The Deepest Ocean on Earth a Scientific Case for Establishing The
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Northern Marianas
Northern Marianas Overview: The Marianas is an archipelago made up by the summits of 15 volcanic mountains in the north-western Pacific Ocean. The Commonwealth of the Northern Mariana Islands (CNMI) is in political union with the United States. Territory: Includes 14 islands, including Saipan, Rota, and Tinian which are inhabited; and Farallon de Pajaros, Maug Islands, Pagan Island, Guguan, Agrihan Island, Sarigan Island, Anatahan Island, Asuncion Island and Farallon de Medinilla which are currently uninhabited due to volcanic activity. The southern islands are limestone with level terraces and fringing coral reefs; the northern islands are volcanic. Land: 477 sq km; Water: 0 sq km; Total: 477 sq km; Coast line: 1,482 km; Highest point: unnamed location on Agrihan 965 m. Location: Oceania, islands in the North Pacific Ocean, about three-quarters of the way from Hawaii to the Philippines. Latitude and Longitude: 15 1' 2" N, 145 4' 5" E. Time Zone: GMT +10 Total Land Area: 477 EEZ: 200 Climate: tropical marine; moderated by northeast trade winds, little seasonal temperature variation; dry season December to June, rainy season July to October. Natural Resources: arable land, fish. All the islands except Farallon de Medinilla and Urracas or Mangs (in the northern group) are more or less densely wooded, and the vegetation is luxuriant, much resembling that of the Carolines, and also of the Philippines, whence many species of plants have been introduced. Owing to the humidity of the soil cryptogams are numerous, as also most kinds of grasses. Agriculture is neglected, in spite of the exceptional advantages offered by the climate and soil. -
Billing Code 3510-JE DEPARTMENT of COMMERCE National Oceanic and Atmospheric Administration Availability of Final Evaluation
This document is scheduled to be published in the Federal Register on 10/09/2020 and available online at federalregister.gov/d/2020-22460, and on govinfo.gov Billing Code 3510-JE DEPARTMENT OF COMMERCE National Oceanic and Atmospheric Administration Availability of Final Evaluation Findings of State Coastal Programs and National Estuarine Research Reserves AGENCY: Office for Coastal Management (OCM), National Ocean Service (NOS), National Oceanic and Atmospheric Administration (NOAA), Department of Commerce (DOC). ACTION: Notice of availability of evaluation findings. SUMMARY: Notice is hereby given of the availability of final evaluation findings of state coastal programs and national estuarine research reserves. The NOAA Office for Coastal Management has completed review of the Coastal Zone Management Program evaluations for the states and territories of California, Commonwealth of the Northern Mariana Islands, Delaware, Georgia, Hawaii, Minnesota, Mississippi, Pennsylvania, Rhode Island, South Carolina, and Wisconsin. In addition, the NOAA Office for Coastal Management has completed review of the National Estuarine Research Reserve evaluations for Great Bay, Hudson River, Kachemak Bay, North Inlet-Winyah Bay, Old Woman Creek, and Rookery Bay, and Sapelo Island. Copies of these final evaluation findings may be downloaded at http://coast.noaa.gov/czm/evaluations/evaluation_findings/index.html or by submitting a written request to the person identified under FOR FURTHER INFORMATION CONTACT. FOR FURTHER INFORMATION CONTACT: Carrie Hall, Evaluator, Planning and Performance Measurement Program, Office for Coastal Management at [email protected] or (240) 530-0730. SUPPLEMENTARY INFORMATION: The states and territories were found to be implementing and enforcing their federally approved Coastal Zone Management Programs, addressing the national coastal management objectives identified in CZMA Section 303(2), and adhering to the programmatic terms of their financial assistance awards. -
38. Structural and Stratigraphic Evolution of the Sumisu Rift, Izu-Bonin Arc1
