Life Is Weird! (Adapted from the 2003 Windows to the Deep Expedition)
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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. -
Benchmark 3: Evaluation of Alternatives with Respect to Existing Conditions August 2015
Salton Sea Funding and Feasibility Action Plan Benchmark 3: Evaluation of Alternatives With Respect to Existing Conditions August 2015 Prepared by: Prepared for: This document is prepared as a living document for public review and comment. Comments may be provided to: Salton Sea Authority 82995 Hwy 111, Suite 200 Indio, CA 92201 Email: [email protected] Comments will be reviewed and incorporated as appropriate. If substantive comments are received, a revised document may be produced and distributed. Preferred citation: Salton Sea Authority (2015). Salton Sea Funding and Feasibility Action Plan Benchmark 3 Report: Evaluation of Alternatives With Respect to Existing Conditions, August Report. Revision Record Revisions to this document will be reviewed and approved through the same level of authority as the original document. All changes to the Benchmark 3 Report must be authorized by the Principal in Charge. Date Version Changes January Working Posted on Salton Sea Authority website. 2015 Draft Included changes from draft review by Salton Sea TCT. June 2015 First Updated hydrology section and inflow Complete projections including Figures 48-52, along with Document editorial revisions. August Revision 1 Added this Revision Record. Corrected title of 2015 California Department of Fish and Wildlife and other minor editorial revisions. Updated discussion of historical flows from 2003-present. Tetra Tech, Inc. i August 2015 Executive Summary This report presents a review of Salton Sea restoration alternatives and their components and determine how well they would perform under current and future inflows. Alternatives are considered with respect to existing hydrologic conditions at the Sea, as of 2014, and projected future hydrology. -
Consequences of Drying Lake Systems Around the World
Consequences of Drying Lake Systems around the World Prepared for: State of Utah Great Salt Lake Advisory Council Prepared by: AECOM February 15, 2019 Consequences of Drying Lake Systems around the World Table of Contents EXECUTIVE SUMMARY ..................................................................... 5 I. INTRODUCTION ...................................................................... 13 II. CONTEXT ................................................................................. 13 III. APPROACH ............................................................................. 16 IV. CASE STUDIES OF DRYING LAKE SYSTEMS ...................... 17 1. LAKE URMIA ..................................................................................................... 17 a) Overview of Lake Characteristics .................................................................... 18 b) Economic Consequences ............................................................................... 19 c) Social Consequences ..................................................................................... 20 d) Environmental Consequences ........................................................................ 21 e) Relevance to Great Salt Lake ......................................................................... 21 2. ARAL SEA ........................................................................................................ 22 a) Overview of Lake Characteristics .................................................................... 22 b) Economic -
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 -
Lled Basins of the Red
Deep-Sea Research I 46 (1999) 1779}1792 Hydrographic changes during 20 years in the brine-"lled basins of the Red Sea Pierre Anschutz! *,GeH rard Blanc!, Fabienne Chatin", Magali Geiller", Marie-Claire Pierret" !De& partement de Ge& ologie et Oce&anographie (D.G.O.), Universite& Bordeaux 1, CNRS UMR 5805, 33405 Talence Cedex, France "Centre de Ge& ochimie de la Surface, Institut de Ge&ologie, Universite& Louis Pasteur, CNRS UMR 7517, 67084, Strasbourg, France Received 16 June 1998; accepted 8 February 1999 Abstract Many of the deep basins "lled by hot brines in the Red Sea have not been investigated since their discovery in the early 1970s. Twenty years later, in September 1992, six of these deeps were revisited. The temperature and salinity of the Suakin, Port Sudan, Chain B, and Nereus deeps ranged from 23.25 to 44.603C and from 144 to 270&. These values were approximately the same in 1972, indicating that the budget of heat and salt was quite balanced. We measured strong gradients of properties in the transition zone between brines and overlying seawater. The contribution of salinity to the density gradient was more than one order of magnitude higher than the opposite contribution of temperature across the seawater}brine interface. Therefore the interface was extemely stable, and the transfer of properties across it was considered to be controlled mostly by molecular di!usion. We calculate that the di!usional transport of salt from the brines to seawater cannot a!ect signi"cantly the salinity of the brines over a 20 year period, which agrees with the observations. -
Ocean Storage
