Libraug Libraries
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
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. -
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. -
I. Türkiye Derin Deniz Ekosistemi Çaliştayi Bildiriler Kitabi 19 Haziran 2017
I. TÜRKİYE DERİN DENİZ EKOSİSTEMİ ÇALIŞTAYI BİLDİRİLER KİTABI 19 HAZİRAN 2017 İstanbul Üniversitesi, Su Bilimleri Fakültesi, Gökçeada Deniz Araştırmaları Birimi, Çanakkale, Gökçeada EDİTÖRLER ONUR GÖNÜLAL BAYRAM ÖZTÜRK NURİ BAŞUSTA Bu kitabın bütün hakları Türk Deniz Araştırmaları Vakfı’na aittir. İzinsiz basılamaz, çoğaltılamaz. Kitapta bulunan makalelerin bilimsel sorumluluğu yazarlarına aittir. All rights are reserved. No part of this publication may be reproduced, stored in a retrieval system, or transmitted in any form or by any means without the prior permission from the Turkish Marine Research Foundation. Copyright © Türk Deniz Araştırmaları Vakfı ISBN-978-975-8825-37-0 Kapak fotoğrafları: Mustafa YÜCEL, Bülent TOPALOĞLU, Onur GÖNÜLAL Kaynak Gösterme: GÖNÜLAL O., ÖZTÜRK B., BAŞUSTA N., (Ed.) 2017. I. Türkiye Derin Deniz Ekosistemi Çalıştayı Bildiriler Kitabı, Türk Deniz Araştırmaları Vakfı, İstanbul, Türkiye, TÜDAV Yayın no: 45 Türk Deniz Araştırmaları Vakfı (TÜDAV) P. K: 10, Beykoz / İstanbul, TÜRKİYE Tel: 0 216 424 07 72, Belgegeçer: 0 216 424 07 71 Eposta: [email protected] www.tudav.org ÖNSÖZ Dünya denizlerinde 200 metre derinlikten sonra başlayan bölgeler ‘Derin Deniz’ veya ‘Deep Sea’ olarak bilinir. Son 50 yılda sualtı teknolojisindeki gelişmelere bağlı olarak birçok ulus bu bilinmeyen deniz ortamlarını keşfetmek için yarışırken yeni cihazlar denemekte ayrıca yeni türler keşfetmektedirler. Özellikle Amerika, İngiltere, Kanada, Japonya başta olmak üzere birçok ülke derin denizlerin keşfi yanında derin deniz madenciliğine de ilgi göstermektedirler. Daha şimdiden Yeni Gine izin ve ruhsatlandırma işlemlerine başladı bile. Bütün bunlar olurken ülkemizde bu konuda çalışan uzmanları bir araya getirerek sinerji oluşturma görevini yine TÜDAV üstlendi. Memnuniyetle belirtmek gerekir ki bu çalıştay amacına ulaşmış 17 değişik kurumdan 30 uzman değişik konularda bildiriler sunarak konuya katkı sunmuşlardır. -
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. -
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. -
Chemical and Thermal Description of the Environment of the Genesis Hydrothermal Vent Community (13°N, EPR)
Cah. Biol. Mar. (1998) 39 : 159-167 Chemical and thermal description of the environment of the Genesis hydrothermal vent community (13°N, EPR) Pierre-Marie SARRADIN1, Jean-Claude CAPRAIS1, Patrick BRIAND1, Françoise GAILL2, Bruce SHILLITO2 et Daniel DESBRUYÈRES1 1 DRO/EP/LEA IFREMER centre de BREST - BP 70 - F-29280 PLOUZANE (France), 2 INSU / CNRS / UPMC Roscoff / Paris (France) Fax: (33) 2 98 22 47 57; e-mail: [email protected] Abstract: The objective of this study is to describe the chemical and physical environment surrounding the vent organisms at the Genesis site (EPR, 2640 m). The main chimney is colonized by Riftia pachyptila, fishes Zoarcidae and crabs Bythograeidae. The top of the smoker is covered with tubes of polychaetes Alvinellidae, the frontier zone by limpet gastropods. Temperature measurements and water sampling were made on an axis along the chimney. The environment was characterized using relationships between chemical concentrations and temperature to provide a chemo-thermal model of the site. Discrete temperature ranges were l-1.6°C in sea water, 1.6- 10°C among Riftia plumes (up to 25°C at the tube base), 7-91°C close to the alvinellid tubes, fluid emission was 262-289°C. This study describes the habitat - 2- -1 -1 of Alvinellidae emphasizing its chemical (£S [H2S + HS + S ] 3-300 µmol l , CO2 3.5-6 mmol l , pH 5.7-7.5) and thermal specificities compared to the Riftia ones (IS 4-12 µmol l-1 ; CO2 2-3.5 mmol 1-1 ; pH 5.8-7.7). The size of Riftia allowed us to define its environment at the organism (temperature gradient along the tube 0.5-1°C cm-1) and population scales (temperature difference between organisms from the same clump: 10-20°C). -