Taylor, B., Fujioka, K., et al., 1992 Proceedings of the Ocean Drilling Program, Scientific Results, Vol. 126 38. STRUCTURAL AND STRATIGRAPHIC EVOLUTION OF THE SUMISU RIFT, IZU-BONIN ARC1 Adam Klaus,2,3 Brian Taylor,2 Gregory F. Moore,2 Mary E. MacKay,2 Glenn R. Brown,4 Yukinobu Okamura,5 and Fumitoshi Murakami5 ABSTRACT The Sumisu Rift, which is ~ 120 km long and 30-50 km wide, is bounded to the north and south by structural and volcanic highs west of the Sumisu and Torishima calderas and longitudinally by curvilinear border fault zones with both convex and concave dips. The zigzag pattern of normal faults (average strikes N23°W and N5°W) indicates fault formation in orthorhombic symmetry in response to N76° ± 10°E extension, orthogonal to the volcanic arc. Three oblique transfer zones divide the rift along strike into four segments with different fault trends and uplift/subsidence patterns. Differential strain across the transfer zones is accommodated by interdigitating, rift-parallel faults and some cross-rift volcanism, rather than by strike- or oblique-slip faults. From estimates of extension (2-5 km), the age of the rift (~2 Ma), and the accelerating subsidence, we infer that the Sumisu Rift is in the early syn-rift stage of backarc basin formation. Following an early sag phase, a half graben formed with a synthetically faulted, structural rollover facing large-offset border fault zones. In the three northern rift segments, the largest faults are on the arc side and dip 60°-75°W, whereas in the southern segment they are on the west side and dip 25°-50°E. -
America&Apos;S Unknown Avifauna: the Birds of the Mariana Islands
ß ß that time have been the basis for con- America's unknown avifauna. siderable concern (Vincent, 1967) and indeed appear to be the basis for the the birds of inclusion of several Mariana birds in the U.S. Fish & Wildlife Service (1976) list of the Mariana Islands Endangered Species.These brief war- time observationswere important, but no significant investigationshave been conductedin the ensuingthirty yearsto "Probably no otherAmerican birds determine the extent to which the are aspoorly known as these." endemic avifauna of these islands may haverecovered. Importantly, no assess- mentshave been made of the impactof H. Douglas Pratt, Phillip L. Bruner the military's aerial planting of the exoticscrubby tree known as tangan- and Delwyn G. Berrett tangan, Leucaenaglauca, to promote revegetationafter the war. This 'treeis known as "koa haole" in Hawaii. restricted both in their time for bird ß ß announcesthe signthat greets observation and in their movements on v•sitors to Guam. Few Americans realize the islands. Their studies were made in authorsURING THEvisitedSUMMER the islandsOF1076the of that the nation's westernmost territories 1945 and 1946 when most of the Mari- Saipan,Tinian, Rota, and Guam, and m he across the International Date Line in anaswere just beginningto recoverfrom 1978 Bruner and Pratt returned to Sai- the far westernPacific. Guam, the larg- the ravagesof war (Baker, 1946).Never- pan and Guam. We havespent a total of est and southernmost of the Mariana theless, population estimates made at 38 man/dayson Saipan,four on Tinian, Islands,has been a United Statesposses- s•on since Spain surrendered her sov- & Agrihan ereigntyover the island at the end of the Sparash-AmericanWar. -
Vegetation Mapping of the Mariana Islands: Commonwealth of the Northern Mariana Islands and Territory of Guam
VEGETATION MAPPING OF THE MARIANA ISLANDS: COMMONWEALTH OF THE NORTHERN MARIANA ISLANDS AND TERRITORY OF GUAM NOVEMBER 2017 FINAL REPORT FRED AMIDON, MARK METEVIER1 , AND STEPHEN E. MILLER PACIFIC ISLAND FISH AND WILDLIFE OFFICE, U.S. FISH AND WILDLIFE SERVICE, HONOLULU, HI 1 CURRENT AGENCY: BUREAU OF LAND MANAGEMENT, MEDFORD, OR Photograph of Alamagan by Curt Kessler, USFWS. Mariana Island Vegetation Mapping Final Report November 2017 CONTENTS List of Figures ............................................................................................................................................................................ 3 List of Tables .............................................................................................................................................................................. 4 Abbreviations ............................................................................................................................................................................ 5 Summary ..................................................................................................................................................................................... 6 Introduction ............................................................................................................................................................................... 7 Description of Project Area ........................................................................................................................................... -
