Ocean Literacy with Each One, Teach One Cards
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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. -
Introduction to Co2 Chemistry in Sea Water
INTRODUCTION TO CO2 CHEMISTRY IN SEA WATER Andrew G. Dickson Scripps Institution of Oceanography, UC San Diego Mauna Loa Observatory, Hawaii Monthly Average Carbon Dioxide Concentration Data from Scripps CO Program Last updated August 2016 2 ? 410 400 390 380 370 2008; ~385 ppm 360 350 Concentration (ppm) 2 340 CO 330 1974; ~330 ppm 320 310 1960 1965 1970 1975 1980 1985 1990 1995 2000 2005 2010 2015 Year EFFECT OF ADDING CO2 TO SEA WATER 2− − CO2 + CO3 +H2O ! 2HCO3 O C O CO2 1. Dissolves in the ocean increase in decreases increases dissolved CO2 carbonate bicarbonate − HCO3 H O O also hydrogen ion concentration increases C H H 2. Reacts with water O O + H2O to form bicarbonate ion i.e., pH = –lg [H ] decreases H+ and hydrogen ion − HCO3 and saturation state of calcium carbonate decreases H+ 2− O O CO + 2− 3 3. Nearly all of that hydrogen [Ca ][CO ] C C H saturation Ω = 3 O O ion reacts with carbonate O O state K ion to form more bicarbonate sp (a measure of how “easy” it is to form a shell) M u l t i p l e o b s e r v e d indicators of a changing global carbon cycle: (a) atmospheric concentrations of carbon dioxide (CO2) from Mauna Loa (19°32´N, 155°34´W – red) and South Pole (89°59´S, 24°48´W – black) since 1958; (b) partial pressure of dissolved CO2 at the ocean surface (blue curves) and in situ pH (green curves), a measure of the acidity of ocean water. -
History of Scuba Diving About 500 BC: (Informa on Originally From
History of Scuba Diving nature", that would have taken advantage of this technique to sink ships and even commit murders. Some drawings, however, showed different kinds of snorkels and an air tank (to be carried on the breast) that presumably should have no external connecons. Other drawings showed a complete immersion kit, with a plunger suit which included a sort of About 500 BC: (Informaon originally from mask with a box for air. The project was so Herodotus): During a naval campaign the detailed that it included a urine collector, too. Greek Scyllis was taken aboard ship as prisoner by the Persian King Xerxes I. When Scyllis learned that Xerxes was to aack a Greek flolla, he seized a knife and jumped overboard. The Persians could not find him in the water and presumed he had drowned. Scyllis surfaced at night and made his way among all the ships in Xerxes's fleet, cung each ship loose from its moorings; he used a hollow reed as snorkel to remain unobserved. Then he swam nine miles (15 kilometers) to rejoin the Greeks off Cape Artemisium. 15th century: Leonardo da Vinci made the first known menon of air tanks in Italy: he 1772: Sieur Freminet tried to build a scuba wrote in his Atlanc Codex (Biblioteca device out of a barrel, but died from lack of Ambrosiana, Milan) that systems were used oxygen aer 20 minutes, as he merely at that me to arficially breathe under recycled the exhaled air untreated. water, but he did not explain them in detail due to what he described as "bad human 1776: David Brushnell invented the Turtle, first submarine to aack another ship. -
Sea-Level Rise for the Coasts of California, Oregon, and Washington: Past, Present, and Future
Sea-Level Rise for the Coasts of California, Oregon, and Washington: Past, Present, and Future As more and more states are incorporating projections of sea-level rise into coastal planning efforts, the states of California, Oregon, and Washington asked the National Research Council to project sea-level rise along their coasts for the years 2030, 2050, and 2100, taking into account the many factors that affect sea-level rise on a local scale. The projections show a sharp distinction at Cape Mendocino in northern California. South of that point, sea-level rise is expected to be very close to global projections; north of that point, sea-level rise is projected to be less than global projections because seismic strain