Seafloor Hydrothermal Activity Along Mid-Ocean Ridge With
www.nature.com/scientificreports OPEN Seafoor hydrothermal activity along mid-ocean ridge with strong melt supply: study from segment Received: 21 February 2019 Accepted: 26 June 2019 27, southwest Indian ridge Published: xx xx xxxx Xihe Yue1,2, Huaiming Li2, Jianye Ren1, Chunhui Tao2,3, Jianping Zhou2, Yuan Wang2 & Xiaoxia Lü1 Continuous tow investigations have shown that the present vent feld inventory along fast to intermediate spreading ridges may be underestimated by at least 3–6 times, while the limited towed line investigations of venting sites along slow to ultra-slow spreading ridges make it impossible to determine their distribution. The Chinese Dayang cruise has conducted detailed towed line surveys of hydrothermal activity on segment 27 of the ultra-slow spreading southwest Indian ridge in 2015. The results have identifed as many as 9 hydrothermal felds along 85-km-long segment, including one confrmed hydrothermal feld, three inferred hydrothermal felds and fve suspected felds. Hydrothermal activities are not only limited along-axis but also found approximately 10 km away from the axis. These vent felds are likely powered by a seismically identifed axial magma chamber, including melt migration along normal faults to fank areas. The calculated hydrothermal activity frequency on segment 27 is approximately 3.6–8 times higher than that calculated from the Interridge database, suggesting that careful system exploration can reveal more hydrothermal activities even on ultra-slow spreading ridges efected by hotspot. Hydrothermal activity is widespread on the seafoor, such as at ocean spreading ridges (OSRs) and arc volcanoes1. Te study of hydrothermal feld plays a key role in ocean-crust interactions, the formation of seafoor massive sulfde deposits and oceanic chemical and biogeochemical cycles2–5. -
Hydrothermal Vent Periphery Invertebrate Community Habitat Preferences of the Lau Basin
California State University, Monterey Bay Digital Commons @ CSUMB Capstone Projects and Master's Theses Capstone Projects and Master's Theses Summer 2020 Hydrothermal Vent Periphery Invertebrate Community Habitat Preferences of the Lau Basin Kenji Jordi Soto California State University, Monterey Bay Follow this and additional works at: https://digitalcommons.csumb.edu/caps_thes_all Recommended Citation Soto, Kenji Jordi, "Hydrothermal Vent Periphery Invertebrate Community Habitat Preferences of the Lau Basin" (2020). Capstone Projects and Master's Theses. 892. https://digitalcommons.csumb.edu/caps_thes_all/892 This Master's Thesis (Open Access) is brought to you for free and open access by the Capstone Projects and Master's Theses at Digital Commons @ CSUMB. It has been accepted for inclusion in Capstone Projects and Master's Theses by an authorized administrator of Digital Commons @ CSUMB. For more information, please contact [email protected]. HYDROTEHRMAL VENT PERIPHERY INVERTEBRATE COMMUNITY HABITAT PREFERENCES OF THE LAU BASIN _______________ A Thesis Presented to the Faculty of Moss Landing Marine Laboratories California State University Monterey Bay _______________ In Partial Fulfillment of the Requirements for the Degree Master of Science in Marine Science _______________ by Kenji Jordi Soto Spring 2020 CALIFORNIA STATE UNIVERSITY MONTEREY BAY The Undersigned Faculty Committee Approves the Thesis of Kenji Jordi Soto: HYDROTHERMAL VENT PERIPHERY INVERTEBRATE COMMUNITY HABITAT PREFERENCES OF THE LAU BASIN _____________________________________________ -
