), UMR 6539 9 CNRS/UBO/IRD/Ifremer, BP 70, 29280, Plouzané, France 4Sorbonne Université, UMR7144, Station Biologique de Roscoff, 29680 Roscoff, France 5CNRS, UMR7144, Station Biologique de Roscoff, 29680 Roscoff, France Correspondence: Yann Lelièvre ([email protected]) Received: 3 October 2017 – Discussion started: 12 October 2017 Revised: 29 March 2018 – Accepted: 7 April 2018 – Published: 4 May 2018 Abstract. Hydrothermal vent sites along the Juan de Fuca community structuring. Vent food webs did not appear to be Ridge in the north-east Pacific host dense populations of organised through predator–prey relationships. For example, Ridgeia piscesae tubeworms that promote habitat hetero- although trophic structure complexity increased with ecolog- geneity and local diversity. A detailed description of the ical successional stages, showing a higher number of preda- biodiversity and community structure is needed to help un- tors in the last stages, the food web structure itself did not derstand the ecological processes that underlie the distribu- change across assemblages. -
Understanding Bioluminescence in Dinoflagellates—How Far Have We Come?
Microorganisms 2013, 1, 3-25; doi:10.3390/microorganisms1010003 OPEN ACCESS microorganisms ISSN 2076-2607 www.mdpi.com/journal/microorganisms Review Understanding Bioluminescence in Dinoflagellates—How Far Have We Come? Martha Valiadi 1,* and Debora Iglesias-Rodriguez 2 1 Department of Evolutionary Ecology, Max Planck Institute for Evolutionary Biology, August-Thienemann-Strasse, Plӧn 24306, Germany 2 Department of Ecology, Evolution and Marine Biology, University of California Santa Barbara, Santa Barbara, CA 93106, USA; E-Mail: [email protected] * Author to whom correspondence should be addressed; E-Mail: [email protected] or [email protected]; Tel.: +49-4522-763277; Fax: +49-4522-763310. Received: 3 May 2013; in revised form: 20 August 2013 / Accepted: 24 August 2013 / Published: 5 September 2013 Abstract: Some dinoflagellates possess the remarkable genetic, biochemical, and cellular machinery to produce bioluminescence. Bioluminescent species appear to be ubiquitous in surface waters globally and include numerous cosmopolitan and harmful taxa. Nevertheless, bioluminescence remains an enigmatic topic in biology, particularly with regard to the organisms’ lifestyle. In this paper, we review the literature on the cellular mechanisms, molecular evolution, diversity, and ecology of bioluminescence in dinoflagellates, highlighting significant discoveries of the last quarter of a century. We identify significant gaps in our knowledge and conflicting information and propose some important research questions -
Ocean Ridge Hydrothermal Vent Fluids Alison Marie Bray University of New Hampshire, Durham
University of New Hampshire University of New Hampshire Scholars' Repository Doctoral Dissertations Student Scholarship Winter 2001 The geochemistry of boron and lithium in mid - ocean ridge hydrothermal vent fluids Alison Marie Bray University of New Hampshire, Durham Follow this and additional works at: https://scholars.unh.edu/dissertation Recommended Citation Bray, Alison Marie, "The eg ochemistry of boron and lithium in mid -ocean ridge hydrothermal vent fluids" (2001). Doctoral Dissertations. 46. https://scholars.unh.edu/dissertation/46 This Dissertation is brought to you for free and open access by the Student Scholarship at University of New Hampshire Scholars' Repository. It has been accepted for inclusion in Doctoral Dissertations by an authorized administrator of University of New Hampshire Scholars' Repository. For more information, please contact [email protected]. NOTE TO USERS This reproduction is the best copy available. __ ® UMI Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. THE GEOCHEMISTRY OF BORON AND LITHIUM IN MID-OCEAN RIDGE HYDROTHERMAL VENT FLUIDS by Alison Marie Bray Bachelor of Arts, University of San Diego, 1995 Master of Science, University of New Hampshire, 1998 Submitted to the University of New Hampshire in Partial Fulfillment of the Requirements for the Degree of Doctor of Philosophy In Earth Sciences December 2001 Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. UMI Number: 3030597 ___ ® UMI UMI Microform 3030597 Copyright 2002 by Bell & Howell Information and Learning Company. All rights reserved. This microform edition is protected against unauthorized copying under Title 17, United States Code. -
