The Truth About Sharks the Story of the Sea Turtle the World of Whales
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Worksheet 5.1--The History of Oceanography
Worksheet 5.1--The History of Oceanography Reading: Introduction to the World’s Oceans pages 4-22 1. The field of oceanography today is so broad that oceanography is usually broken down into a number of sub disciplines: a. ________________________________________ includes the study of the earth at the sea’s edge and below its surface b. ________________________________________ investigates how and why the oceans move c. ________________________________________ is the study of heat transfer, water cycles, and air-sea interactions. d. ________________________________________ studies the composition and history of the water e. ________________________________________ concerns the marine organisms and the relationship between these organisms and the environment. f. ________________________________________ is the discipline that designs and plans equipment and installations for use at sea. 2. When did oceanography begin to develop as a modern science? ____________________ The Early Times 3. Around 200 BC the Egyptian scientist Eratosthenes mapped the known world and calculated the circumference of the earth as 40,250 km. Today’s measurement is ______________ . How far from the correct value was Erathosthenes? 4. Approximately 350 years later the Roman Scientist Ptolemy produced the world’s first atlas. His atlas listed more than 8,000 places by latitude and longitude but his work contained a major flaw. What was it? 5. What difference would it have made for Columbus and other explorers if they had used Erathosthenes’ more accurate estimate of the earth’s circumference rather than Ptolemy’s flawed estimate? The Middle Ages 6. When did the Vikings reach North America? _______________ 7. Who first established regular trade routes across the Indian Ocean? _______________ 8. -
Deep-Sea Mining: the Basics
A fact sheet from June 2018 NOAA Office of Ocean Exploration and Research Deep-sea Mining: The Basics Overview The deepest parts of the world’s ocean feature ecosystems found nowhere else on Earth. They provide habitat for multitudes of species, many yet to be named. These vast, lightless regions also possess deposits of valuable minerals in rich concentrations. Deep-sea extraction technologies may soon develop to the point where exploration of seabed minerals can give way to active exploitation. The International Seabed Authority (ISA) is charged with formulating and enforcing rules for all seabed mining that takes place in waters beyond national jurisdictions. These rules are now under development. Environmental regulations, liability and financial rules, and oversight and enforcement protocols all must be written and approved within three to five years. Figure 1 Types of Deep-sea Mining Production support vessel Return pipe Riser pipe Cobalt Seafloor massive Polymetallic crusts sulfides nodules Subsurface plumes 800-2,500 from return water meters deep Deposition 1,000-4,000 meters deep 4,000-6,500 meters deep Cobalt-rich Localized plumes Seabed pump Ferromanganeseferromanganese from cutting crusts Seafloor production tool Nodule deposit Massive sulfide deposit Sediment Source: New Zealand Environment Guide © 2018 The Pew Charitable Trusts 2 The legal foundations • The United Nations Convention on the Law of the Sea (UNCLOS). Also known as the Law of the Sea Treaty, UNCLOS is the constitutional document governing mineral exploitation on the roughly 60 percent of the world seabed that lies beyond national jurisdictions. UNCLOS took effect in 1994 upon passage of key enabling amendments designed to spur commercial mining. -
New Frontiers in Ocean Exploration the E/V Nautilus, NOAA Ship Okeanos Explorer, and R/V Falkor 2018 Field Season