is pushing the land upward. ny significant sea-level In compliance with a rise will pose enor- 2008 executive order, mous risks to the California state agencies have A been incorporating projec- valuable infrastructure, devel- opment, and wetlands that line tions of sea-level rise into much of the 1,600 mile shore- their coastal planning. This line of California, Oregon, and study provides the first Washington. For example, in comprehensive regional San Francisco Bay, two inter- projections of the changes in national airports, the ports of sea level expected in San Francisco and Oakland, a California, Oregon, and naval air station, freeways, Washington. housing developments, and sports stadiums have been Global Sea-Level Rise built on fill that raised the land Following a few thousand level only a few feet above the years of relative stability, highest tides. The San Francisco International Airport (center) global sea level has been Sea-level change is linked and surrounding areas will begin to flood with as rising since the late 19th or to changes in the Earth’s little as 40 cm (16 inches) of sea-level rise, a early 20th century, when climate. -
Causes of Sea Level Rise
FACT SHEET Causes of Sea OUR COASTAL COMMUNITIES AT RISK Level Rise What the Science Tells Us HIGHLIGHTS From the rocky shoreline of Maine to the busy trading port of New Orleans, from Roughly a third of the nation’s population historic Golden Gate Park in San Francisco to the golden sands of Miami Beach, lives in coastal counties. Several million our coasts are an integral part of American life. Where the sea meets land sit some of our most densely populated cities, most popular tourist destinations, bountiful of those live at elevations that could be fisheries, unique natural landscapes, strategic military bases, financial centers, and flooded by rising seas this century, scientific beaches and boardwalks where memories are created. Yet many of these iconic projections show. These cities and towns— places face a growing risk from sea level rise. home to tourist destinations, fisheries, Global sea level is rising—and at an accelerating rate—largely in response to natural landscapes, military bases, financial global warming. The global average rise has been about eight inches since the centers, and beaches and boardwalks— Industrial Revolution. However, many U.S. cities have seen much higher increases in sea level (NOAA 2012a; NOAA 2012b). Portions of the East and Gulf coasts face a growing risk from sea level rise. have faced some of the world’s fastest rates of sea level rise (NOAA 2012b). These trends have contributed to loss of life, billions of dollars in damage to coastal The choices we make today are critical property and infrastructure, massive taxpayer funding for recovery and rebuild- to protecting coastal communities. -
Natural Variability of the Arctic Ocean Sea Ice During the Present Interglacial
Natural variability of the Arctic Ocean sea ice during the present interglacial Anne de Vernala,1, Claude Hillaire-Marcela, Cynthia Le Duca, Philippe Robergea, Camille Bricea, Jens Matthiessenb, Robert F. Spielhagenc, and Ruediger Steinb,d aGeotop-Université du Québec à Montréal, Montréal, QC H3C 3P8, Canada; bGeosciences/Marine Geology, Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research, 27568 Bremerhaven, Germany; cOcean Circulation and Climate Dynamics Division, GEOMAR Helmholtz Centre for Ocean Research, 24148 Kiel, Germany; and dMARUM Center for Marine Environmental Sciences and Faculty of Geosciences, University of Bremen, 28334 Bremen, Germany Edited by Thomas M. Cronin, U.S. Geological Survey, Reston, VA, and accepted by Editorial Board Member Jean Jouzel August 26, 2020 (received for review May 6, 2020) The impact of the ongoing anthropogenic warming on the Arctic such an extrapolation. Moreover, the past 1,400 y only encom- Ocean sea ice is ascertained and closely monitored. However, its pass a small fraction of the climate variations that occurred long-term fate remains an open question