Development of Bioaccumulation Factors for Protection of Fish and Wildlife in the Great Lakes
National Sediment Bioaccumulation Conference Development of Bioaccumulation Factors for Protection of Fish and Wildlife in the Great Lakes Philip M. Cook and Dr. Lawrence P. Burkhard U.S. Environmental Protection Agency, Office of Research and Development, Duluth, Minnesota ioaccumulation factor (BAF) development for ap factors that must be considered when predicting bioaccu plication to the Great Lakes, and in particular for mulation from measured or predicted concentrations of the recent Great Lakes Water Quality Initiative chemicals in the water and sediments of the ecosystem. (GLWQI) effort of U.S. EPA and the respective Great Lakes The bioavailability considerations that remain, after in states, illustrates the importance of the linkage between corporating the influence of organism lipid, organic car sediments and the water column and its influence on bon in water and sediments, and trophic level into BAFfds B f exposure of all aquatic biota. This presentation included and BSAFs to reduce uncertainty for site-specific a discussion of the development and application of bioavailability conditions, are shown on the z-axis. Ba bioaccumulation factors for fish, both water-based BAFs sically, this residual bioavailability factor is the chemical and biota-sediment accumulation factors (BSAFs), with distribution between water and sediment which can vary emphasis on the role of sediments in bioaccumulation of between ecosystems or vary temporally and spatially persistent, hydrophobic non-polar organic chemicals by within an ecosystem. Chemical properties which influ both benthic and pelagic organisms. Choices of bioaccu ence bioaccumulation are shown on the x-axis. The mulation factors are important because they will strongly octanol-water partition coefficient (Kow) is the primary influence predictions of toxic effects in aquatic organ indicator of chemical hydrophobicity and bioaccumula isms, especially when chemical residue-based dose-re tion potential. -
An Estimate of Hydrothermal Fluid Residence Times and Vent Chimney
Earth and Planetary Science Letters, 76 (1985/86) 35-44 35 Elsevier Science Publishers B.V., Amsterdam Printed in The Netherlands [6] An estimate of hydrothermal fluid residence times and vent chimney growth rates based on 210 Pb/Pb ratios and mineralogic studies of sulfides dredged from the Juan de Fuca Ridge David Kadko ~, Randolph Koski 2 Mitsunobu Tatsumoto 3 and Robin Bouse 2 i College of Oceanograpt~v, Oregon State Unieersio,, Cort,allis, OR 97331 (U.S.A.) : U.S. Geological Survey, 345 3~iiddlefield Road, Menlo Park, CA 94025 (U.S.A.) -~ U.S. Geological Survey, Denver. CO 80225 (U.S.A.) Received January 22, 1985; revised version received August 26, 1985 The 2u~Pb/Pb ratios across two sulfide samples dredged from the Juan de Fuca Ridge are used to estimate the growth rate of the sulfide material and the residence time of the hydrothermal fluid within the oceanic crust from the onset of basalt alteration. 21°Pb is added to the hydrothermal fluid by two processes: (1) high-temperature alteration of basalt and (2) if the residence time of the fluid is on the order of the 22.3-year half-life of 210 Pb, by in-situ growth from 222 Rn (Krishnaswami and Turekian, 1982). Stable lead is derived only from the alteration of basalt. The 21°Pb/Pb ratio across one sample was - 0.5 dpm/10 6 g Pb, and across the other it was - 0.4 dpm/10 6 g Pb. These values are quite close to the 23SU/Pb ratios of basalts from the area, suggesting that the residence time of the hydrothermal fluid from the onset of basalt alteration is appreciably less than the mean life of 21°pb. -
Ecological Characterization of Bioluminescence in Mangrove Lagoon, Salt River Bay, St. Croix, USVI