A New Vent Limpet in the Genus Lepetodrilus (Gastropoda: Lepetodrilidae) from Southern Ocean Hydrothermal Vent Fields Showing High Phenotypic Plasticity
fmars-06-00381 July 15, 2019 Time: 15:56 # 1 ORIGINAL RESEARCH published: 16 July 2019 doi: 10.3389/fmars.2019.00381 A New Vent Limpet in the Genus Lepetodrilus (Gastropoda: Lepetodrilidae) From Southern Ocean Hydrothermal Vent Fields Showing High Phenotypic Plasticity Katrin Linse1*, Christopher Nicolai Roterman2 and Chong Chen3 1 British Antarctic Survey, Cambridge, United Kingdom, 2 Department of Zoology, University of Oxford, Oxford, United Kingdom, 3 X-STAR, Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Yokosuka, Japan The recently discovered hydrothermal vent ecosystems in the Southern Ocean host a suite of vent-endemic species, including lepetodrilid limpets dominating in abundance. Limpets were collected from chimneys, basalts and megafauna of the East Scotia Ridge Edited by: segments E2 and E9 and the Kemp Caldera at the southern end of the South Sandwich Wei-Jen Chen, Island arc. The limpets varied in size and shell morphology between vent fields and National Taiwan University, Taiwan displayed a high degree of phenotypic plasticity. Size frequency analyses between vent Reviewed by: fields suggests continuous reproduction in the limpet and irregular colonisation events. Marjolaine Matabos, Institut Français de Recherche pour Phylogenetic reconstructions and comparisons of mitochondrial COI gene sequences l’Exploitation de la Mer (IFREMER), revealed a level of genetic similarity between individuals from the three vent fields France Junlong Zhang, consistent with them belonging to a single molecular operational taxonomic unit. Here Institute of Oceanology (CAS), China we describe Lepetodrilus concentricus n. sp., and evaluate its genetic distinctness and *Correspondence: pylogenetic position with congeners based on the same gene. Results indicate that Katrin Linse L. -
Revisiting the Lepetodrilus Elevatus Species Complex
Revisiting the Lepetodrilus elevatus species complex (Vetigastropoda: Lepetodrilidae), using samples from the Galápagos and Guaymas hydrothermal vent systems Marjolaine Matabos, Didier Jollivet To cite this version: Marjolaine Matabos, Didier Jollivet. Revisiting the Lepetodrilus elevatus species complex (Vetigas- tropoda: Lepetodrilidae), using samples from the Galápagos and Guaymas hydrothermal vent systems. Journal of Molluscan Studies, Oxford University Press (OUP), 2019, 85 (1), pp.154-165. 10.1093/mol- lus/eyy061. hal-02354593 HAL Id: hal-02354593 https://hal.archives-ouvertes.fr/hal-02354593 Submitted on 7 Nov 2019 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. 1 Revisiting the Lepetodrilus elevatus species complex (Vetigastropoda: 2 Lepetodrilidae), using samples from the Galápagos and Guaymas 3 hydrothermal vent systems 4 Marjolaine Matabos1 and Didier Jollivet2 5 6 1IFREMER, Centre de Bretagne, REM/EEP, Laboratoire Environnement Profond, 7 29280 Plouzané, France; and 8 2Sorbonne Université, UPMC Univ. Paris 06, CNRS UMR 7144, Adaptation et 9 Diversité en Milieu Marin, Equipe ABICE, Station Biologique de Roscoff, 29688 10 Roscoff, France 11 Correspondence: M. Matabos; e-mail: [email protected] 12 (Received 7 June 2018 ; editorial decision 9 November 2018) 13 Running head: LEPETODRILUS ELEVATUS SPECIES COMPLEX 14 15 1 16 ABSTRACT 17 The current distribution ranges of vent species result from the complex tectonic history 18 of oceanic ridges. -