Philippine Sea Plate Inception, Evolution, and Consumption with Special Emphasis on the Early Stages of Izu-Bonin-Mariana Subduction Lallemand
Progress in Earth and Planetary Science Philippine Sea Plate inception, evolution, and consumption with special emphasis on the early stages of Izu-Bonin-Mariana subduction Lallemand Lallemand Progress in Earth and Planetary Science (2016) 3:15 DOI 10.1186/s40645-016-0085-6 Lallemand Progress in Earth and Planetary Science (2016) 3:15 Progress in Earth and DOI 10.1186/s40645-016-0085-6 Planetary Science REVIEW Open Access Philippine Sea Plate inception, evolution, and consumption with special emphasis on the early stages of Izu-Bonin-Mariana subduction Serge Lallemand1,2 Abstract We compiled the most relevant data acquired throughout the Philippine Sea Plate (PSP) from the early expeditions to the most recent. We also analyzed the various explanatory models in light of this updated dataset. The following main conclusions are discussed in this study. (1) The Izanagi slab detachment beneath the East Asia margin around 60–55 Ma likely triggered the Oki-Daito plume occurrence, Mesozoic proto-PSP splitting, shortening and then failure across the paleo-transform boundary between the proto-PSP and the Pacific Plate, Izu-Bonin-Mariana subduction initiation and ultimately PSP inception. (2) The initial splitting phase of the composite proto-PSP under the plume influence at ∼54–48 Ma led to the formation of the long-lived West Philippine Basin and short-lived oceanic basins, part of whose crust has been ambiguously called “fore-arc basalts” (FABs). (3) Shortening across the paleo-transform boundary evolved into thrusting within the Pacific Plate at ∼52–50 Ma, allowing it to subduct beneath the newly formed PSP, which was composed of an alternance of thick Mesozoic terranes and thin oceanic lithosphere. -
Ishikukaepsl10.Pdf
Earth and Planetary Science Letters 294 (2010) 111–122 Contents lists available at ScienceDirect Earth and Planetary Science Letters journal homepage: www.elsevier.com/locate/epsl Migrating shoshonitic magmatism tracks Izu–Bonin–Mariana intra-oceanic arc rift propagation O. Ishizuka a,b,⁎, M. Yuasa a, Y. Tamura b, H. Shukuno b, R.J. Stern c, J. Naka b, M. Joshima a, R.N. Taylor d a Institute of Geology and Geoinformation, Geological Survey of Japan/AIST, Central 7, 1-1-1, Higashi, Tsukuba, Ibaraki, 305-8567, Japan b IFREE, JAMSTEC, 2-15 Natsushima, Yokosuka, Kanagawa, 237-0061, Japan c Dept. of Geosciences, University of Texas at Dallas, Richardson TX 75083-0688, USA d National Oceanography Centre, Southampton, European Way, Southampton, SO14 3ZH, UK article info abstract Article history: The southernmost Izu–Bonin arc and northernmost Mariana arc are characterized by K-rich and shoshonitic Received 22 November 2009 lavas, referred to as the alkalic volcano province (AVP). These compositions are unusual for intra-oceanic arcs Received in revised form 6 March 2010 and the interpretation of the AVP is controversial. Rifting to form the Mariana Trough back-arc basin occurs Accepted 12 March 2010 just south of the AVP although back-arc seafloor spreading has not begun. Here we report the results of Available online 9 April 2010 dredge sampling of the West Mariana Ridge (WMR) in the region of rift propagation; this recovered Editor: R.W. Carlson exclusively medium K to shoshonitic basalts that show clear arc-like geochemical signatures. Ar–Ar ages of WMR shoshonitics systematically young northward. -
Microbiology of Seamounts Is Still in Its Infancy