as its natural variability during the Cenozoic (7, 8), even during the present interglacial, on centennial to millennial timescales is not well documented. i.e., the Holocene (9), which began ∼11,700 y ago. To assess Here, we use marine sedimentary records to reconstruct Arctic Arctic sea-ice instabilities further back in time, the analyses of sea-ice fluctuations. Cores collected along the Lomonosov Ridge sedimentary archives is required but represents a challenge (10, that extends across the Arctic Ocean from northern Greenland to 11). Suitable sedimentary sequences with a reliable chronology the Laptev Sea were radiocarbon dated and analyzed for their and biogenic content allowing oceanographical reconstructions micropaleontological and palynological contents, both bearing in- can be recovered from Arctic Ocean shelves, but they rarely formation on the past sea-ice cover. -
OCEAN WARMING • the Ocean Absorbs Most of the Excess Heat from Greenhouse Gas Emissions, Leading to Rising Ocean Temperatures
NOVEMBER 2017 OCEAN WARMING • The ocean absorbs most of the excess heat from greenhouse gas emissions, leading to rising ocean temperatures. • Increasing ocean temperatures affect marine species and ecosystems. Rising temperatures cause coral bleaching and the loss of breeding grounds for marine fishes and mammals. • Rising ocean temperatures also affect the benefits humans derive from the ocean – threatening food security, increasing the prevalence of diseases and causing more extreme weather events and the loss of coastal protection. • Achieving the mitigation targets set by the Paris Agreement on climate change and limiting the global average temperature increase to well below 2°C above pre-industrial levels is crucial to prevent the massive, irreversible impacts of ocean warming on marine ecosystems and their services. • Establishing marine protected areas and putting in place adaptive measures, such as precautionary catch limits to prevent overfishing, can protect ocean ecosystems and shield humans from the effects of ocean warming. The distribution of excess heat in the ocean is not What is the issue? uniform, with the greatest ocean warming occurring in The ocean absorbs vast quantities of heat as a result the Southern Hemisphere and contributing to the of increased concentrations of greenhouse gases in subsurface melting of Antarctic ice shelves. the atmosphere, mainly from fossil fuel consumption. The Fifth Assessment Report published by the Intergovernmental Panel on Climate Change (IPCC) in 2013 revealed that the ocean had absorbed more than 93% of the excess heat from greenhouse gas emissions since the 1970s. This is causing ocean temperatures to rise. Data from the US National Oceanic and Atmospheric Administration (NOAA) shows that the average global sea surface temperature – the temperature of the upper few metres of the ocean – has increased by approximately 0.13°C per decade over the past 100 years. -
Chapter 51. Biological Communities on Seamounts and Other Submarine Features Potentially Threatened by Disturbance
Chapter 51. Biological Communities on Seamounts and Other Submarine Features Potentially Threatened by Disturbance Contributors: J. Anthony Koslow, Peter Auster, Odd Aksel Bergstad, J. Murray Roberts, Alex Rogers, Michael Vecchione, Peter Harris, Jake Rice, Patricio Bernal (Co-Lead members) 1. Physical, chemical, and ecological characteristics 1.1 Seamounts Seamounts are predominantly submerged volcanoes, mostly extinct, rising hundreds to thousands of metres above the surrounding seafloor. Some also arise through tectonic uplift. The conventional geological definition includes only features greater than 1000 m in height, with the term “knoll” often used to refer to features 100 – 1000 m in height (Yesson et al., 2011). However, seamounts and knolls do not appear to differ much ecologically, and human activity, such as fishing, focuses on both. We therefore include here all such features with heights > 100 m. Only 6.5 per cent of the deep seafloor has been