Ecological Characterization of Bioluminescence in Mangrove Lagoon, Salt River Bay, St. Croix, USVI James L. Pinckney (PI)* Dianne I. Greenfield Claudia Benitez-Nelson Richard Long Michelle Zimberlin University of South Carolina Chad S. Lane Paula Reidhaar Carmelo Tomas University of North Carolina - Wilmington Bernard Castillo Kynoch Reale-Munroe Marcia Taylor University of the Virgin Islands David Goldstein Zandy Hillis-Starr National Park Service, Salt River Bay NHP & EP 01 January 2013 – 31 December 2013 Duration: 1 year * Contact Information Marine Science Program and Department of Biological Sciences University of South Carolina Columbia, SC 29208 (803) 777-7133 phone (803) 777-4002 fax [email protected] email 1 TABLE OF CONTENTS INTRODUCTION ............................................................................................................................................... 4 BACKGROUND: BIOLUMINESCENT DINOFLAGELLATES IN CARIBBEAN WATERS ............................................... 9 PROJECT OBJECTIVES ..................................................................................................................................... 19 OBJECTIVE I. CONFIRM THE IDENTIY OF THE BIOLUMINESCENT DINOFLAGELLATE(S) AND DOMINANT PHYTOPLANKTON SPECIES IN MANGROVE LAGOON ........................................................................ 22 OBJECTIVE II. COLLECT MEASUREMENTS OF BASIC WATER QUALITY PARAMETERS (E.G., TEMPERATURE, SALINITY, DISSOLVED O2, TURBIDITY, PH, IRRADIANCE, DISSOLVED NUTRIENTS) FOR CORRELATION WITH PHYTOPLANKTON -
Determining the Depth Limit of Bioluminescent Sources in Scattering Media
bioRxiv preprint doi: https://doi.org/10.1101/2020.04.21.044982; this version posted April 23, 2020. The copyright holder for this preprint (which was not certified by peer review) is the author/funder. All rights reserved. No reuse allowed without permission. Determining the Depth Limit of Bioluminescent Sources in Scattering Media. Ankit Raghuram1,*, Fan Ye1, Jesse K. Adams1,2, Nathan Shaner3, Jacob T. Robinson1,2,4,5, Ashok Veeraraghavan1,2,6 1 Department of Electrical and Computer Engineering, Rice University, Houston, TX 77005, USA 2 Applied Physics Program, Rice University, Houston, TX 77005, USA 3 Department of Neurosciences, University of California San Diego, La Jolla, CA 92093, USA 4 Department of Neuroscience, Baylor College of Medicine, Houston, TX 77030, USA 5 Department of Bioengineering, Rice University, Houston, TX 77005, USA 6 Department of Computer Science, Rice University, Houston TX 77005, USA * [email protected] Abstract Bioluminescence has several potential advantages compared to fluorescence microscopy for in vivo biological imaging. Because bioluminescence does not require excitation light, imaging can be performed for extended periods of time without phototoxicity or photobleaching, and optical systems can be smaller, simpler, and lighter. Eliminating the need for excitation light may also affect how deeply one can image in scattering biological tissue, but the imaging depth limits for bioluminescence have yet to be reported. Here, we perform a theoretical study of the depth limits of bioluminescence microscopy and find that cellular resolution imaging should be possible at a depth of 5-10 mean free paths (MFPs). This limit is deeper than the depth limit for confocal microscopy and slightly lower than the imaging limit expected for two-photon microscopy under similar conditions. -
Structure and Distribution of Cold Seep Communities Along the Peruvian Active Margin: Relationship to Geological and Fluid Patterns
MARINE ECOLOGY PROGRESS SERIES Vol. 132: 109-125, 1996 Published February 29 Mar Ecol Prog Ser l Structure and distribution of cold seep communities along the Peruvian active margin: relationship to geological and fluid patterns 'Laboratoire Ecologie Abyssale, DROIEP, IFREMER Centre de Brest, BP 70, F-29280 Plouzane, France '~epartementdes Sciences de la Terre, UBO, 6 ave. Le Gorgeu, F-29287 Brest cedex, France 3~aboratoireEnvironnements Sedimentaires, DROIGM, IFREMER Centre de Brest, BP 70, F-29280 Plouzane, France "niversite P. et M. Curie, Observatoire Oceanologique de Banyuls, F-66650 Banyuls-sur-Mer, France ABSTRACT Exploration of the northern Peruvian subduction zone with the French submersible 'Nau- tile' has revealed benthlc communities dominated by new species of vesicomyid bivalves (Calyptogena spp and Ves~comyasp ) sustained by methane-nch fluid expulsion all along the continental margin, between depths of 5140 and 2630 m Videoscoplc studies of 25 dives ('Nautiperc cruise 1991) allowed us to describe the distribution of these biological conlnlunities at different spahal scales At large scale the communities are associated with fluid expuls~onalong the major tectonic features (scarps, canyons) of the margln At a smaller scale on the scarps, the distribuhon of the communities appears to be con- trolled by fluid expulsion along local fracturatlon features such as joints, faults and small-scale scars Elght dlves were made at one particular geological structure the Middle Slope Scarp (the scar of a large debns avalanche) where numerous -