New Frontiers in Ocean Exploration The E/V Nautilus, NOAA Ship Okeanos Explorer, and R/V Falkor 2018 Field Season GUEST EDITORS Nicole A. Raineault and Joanne Flanders Oceanography Vol. 32, No. 1, Supplement, March 2019 a PREFERRED CITATION Raineault, N.A, and J. Flanders, eds. 2019. New frontiers in ocean exploration: The E/V Nautilus, NOAA Ship Okeanos Explorer, and R/V Falkor 2018 field season. Oceanography 32(1), supplement, 150 pp., https://doi.org/10.5670/oceanog.2019.supplement.01. FRONT COVER A high-density habitat consisting of deep-sea sponge, coral, and squat lobsters on a previously unmapped and unex- plored seamount in Papahānaumokuākea Marine National Monument. The photo was taken during E/V Nautilus cruise NA101. Image credit: D. Fornari (WHOI-MISO Facility) and OET The R/V Falkor team dove on “Rosebud,” a whale fall that was placed by researchers off San Diego, California, in La Jolla Canyon. Researchers noted changes in composition and life forms around the location in a beautiful, exciting dive investigating ecosystems unique to whale falls. Image credit: SOI b It Takes a Village! Managing Data from Okeanos Explorer By Barry Eakins, Susan Gottfried, Patrick Murphy, David Lovalvo, and Derek Sowers NOAA Ship Okeanos Explorer is a telepresence-enabled for near-real-time data sharing. The OER mapping team exploration vessel managed by NOAA’s Office of Marine and pioneered “telemapping” workflows to enable near-real- Aviation Operations with mission equipment operated by time processing of bathymetric data from its shoreside NOAA’s Office of Ocean Exploration and Research, in part- facility at the University of New Hampshire (UNH). -
Deep-Sea Life Issue 8, November 2016 Cruise News Going Deep: Deepwater Exploration of the Marianas by the Okeanos Explorer
Deep-Sea Life Issue 8, November 2016 Welcome to the eighth edition of Deep-Sea Life: an informal publication about current affairs in the world of deep-sea biology. Once again we have a wealth of contributions from our fellow colleagues to enjoy concerning their current projects, news, meetings, cruises, new publications and so on. The cruise news section is particularly well-endowed this issue which is wonderful to see, with voyages of exploration from four of our five oceans from the Arctic, spanning north east, west, mid and south Atlantic, the north-west Pacific, and the Indian Ocean. Just imagine when all those data are in OBIS via the new deep-sea node…! (see page 24 for more information on this). The photo of the issue makes me smile. Angelika Brandt from the University of Hamburg, has been at sea once more with her happy-looking team! And no wonder they look so pleased with themselves; they have collected a wonderful array of life from one of the very deepest areas of our ocean in order to figure out more about the distribution of these abyssal organisms, and the factors that may limit their distribution within this region. Read more about the mission and their goals on page 5. I always appreciate feedback regarding any aspect of the publication, so that it may be improved as we go forward. Please circulate to your colleagues and students who may have an interest in life in the deep, and have them contact me if they wish to be placed on the mailing list for this publication. -
Teeth Penetration Force of the Tiger Shark Galeocerdo Cuvier and Sandbar Shark Carcharhinus Plumbeus
Journal of Fish Biology (2017) 91, 460–472 doi:10.1111/jfb.13351, available online at wileyonlinelibrary.com Teeth penetration force of the tiger shark Galeocerdo cuvier and sandbar shark Carcharhinus plumbeus J. N. Bergman*†‡, M. J. Lajeunesse* and P. J. Motta* *University of South Florida, Department of Integrative Biology, 4202 East Fowler Avenue, Tampa, FL 33620, U.S.A. and †Florida Fish and Wildlife Conservation Commission, Florida Fish and Wildlife Research Institute, 100 Eighth Avenue S.E., Saint Petersburg, FL 33701, U.S.A. (Received 16 February 2017, Accepted 15 May 2017) This study examined the minimum force required of functional teeth and replacement teeth in the tiger shark Galeocerdo cuvier and the sandbar shark Carcharhinus plumbeus to penetrate the scales and muscle of sheepshead Archosargus probatocephalus and pigfish Orthopristis chrysoptera. Penetra- tion force ranged from 7·7–41·9and3·2–26·3 N to penetrate A. probatocephalus and O. chrysoptera, respectively. Replacement teeth required significantly less force to penetrate O. chrysoptera for both shark species, most probably due to microscopic wear of the tooth surfaces supporting the theory shark teeth are replaced regularly to ensure sharp teeth that are efficient for prey capture. © 2017 The Fisheries Society of the British Isles Key words: biomechanics; bite force; Elasmobranchii; teleost; tooth morphology. INTRODUCTION Research on the functional morphology of feeding in sharks has typically focused on the kinematics and mechanics of cranial movement (Ferry-Graham, 1998; Wilga et al., 2001; Motta, 2004; Huber et al., 2005; Motta et al., 2008), often neglecting to integrate the function of teeth (but see Ramsay & Wilga, 2007; Dean et al., 2008; Whitenack et al., 2011). -