mapped, so the global number of seamounts must be estimated, usually from a combination of satellite altimetry and multibeam data as well as extrapolation based on size-frequency relationships of seamounts for smaller features. Estimates have varied widely as a result of differences in methodologies as well as changes in the resolution of data. Yesson et al. (2011) identified 33,452 seamount and guyot features > 1000 m in height and 138,412 knolls (100 – 1000 m), whereas Harris et al. (2014) identified 10,234 seamount and guyot features, based on a stricter definition that restricted seamounts to conical forms. Estimates of total abundance range to >100,000 seamounts and to 25 million for features > 100 m in height (Smith 1991; Wessel et al., 2010). -
Dives of the Bathyscaph Trieste, 1958-1963: Transcriptions of Sixty-One Dictabelt Recordings in the Robert Sinclair Dietz Papers, 1905-1994
Dives of the Bathyscaph Trieste, 1958-1963: Transcriptions of sixty-one dictabelt recordings in the Robert Sinclair Dietz Papers, 1905-1994 from Manuscript Collection MC28 Archives of the Scripps Institution of Oceanography University of California, San Diego La Jolla, California 92093-0219: September 2000 This transcription was made possible with support from the U.S. Naval Undersea Museum 2 TABLE OF CONTENTS INTRODUCTION ...........................................................................................................................4 CASSETTE TAPE 1 (Dietz Dictabelts #1-5) .................................................................................6 #1-5: The Big Dive to 37,800. Piccard dictating, n.d. CASSETTE TAPE 2 (Dietz Dictabelts #6-10) ..............................................................................21 #6: Comments on the Big Dive by Dr. R. Dietz to complete Piccard's description, n.d. #7: On Big Dive, J.P. #2, 4 Mar., n.d. #8: Dive to 37,000 ft., #1, 14 Jan 60 #9-10: Tape just before Big Dive from NGD first part has pieces from Rex and Drew, Jan. 1960 CASSETTE TAPE 3 (Dietz Dictabelts #11-14) ............................................................................30 #11-14: Dietz, n.d. CASSETTE TAPE 4 (Dietz Dictabelts #15-18) ............................................................................39 #15-16: Dive #61 J. Piccard and Dr. A. Rechnitzer, depth of 18,000 ft., Piccard dictating, n.d. #17-18: Dive #64, 24,000 ft., Piccard, n.d. CASSETTE TAPE 5 (Dietz Dictabelts #19-22) ............................................................................48 #19-20: Dive Log, n.d. #21: Dr. Dietz on the bathysonde, n.d. #22: from J. Piccard, 14 July 1960 CASSETTE TAPE 6 (Dietz Dictabelts #23-25) ............................................................................57 #23-25: Italian Dive, Dietz, Mar 8, n.d. CASSETTE TAPE 7 (Dietz Dictabelts #26-29) ............................................................................64 #26-28: Italian Dive, Dietz, n.d. -
Animal Utilization by the Cozumel Maya: Interpretation Through Faunal Analysis
Animal utilization by the Cozumel Maya: interpretation through faunal analysis Item Type text; Dissertation-Reproduction (electronic) Authors Hamblin, Nancy Lee Publisher The University of Arizona. Rights Copyright © is held by the author. Digital access to this material is made possible by the University Libraries, University of Arizona. Further transmission, reproduction or presentation (such as public display or performance) of protected items is prohibited except with permission of the author. Download date 11/10/2021 13:10:15 Link to Item http://hdl.handle.net/10150/565460 ANIMAL UTILIZATION BY THE COZUMEL MAYA; INTERPRETATION THROUGH FAUNAL ANALYSIS by Nancy Lee Hamblin A Dissertation Submitted to the Faculty of the DEPARTMENT OF ANTHROPOLOGY In Partial Fulfillment of the Requirements For the Degree of DOCTOR OF PHILOSOPHY In the Graduate College THE UNIVERSITY OF ARIZONA 1 9 8 0 - Copyright 1980 Nancy Lee Hamblin (c ) 1980 NANCY LEE HAMBLIN ALL RIGHTS RESERVED THE UNIVERSITY OF ARIZONA GRADUATE COLLEGE As