or collective redistirbution of any portion of this article by photocopy machine, reposting, or other means is permitted only with the approval of The approval portionthe ofwith any articlepermitted only photocopy by is of machine, reposting, this means or collective or other redistirbution This article has This been published in MOUNTAINS IN THE SEA Oceanography MICROBIOLOGY journal of The 23, Number 1, a quarterly , Volume OF SEAMOUNTS Common Patterns Observed in Community Structure O ceanography ceanography S BY DAVID EmERSON AND CRAIG L. MOYER ociety. © 2010 by The 2010 by O ceanography ceanography O ceanography ceanography ABSTRACT. Much interest has been generated by the discoveries of biodiversity InTRODUCTION S ociety. ociety. associated with seamounts. The volcanically active portion of these undersea Microbial life is remarkable for its resil- A mountains hosts a remarkably diverse range of unusual microbial habitats, from ience to extremes of temperature, pH, article for use and research. this copy in teaching to granted ll rights reserved. is Permission S ociety. ociety. black smokers rich in sulfur to cooler, diffuse, iron-rich hydrothermal vents. As and pressure, as well its ability to persist S such, seamounts potentially represent hotspots of microbial diversity, yet our and thrive using an amazing number or Th e [email protected] to: correspondence all end understanding of the microbiology of seamounts is still in its infancy. Here, we of organic or inorganic food sources. discuss recent work on the detection of seamount microbial communities and the Nowhere are these traits more evident observation that specific community groups may be indicative of specific geochemical than in the deep ocean. -
Coral Reef Status Report for the Northern Mariana Islands
1 Coral reef condition: 20 8 A status report for the FAIR NORTHERN MARIANA ISLANDS Coral reefs are important Healthy coral reefs are among the most biologically diverse ecosystems on Earth, with high cultural and economic significance. Located in the western Pacific basin, the Commonwealth of the Northern Mariana Islands (CNMI) is made up of 14 islands extending over 600 kilometers. Coral reefs are important to the people of CNMI because they provide traditional and subsistence uses, production of commercial food products, recreational opportunities for a healthy tourist economy, and physical protection from storms. Culture and Food The indigenous ethnic groups of the Marianas, the Chamorro and Carolinian, are closely tied to the natural environment. Surveys indicate that about 96% of residents who go fishing, do so to feed their families. Ancient Chamorros and Carolinians were expert fishermen with inherent knowledge of harvesting reef fish species such as tàtaga (unicornfish), mafute’ (emperor), and palakse’ (parrotfish). Traditional fishing methods such as Trianni Mike spearfishing and talaya (throw-net) help preserve the cultural identity of the islands. The connection between coral reefs and society is integral as the reefs provide habitat for most species as well as numerous ecosystem services, including protection of culturally significant areas along the CNMI coastlines. Surveys of CNMI residents indicate that 91% of respondents agree that coral reefs are important to their culture (NOAA National Centers for Coastal Ocean Science 2018). Alexandra Fries Alexandra Tourism The economic importance of the CNMI coral reef ecosystem is significant. In addition to providing food, shelter, and cultural significance for the citizens of CNMI, the coral reefs generate revenue from tourists and recreational users that are attracted to the beauty of the coral and its inhabitants. -
COCONUT CRAB (Birgus Latro) SURVEYS on PAGAN, COMMONWEALTH of the NORTHERN MARIANAS ISLANDS
COCONUT CRAB (Birgus latro) SURVEYS ON PAGAN, COMMONWEALTH OF THE NORTHERN MARIANAS ISLANDS Prepared by: Scott Vogt Wildlife Biologist U.S. Navy Naval Facilities Engineering Far East Command Yokosuka, Japan December 2010 INTRODUCTION The coconut or robber crab (Birgus latro) has a wide distribution ranging from Eastern Africa, through the Indian Ocean islands to the Pacific Ocean islands (Fletcher and Amos, 1994). Due to its large size, ease of collection and palatable flesh, the coconut crab is often over-harvested when it occurs in the vicinity of human habitation. The Mariana Islands are no exception and this species is heavily harvested as a cultural resource. Surveys on Guam (USFWS, 2001), Saipan (Kessler, 2006) and Tinian (U.S. Navy, 2008) have documented