Ore Bin / Oregon Geology Magazine / Journal
State of Oregon The ORE BIN· Department of Geology Volume 34,no. 10 and Mineral Industries 1069 State Office BI dg. October 1972 Portland Oregon 97201 FOSSil SHARKS IN OREGON Bruce J. Welton* Approximately 21 species of sharks, skates, and rays are either indigenous to or occasionally visit the Oregon coast. The Blue Shark Prionace glauca, Soup-fin Shark Galeorhinus zyopterus, and the Dog-fish Shark Squalus acanthias commonly inhabit our coastal waters. These 21 species are represented by 16 genera, of which 10 genera are known from the fossi I record in Oregon. The most common genus encountered is the Dog-fish Shark Squalus. The sharks, skates, and rays, (all members of the Elasmobranchii) have a fossil record extending back into the Devonian period, but many major groups became extinct before or during the Mesozoic. A rapid expansion in the number of new forms before the close of the Mesozoic gave rise to practically all the Holocene families living today. Paleozoic shark remains are not known from Oregon, but teeth of the Cretaceous genus Scapanorhyn chus have been collected from the Hudspeth Formation near Mitchell, Oregon. Recent work has shown that elasmobranch teeth occur in abundance west of the Cascades in marine Tertiary strata ranging in age from late Eocene to middle Miocene (Figures 1 and 2). All members of the EIasmobranchii possess a cartilaginous endoskeleton which deteriorates rapidly upon death and is only rarely preserved in the fossil record. Only under exceptional conditions of preservation, usually in a highly reducing environment, will cranial or postcranial elements be fossilized. -
The Ernst Quarries Pricing Digging in the Sharktooth Hill Fossil Formation
The Ernst Quarries Pricing Digging in the Sharktooth Hill Fossil Formation OUR PRICING ALL PRICES ARE PER PERSON Admission ........................................................................ $40 Group Discounts for 10 or more, email for information. Everyone entering the property is subject to admission and a signed waiver, NO EXCEPTIONS. Check-in is between 7:45 and 8:15am at our staging point. A vehicle is required, no hikers or walking from the staging area is permitted. For safety reasons, a vehicle must stay with the participants (no drop offs). Unfortunately, we CANNOT accept debit or credit card payments at this time. Cash and checks are the ONLY methods of payment, and need to be presented prior to digging. WE LEAVE THE STAGING AREA PROMPTLY AT 8:30AM! If you cannot make the start time, please call prior to 8am and we can attempt to accommodate you, but there are no guarantees. You will caravan in your own vehicles to the property and arrive by 8:45am. After a short orientation/tour, you are free to begin digging (approx. 9am start after orientation). Due to ongoing construction activities, we currently cannot support any low profile vehicles. This includes cars such as Mini's, VW Bugs, and custom lowered vehicles. ALL TOOLS ARE PROVIDED. Children under 18 MUST be accompanied by an adult. Children under 8 must remain with an adult at all times (No Exceptions). Children under five will not be allowed to participate in digging actives with tooling. No dogs are allowed, this is for their safety. Many of the manageable hazards to humans are unmanageable and deadly to dogs. -
Seafloor Mapping | Educator
SEAFLOOR MAPPING | EDUCATOR Links to Next S T E M Generations Science Supplement Video | Standards | https://www.youtube.com/watch?v=rEPXuXf0_Ws https://vimeo.com/153100152 (password: exploration) MS-PS4-2: Develop and use a model to Pacing | 2 - 3 class periods (45 minutes each) describe that waves Background Needed | Basic understanding of sound, waves, earth history, earth are reflected, processes, sonar absorbed, or Assessment | Scientific & Technical Reporting rubric provided transmitted through Materials/Resources | various materials. ‣ Simulated seafloor boxes ‣ Low Resolution Grid (http://nautl.us/2eg1p5V) and High Resolution Grid MS-ESS2-3: Analyze and interpret data on (http://nautl.us/2dKZ7IN) ‣ the distribution of Wooden dowels fossils and rocks, ‣ Student data sheets continental shapes, ‣ Colored pencils and seafloor ‣ Calculators structures to provide ‣ Computers