Reconstructing the History of Fluid Flow at Cold Seep Sites from Ba/Ca Ratios
Limnol. Oceanogr., 46(7), 2001, 1701±1708 q 2001, by the American Society of Limnology and Oceanography, Inc. Reconstructing the history of ¯uid ¯ow at cold seep sites from Ba/Ca ratios in vesicomyid clam shells M. E. Torres1 COAS, 104 Ocean Administration Building, Oregon State University, Corvallis, Oregon 97331 J. P. Barry MBARI, 7700 Sandholdt Road, Moss Landing, California 95039 D. A. Hubbard COAS, 104 Ocean Administration Building, Oregon State University, Corvallis, Oregon 97331 E. Suess GEOMAR, 1-3 Wischhofstrasse, Kiel D-24148, Germany Abstract Hydrogen sul®de discharge at cold seep sites is recorded as enrichment in the barium to calcium (Ba/Ca) ratio in shells of vesicomyid clams collected live from cold seeps in Monterey Canyon and the Cascadia margin. A direct relationship between increased Ba ¯uxes from cold seeps and Ba incorporation into shells was established for the Cascadia margin site. For the Monterey canyon site, a 2-yr episode of high ¯uid ¯ow centered on 1992 was inferred from coherent changes in the Ba/Ca pro®les of three Calyptogena kilmeri shells. Comparison with precipitation and d18O data indicates that this high-¯ow period may have been driven by an increase in rainfall after the 1988±1990 California drought. High-resolution records preserved in clam shells are shown to be useful in elucidating charac- teristics, history, and possible mechanisms driving ¯uid discharge at continental margin seeps, thus establishing their potential use as paleotracers of ¯uid seepage events. An extensive set of geophysical and geochemical mea- seepage along continental margins. Carbon and oxygen iso- surements is currently available to document the ¯ow and tope records of calcareous macrofossils have long been used expulsion of ¯uids at transform and convergent margins. -
Lakes: Ann, Gilchrist, Grove, Leven, Reno, Villard, Smith)
Status and Trend Monitoring Summary for Selected Pope and Douglas County, Minnesota Lakes 2000 (Lakes: Ann, Gilchrist, Grove, Leven, Reno, Villard, Smith) Minnesota Pollution Control Agency Environmental Outcomes Division Environmental Monitoring and Analysis Section Andrea Plevan and Steve Heiskary September 2001 Printed on recycled paper containing at least 10 percent fibers from paper recycled by consumers. This material may be made available in other formats, including Braille, large format and audiotape. MPCA Status and Trend Monitoring Summary for 2000 Pope County Lakes Part 1: Purpose of study and background information on MN lakes The Minnesota Pollution Control Agency’s (MPCA) core lake-monitoring programs include the Citizen Lake Monitoring Program (CLMP), the Lake Assessment Program (LAP), and the Clean Water Partnership (CWP) Program. In addition to these programs, the MPCA annually monitors numerous lakes to provide baseline water quality data, provide data for potential LAP and CWP lakes, characterize lake conditions in different regions of the state, examine year-to-year variability in ecoregion reference lakes, and provide additional trophic status data for lakes exhibiting trends in Secchi transparency. In the latter case, we attempt to determine if the trends in Secchi transparency are “real,” i.e., if supporting trophic status data substantiate whether a change in trophic status has occurred. The lake sampling efforts also provide a means to respond to citizen concerns about protecting or improving the lake in cases where no data exists to evaluate the quality of the lake. For efficient sampling, we tend to select geographic clusters of lakes (e.g., focus on a specific county) whenever possible.