Genetic Diversity and Connectivity of Deepsea Hydrothermal Vent
Molecular Ecology (2010) 19, 4391–4411 doi: 10.1111/j.1365-294X.2010.04789.x INVITED REVIEW Genetic diversity and connectivity of deep-sea hydrothermal vent metapopulations ROBERT C. VRIJENHOEK Monterey Bay Aquarium Research Institute, 7700 Sandholdt Road, Moss Landing, CA 95039, USA Abstract Deep-sea hydrothermal vents provide ephemeral habitats for animal communities that depend on chemosynthetic primary production. Sporadic volcanic and tectonic events destroy local vent fields and create new ones. Ongoing dispersal and cycles of extirpation and colonization affect the levels and distribution of genetic diversity in vent metapopulations. Several species exhibit evidence for stepping-stone dispersal along relatively linear, oceanic, ridge axes. Other species exhibit very high rates of gene flow, although natural barriers associated with variation in depth, deep-ocean currents, and lateral offsets of ridge axes often subdivide populations. Various degrees of impedance to dispersal across such boundaries are products of species-specific life histories and behaviours. Though unrelated to the size of a species range, levels of genetic diversity appear to correspond with the number of active vent localities that a species occupies within its range. Pioneer species that rapidly colonize nascent vents tend to be less subdivided and more diverse genetically than species that are slow to establish colonies at vents. Understanding the diversity and connectivity of vent metapopulations provides essential information for designing deep-sea preserves in regions that are under consideration for submarine mining of precious metals. Keywords: hydrothermal vent, metapopulations, stepping-stone dispersal Received 30 April 2010; revision received 13 July 2010; accepted 15 July 2010 ‘There are many questions to be answered about these animal bacteria that fix organic carbon and serve as primary communities. -
Data Sources the Next 64 Pages Comprise a Reference List
SUPPORTING INFORMATION APPENDIX 1: Data Sources The next 64 pages comprise a reference list for all literary sources given as references for trait scores and/or comments in the sFDvent raw (marked with an asterisk (*) if not then included in recommended) and/or recommended datasets (Tables S4.3 and S4.2, respectively). These references are not in alphabetical order, as the database is a ‘living’ record, so new references will be added and a new number assigned. In the recommended dataset (Table S4.2), the references are recorded according to the numbers listed below (and in Table S1.1), to ensure that citations are relatively easy for users to carry through when conducting analyses using subsets of the data, for example. If a score in the recommended dataset is supported by more than one reference, multiple reference identifiers are provided and separated by a semi-colon (;). The references are not provided as numbers / identifiers in the other versions of the dataset, as information is lost during this processing step (e.g., ‘expert opinion’, or 66, replaces comments made by experts in each reference column regarding additional observations, rationale for certainty scores, etc.), which may prove useful for some users. Other versions of the dataset thus maintain raw reference entries for transparency and as potentially useful metadata. We provide a copy of the recommended dataset without the references as numbers (Table S4.2A), in case it is easier for users to cross-reference between the two sheets to seek additional comments for a given data subset of interest. 1. Aguado, M.