with Microsoft Excel (optional) evidence of the past plate motions. Overview MS-ESS3-1: Construct This module is designed to introduce students to multibeam sonar mapping. a scientific Students will use simulated sonar beams to produce depth data on a seafloor. explanation based on They will then take this data and produce a bathymetric map. Students will be evidence for how the asked to infer seafloor features based on two resolutions (low and high) of sonar uneven distributions imagery. Bathymetric maps can be produced by hand or students can easily use of Earth's mineral, Excel to produce 3D bathymetric images. energy, and groundwater resources are the Objectives & Learning Outcomes ‣ result of past and Students will be able to explain the importance of seafloor mapping to current geoscience understand the earth and ocean as well as understand how little of the global processes. -
Chapter 25 Creating a National Strategy For
PART VII SCIENCE-BASED DECISIONS: A DVANCING O UR U NDERSTANDING OF THE O CEANS CHAPTER 25 CREATING A NATIONAL STRATEGY FOR INCREASING SCIENTIFIC KNOWLEDGE ...............................................................374 CHAPTER 26 ACHIEVING A SUSTAINED, INTEGRATED OCEAN OBSERVING SYSTEM..........394 CHAPTER 27 ENHANCING OCEAN INFRASTRUCTURE AND TECHNOLOGY DEVELOPMENT........................................................................412 CHAPTER 28 MODERNIZING OCEAN DATA AND INFORMATION SYSTEMS ..................428 CHAPTER 25 CREATING A NATIONAL STRATEGY FOR INCREASING SCIENTIFIC KNOWLEDGE cean managers and policy makers need comprehensive scientific information Oabout the ocean and its environment to make wise decisions. Increased knowl- edge will help achieve sustainable resource use, economic development, and con- servation of the ocean’s biological diversity and natural beauty. However, to ensure the highest return on the nation’s investment in ocean research, exploration, and marine operations, a national strategy is needed. The strategy should coordinate and prioritize basic and applied ocean and coastal research supported by all federal agencies, increase partnerships with the academic and private sectors, promote enhanced ocean exploration, and coordinate federal marine operations to reduce redundancies. Significantly increased research in ocean-related natural and social sciences will also be key to fostering a new era of ecosystem-based management supported by sound science. Fortifying the Foundations of Ocean Understanding cean science and technology are integral parts of the overall OU.S. research enterprise and contribute greatly to society. They are essential to understanding the Earth’s environment and how it changes over time, improving climate predictions, managing marine resources wisely, finding beneficial new uses of ocean resources, protect- ing national security, and unlocking the basic mysteries of life on Earth. -
Re-Evaluation of Pachycormid Fishes from the Late Jurassic of Southwestern Germany
Editors' choice Re-evaluation of pachycormid fishes from the Late Jurassic of Southwestern Germany ERIN E. MAXWELL, PAUL H. LAMBERS, ADRIANA LÓPEZ-ARBARELLO, and GÜNTER SCHWEIGERT Maxwell, E.E., Lambers, P.H., López-Arbarello, A., and Schweigert G. 2020. Re-evaluation of pachycormid fishes from the Late Jurassic of Southwestern Germany. Acta Palaeontologica Polonica 65 (3): 429–453. Pachycormidae is an extinct group of Mesozoic fishes that exhibits extensive body size and shape disparity. The Late Jurassic record of the group is dominated by fossils from the lithographic limestone of Bavaria, Germany that, although complete and articulated, are not well characterized anatomically. In addition, stratigraphic and geographical provenance are often only approximately known, making these taxa difficult to place in a global biogeographical context. In contrast, the late Kimmeridgian Nusplingen Plattenkalk of Baden-Württemberg is a well-constrained locality yielding hundreds of exceptionally preserved and prepared vertebrate fossils. Pachycormid fishes are rare, but these finds have the potential to broaden our understanding of anatomical variation within this group, as well as provide new information regarding the trophic complexity of the Nusplingen lagoonal ecosystem. Here, we review the fossil record of Pachycormidae from Nusplingen, including one fragmentary and two relatively complete skulls, a largely complete fish, and a fragment of a caudal fin. These finds can be referred to three taxa: Orthocormus sp., Hypsocormus posterodorsalis sp. nov., and Simocormus macrolepidotus gen. et sp. nov. The latter taxon was erected to replace “Hypsocormus” macrodon, here considered to be a nomen dubium. Hypsocormus posterodorsalis is known only from Nusplingen, and is characterized by teeth lacking apicobasal ridging at the bases, a dorsal fin positioned opposite the anterior edge of the anal fin, and a hypural plate consisting of a fused parhypural and hypurals. -