277 6 Ocean storage Coordinating Lead Authors Ken Caldeira (United States), Makoto Akai (Japan) Lead Authors Peter Brewer (United States), Baixin Chen (China), Peter Haugan (Norway), Toru Iwama (Japan), Paul Johnston (United Kingdom), Haroon Kheshgi (United States), Qingquan Li (China), Takashi Ohsumi (Japan), Hans Pörtner (Germany), Chris Sabine (United States), Yoshihisa Shirayama (Japan), Jolyon Thomson (United Kingdom) Contributing Authors Jim Barry (United States), Lara Hansen (United States) Review Editors Brad De Young (Canada), Fortunat Joos (Switzerland) 278 IPCC Special Report on Carbon dioxide Capture and Storage Contents EXECUTIVE SUMMARY 279 6.7 Environmental impacts, risks, and risk management 298 6.1 Introduction and background 279 6.7.1 Introduction to biological impacts and risk 298 6.1.1 Intentional storage of CO2 in the ocean 279 6.7.2 Physiological effects of CO2 301 6.1.2 Relevant background in physical and chemical 6.7.3 From physiological mechanisms to ecosystems 305 oceanography 281 6.7.4 Biological consequences for water column release scenarios 306 6.2 Approaches to release CO2 into the ocean 282 6.7.5 Biological consequences associated with CO2 6.2.1 Approaches to releasing CO2 that has been captured, lakes 307 compressed, and transported into the ocean 282 6.7.6 Contaminants in CO2 streams 307 6.2.2 CO2 storage by dissolution of carbonate minerals 290 6.7.7 Risk management 307 6.2.3 Other ocean storage approaches 291 6.7.8 Social aspects; public and stakeholder perception 307 6.3 Capacity and fractions retained -
Okeanos Explorer Rov Dive Summary
OKEANOS EXPLORER ROV DIVE SUMMARY Site Name GB907 Expedition Kelley Elliott/ Coordinator/ Brian Bingham ROV Lead Stephanie Farrington (Biology) Science Team Leads Jamie Austin (Geology) General Area Gulf of Mexico Descriptor Cruise Season Leg Dive Number ROV Dive Name EX1402 3 DIVE02 ROV: Deep Discoverer Equipment Deployed Camera Platform: Seirios CTD Depth Altitude Scanning Sonar USBL Position Heading ROV Measurements Pitch Roll HD Camera 1 HD Camera 2 Low Res Cam 1 Low Res Cam 2 Low Res Cam 3 Low Res Cam 4 Low Res Cam 2 Equipment N/A Malfunctions Dive Summary: EX1402L3_DIVE02 ^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^ In Water at: 2014-04-13T13:45:38.439000 27°, 05.899' N ; 092°, 37.310' W Out Water at: 2014-04-13T19:12:34.841000 27°, 05.096' N ; 092°, 36.588' W ROV Dive Summary Off Bottom at: 2014-04-13T18:24:04.035000 (From processed ROV 27°, 05.455' N ; 092°, 36.956' W data) On Bottom at: 2014-04-13T14:31:16.507000 27°, 05.519' N ; 092°, 37.099' W Dive duration: 5:26:56 Bottom Time: 3:52:47 Max. depth: 1266.7 m Special Notes Primary Jamie Austin, EX, UT Austin, [email protected] Stephanie Farrington, EX, HBOI/FAU, [email protected] Andrea Quattrini, Temple, Temple, [email protected] Scientists Involved Bernie Ball, Duke, Duke, [email protected] (please provide name / Brian Kinlan, NOAA NMFS, [email protected] location / affiliation / email) Carolyn Ruppel, Woods Hole, USGS, [email protected] Erik Cordes, Temple, Temple, [email protected] Larry Mayer, UNH, UNH CCOM, [email protected] Michael Vecchione, -
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 -
A Phytoremediation Pilot Project at the LCP Chemicals
Case Study LCP Chemicals Site Phytoremediation Pilot Project Shea Jones Remedial Project Manager EPA Region 4 Outline of Presentation z Background Information z Groundwater Quality z Groundwater Seeps z Project Goal z Implementation of Project z Community and Agency Concerns z Current Status z Next Steps z Lessons Learned Background Information z 550-acre site z Former oil refinery, paint manufacturing co., power plant, and chlor-alkali facility operated from 1919- 1994 z Significant PRP-led removal actions in 1999 ($60 million) z Soil and sediment contaminated with lead, mercury, and PCBs z Fish advisories z Currently in RI/FS phase Groundwater Quality z Multiple rounds of horizontal and vertical well data z Hg levels as high as 330 ppb and Pb as high as 120 ppb z Hg found below a sandstone layer z Caustic Brine Pool below old cell buildings z Removal Action Groundwater Seeps z During conditions of high water table, seepage of groundwater occurs along portions of the shoreline that separates the upland soils from the tidal marsh z Dark brown color z Some COCs present at elevated levels (74 ppb Hg and 60 ppb Pb) Project Goal z To locally suppress the groundwater table (0.9 ft) and therefore, prevent the seeps from recontaminating the marsh z Secondary Goals – Create a root zone that will degrade organic contaminants through microbial degradation – Stabilize metals and take them up (lower mobility and availability) z Insert first scanned picture showing seep location z Insert scanned pics showing conceptual site model Plant Selection z List of potentially applicable plants was examined z List narrowed based on tolerance to site conditions (i.e. -
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 -
Algae Flora of Graduation Towers in the Town of Ciechocinek
Ecological Questions 14/2011: 25 – 29 DOI: 10.2478/v10090-011-0007-6 Algae flora of graduation towers in the town of Ciechocinek Marta Luścińska, Malwina Gadziemska Department of Plant Ecology and Nature Protection Nicolaus Copernicus University, Gagarina 9, 87–100 Toruń e-mail: [email protected] Summary. The research was focused on algae occurring on wooden constructions of three graduation towers, which are the main ele- ments of historical salt production technology, located in the health-resort of Ciechocinek in the region of Kujawy. The research also included algae occurring in reservoirs with brine condensed on graduation towers, as well as algae from puddles and the soil under the graduation towers. 52 algae taxa were recorded in the collected material. Representatives of the following phyla were distinguished: 5 taxa of Cyanoprokaryota, 46 taxa of Heterokontophyta (including 44 taxa of diatoms) and 7 taxa of Chlorophyta. Samples from the sites with brine of the lowest salt concentration (4%) turned out to be the most abundant in species. Key words: halophylic algae, diatoms Chlorophyta, Dunalulla, brine, saline soils. 1. Introduction ers no. 1 and 3 (Fig. 1). She reported the occurrence of 44 algae species, mainly diatoms. All the aforementioned studies focused on algae in- The occurrence of algae in the environment with extreme habiting puddles and small water bodies with different de- salinity, such as gradually thickened brine flowing down grees of salinity, located within salt marshes. Whereas the the graduation towers in Ciechocinek, evoked interest present paper aims at investigating the algae flora occur- among researchers already since the end of the 19th cen- ring on construction elements of the graduation towers, as tury.