over-harvested populations. Coconut crabs are a type of hermit crab; however they abandon the necessity of residing in a discarded snail shell at a small size and go through life with no added protection other than their own carapace. They are the largest land dwelling invertebrate in the world and can reach a weight in excess of 5kg. Coconut crabs breed on land but the female releases the eggs in the ocean where they immediately hatch. The oceanic larval stage lasts 2-3 weeks (Fletcher and Amos, 1994). Once on land the growth rate is slow and it is estimated to take 8-10 years to reach the CNMI legal size limit of 3 inches (76mm) across the back (Brown and Fielder, 1991). On the southern islands (Rota, Saipan Tinian and Aguiguan), the Commonwealth of the Northern Mariana Islands – Division of Fish & Wildlife has established a legal crab hunting season from September 15 - November 15. -
NOAA's National Ocean Service: Estuaries
NOAA's National Ocean Service: Estuaries NOS home NOS education home site index Welcome to Estuaries This site NOAA Estuaries Roadmap Estuaries are bodies of water and their Estuaries Lesson Plans surrounding coastal habitats typically found where rivers meet the sea. Estuaries harbor unique plant and animal communities because their waters are brackish—a mixture of fresh water draining from the land and salty Welcome seawater. What is an Estuary? Estuaries are some of the most productive ecosystems in the world. Many animal species Why Are Estuaries rely on estuaries for food and as places to nest Important? and breed. Humans communities also rely on estuaries for food, recreation and jobs. º Economy & Environment Of the 32 largest cities in the world, 22 are located on estuaries (Ross, 1995). Not º Ecosystem Services surprisingly, human activities have led to a decline in the health of estuaries, making them Classifying Estuaries one of the most threatened ecosystems on Estuarine habitats are typically found where Earth. NOAA's National Estuarine Research rivers meet the sea. Mouse over the image º Geology Reserve System (NERRS), in partnership with to see some of the estuarine areas highlighted coastal states, monitors the health of in this tutorial. Click on image for more details and a larger image. º Water Circulation estuaries, educates the public about these ecosystems, and helps communities manage Estuarine Habitats their coastal resources. Adaptations to Life in the Estuary Disturbances to Estuaries º Natural º Human Monitoring Estuaries The Future References Estuaries are both beautiful and ecologically New York City, with a population of over eight bountiful. -
Terrestrial Arthropod Surveys on Pagan Island, Northern Marianas
Terrestrial Arthropod Surveys on Pagan Island, Northern Marianas Neal L. Evenhuis, Lucius G. Eldredge, Keith T. Arakaki, Darcy Oishi, Janis N. Garcia & William P. Haines Pacific Biological Survey, Bishop Museum, Honolulu, Hawaii 96817 Final Report November 2010 Prepared for: U.S. Fish and Wildlife Service, Pacific Islands Fish & Wildlife Office Honolulu, Hawaii Evenhuis et al. — Pagan Island Arthropod Survey 2 BISHOP MUSEUM The State Museum of Natural and Cultural History 1525 Bernice Street Honolulu, Hawai’i 96817–2704, USA Copyright© 2010 Bishop Museum All Rights Reserved Printed in the United States of America Contribution No. 2010-015 to the Pacific Biological Survey Evenhuis et al. — Pagan Island Arthropod Survey 3 TABLE OF CONTENTS Executive Summary ......................................................................................................... 5 Background ..................................................................................................................... 7 General History .............................................................................................................. 10 Previous Expeditions to Pagan Surveying Terrestrial Arthropods ................................ 12 Current Survey and List of Collecting Sites .................................................................. 18 Sampling Methods ......................................................................................................... 25 Survey Results ..............................................................................................................