Semionotiform Fish from the Upper Jurassic of Tendaguru (Tanzania)
Mitt. Mus. Nat.kd. Berl., Geowiss. Reihe 2 (1999) 135-153 19.10.1999 Semionotiform Fish from the Upper Jurassic of Tendaguru (Tanzania) Gloria Arratial & Hans-Peter Schultze' With 12 figures Abstract The late Late Jurassic fishes collected by the Tendaguru expeditions (1909-1913) are represented only by a shark tooth and various specimens of the neopterygian Lepidotes . The Lepidotes is a new species characterized by a combination of features such as the presence of scattered tubercles in cranial bones of adults, smooth ganoid scales, two suborbital bones, one row of infraorbital bones, non-tritoral teeth, hyomandibula with an anteriorly expanded membranous outgrowth, two extrascapular bones, two postcleithra, and the absence of fringing fulcra on all fins. Key words: Fishes, Actinopterygii, Semionotiformes, Late Jurassic, East-Africa . Zusammenfassung Die spätoberjurassischen Fische, die die Tendaguru-Expedition zwischen 1909 und 1913 gesammelt hat, sind durch einen Haizahn und mehrere Exemplare des Neopterygiers Lepidotes repräsentiert. Eine neue Art der Gattung Lepidotes ist be- schrieben, sie ist durch eine Kombination von Merkmalen (vereinzelte Tuberkel auf den Schädelknochen adulter Tiere, glatte Ganoidschuppen, zwei Suborbitalia, eine Reihe von Infraorbitalia, nichttritoriale Zähne, Hyomandibulare mit einer membra- nösen nach vorne gerichteten Verbreiterung, zwei Extrascapularia, zwei Postcleithra und ohne sich gabelnde Fulkren auf dem Vorderrand der Flossen) gekennzeichnet. Schlüsselwörter: Fische, Actinopterygii, Semionotiformes, Oberer Jura, Ostafrika. Introduction margin, crescent shaped lateral line pore, and the number of scales in vertical and longitudinal At the excavations of the Tendaguru expeditions rows), and on the shape of teeth (non-tritoral) . (1909-1913), fish remains were collected to- However, the Tendaguru lepidotid differs nota- gether with the spectacular reptiles in sediments bly from L. -
Stomach Contents of the Archaeocete Basilosaurus Isis: Apex Predator in Oceans of the Late Eocene
RESEARCH ARTICLE Stomach contents of the archaeocete Basilosaurus isis: Apex predator in oceans of the late Eocene 1☯ 2³ 3³ 3☯ Manja VossID *, Mohammed Sameh M. Antar , Iyad S. Zalmout , Philip D. Gingerich 1 Museum fuÈr Naturkunde Berlin, Leibniz-Institute for Evolution and Biodiversity Science, Berlin, Germany, 2 Department of Geology and Paleontology, Nature Conservation Sector, Egyptian Environmental Affairs Agency, Cairo, Egypt, 3 Museum of Paleontology, University of Michigan, Ann Arbor, Michigan, United States of America a1111111111 a1111111111 ☯ These authors contributed equally to this work. a1111111111 ³ These authors also contributed equally to this work. a1111111111 * [email protected] a1111111111 Abstract Apex predators live at the top of an ecological pyramid, preying on animals in the pyramid OPEN ACCESS below and normally immune from predation themselves. Apex predators are often, but not Citation: Voss M, Antar MSM, Zalmout IS, always, the largest animals of their kind. The living killer whale Orcinus orca is an apex pred- Gingerich PD (2019) Stomach contents of the ator in modern world oceans. Here we focus on an earlier apex predator, the late Eocene archaeocete Basilosaurus isis: Apex predator in oceans of the late Eocene. PLoS ONE 14(1): archaeocete Basilosaurus isis from Wadi Al Hitan in Egypt, and show from stomach con- e0209021. https://doi.org/10.1371/journal. tents that it fed on smaller whales (juvenile Dorudon atrox) and large fishes (Pycnodus pone.0209021 mokattamensis). Our observations, the first direct evidence of diet in Basilosaurus isis, con- Editor: Carlo Meloro, Liverpool John Moores firm a predator-prey relationship of the two most frequently found fossil whales in Wadi Al- University, UNITED KINGDOM Hitan, B.