members of the Final Examination Committee, we certify that we have read the dissertation prepared by Nancy Lee Hamblin entitled ANIMAL UTILIZATION BY THE COZUMEL MAYA: INTERPRETATION________ ■■ THROUGH FAUNAL ANALYSIS_______________________________________ and recommend that it be accepted as fulfilling the dissertation requirement *or the Degree of ________ Doctor of Philosophy_________________________ . L i __ M f r l c A . / f Date / f f a n A /y- i m Date Date Date Date Final approval and acceptance of this dissertation is contingent upon the candidate's submission of the final copy of the dissertation to the Graduate College. I hereby certify that I have read this dissertation prepared under my direction and recommend that it be accepted as fulfilling the dissertation requirement. -
Altitude on Cartographic Materials and Its Correction According to New Measurement Techniques
remote sensing Article Altitude on Cartographic Materials and Its Correction According to New Measurement Techniques Kamil Maciuk 1,* , Michał Apollo 2 , Joanna Mostowska 3 , Tomáš Lepeška 4 , Mojca Poklar 5 , Tomasz Noszczyk 6 , Pawel Kroh 7 , Artur Krawczyk 8 , Łukasz Borowski 9 and Polona Pavlovˇciˇc-Prešeren 10 1 Department of Integrated Geodesy and Cartography, AGH University of Science and Technology, Al. Mickiewicza 30, 30-059 Krakow, Poland 2 Department of Tourism and Regional Studies, Institute of Geography, Pedagogical University of Cracow, ul. Podchor ˛azych˙ 2, 30-084 Krakow, Poland; [email protected] 3 Faculty of Geography and Regional Studies, University of Warsaw, ul. Krakowskie Przedmie´scie30, 00-927 Warszaw, Poland; [email protected] 4 Department of Applied Ecology, Faculty of Ecology and Environmental Sciences, Technical University in Zvolen, ul. T. G. Masaryka 24, 960 01 Zvolen, Slovakia; [email protected] 5 Faculty of Humanities, University of Primorska, Titov trg 5, 6000 Koper, Slovenia; [email protected] 6 Department of Land Management and Landscape Architecture, Faculty of Environmental Engineering and Land Surveying, University of Agriculture in Krakow, ul. Balicka 253 C, 30-198 Kraków, Poland; [email protected] 7 Faculty of Geography and Biology, Pedagogical University of Cracow, ul. Podchor ˛azych˙ 2, 30-084 Kraków, Poland; [email protected] 8 Department of Mine Areas Protection, Geoinformatics and Mine Surveying, AGH University of Science and Technology, Al. Mickiewicza -
BOULDERS on ASTEROIDS DIDYMOS and DIMORPHOS: FUTURE DART-Liciacube OBSERVATIONS
52nd Lunar and Planetary Science Conference 2021 (LPI Contrib. No. 2548) 1116.pdf BOULDERS ON ASTEROIDS DIDYMOS AND DIMORPHOS: FUTURE DART-LICIACube OBSERVATIONS M. Pajola1, A. Lucchetti1, S. Ivanovski2, G. Poggiali3,4, S. Ieva5, D. Perna5, E. Dotto5, V. Della Corte6, G. Cremonese1, M. Amoroso7, S. Pirrotta7, E. Mazzotta Epifani5, A. Cheng8, N. Chabot8, A. Rivkin8, O. Barnouin8, C. Ernst8, R.T. Daly8, M. Hirabayashi9, E. Asphaug10, S.R. Schwartz10, J.M. Trigo-Rodriguez11, E.G. Fahnestock12, P. Michel13, I. Bertini14, J.R. Brucato3, A. Capannolo15, B. Cotugno16, V. Di Tana16, I. Gai17, G. Impresario7, M. Lavagna15, A. Meneghin3, F. Miglioretti16, D. Modenini17, P. Palumbo14,6, A. Rossi18, E. Simioni1, S. Simonetti16, P. Tortora17, M. Zannoni17, G. Zanotti15, A. Zinzi19,7. 1INAF-Astronomical Observatory of Padova, Vic. Osservatorio 5, 35122 Padova, Italy ([email protected]); 2INAF Osservatorio Astronomico di Trieste, Trieste, Italy; 3INAF Osservatorio Astrofisico di Arcetri, Firenze, Italy; 4Università di Firenze, Dipartimento di Fisica e Astronomia, Sesto Fiorentino (Firenze), Italy; 5INAF Osservatorio Astronomico di Roma, Monte Porzio Catone (Roma), Italy; 6INAF Istituto di Astrofisica e Planetologia Spaziali, Roma, Italy; 7Agenzia Spaziale Italiana, via del Politecnico, 00133 Roma, Italy; 8Johns Hopkins University Applied Physics Laboratory, Laurel, MD-USA; 9Auburn University, Auburn, AL-USA; 10Lunar and Planetary Laboratory, University of Arizona, Tucson, AZ-USA; 11Institute of Space Sciences (IEEC-CSIC), Dept. of Astrophysics,