Classification of Wetlands and Deepwater Habitats of the United States
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Classification of Wetlands and Deepwater Habitats of the United States
Pfego-/6^7fV SDMS DocID 463450 ^7'7/ Biological Services Program \ ^ FWS/OBS-79/31 DECEMBER 1979 Superfund Records Center ClassificaHioFF^^^ V\Aetlands and Deepwater Habitats of the United States KPHODtKtD BY NATIONAL TECHNICAL INFOR/V^ATION SERVICE U.S. IKPARTMEN TOF COMMERCt SPRINGMflO, VA. 22161 Fish and Wildlife Service U.S. Department of the Interior (USDI) C # The Biological Services Program was established within the U.S. Fish . and Wildlife Service to supply scientific information and methodologies on key environmental issues which have an impact on fish and wildlife resources and their supporting ecosystems. The mission of the Program is as follows: 1. To strengthen the Fish and Wildlife Service in its role as a primary source of Information on natural fish and wildlife resources, par ticularly with respect to environmental impact assessment. 2. To gather, analyze, and present information that will aid decision makers in the identification and resolution of problems asso ciated with major land and water use changes. 3. To provide better ecological information and evaluation for Department of the Interior development programs, such as those relating to energy development. Information developed by the Biological Services Program is intended for use in the planning and decisionmaking process, to prevent or minimize the impact of development on fish and wildlife. Biological Services research activities and technical assistance services are based on an analysis of the issues, the decisionmakers involved and their information neeids, and an evaluation of the state^f-the-art to Identify information gaps and determine priorities. This Is a strategy to assure that the products produced and disseminated will be timely and useful. -
Appendix 1 Table A1
OIK-00806 Kordas, R. L., Dudgeon, S., Storey, S., and Harley, C. D. G. 2014. Intertidal community responses to field-based experimental warming. – Oikos doi: 10.1111/oik.00806 Appendix 1 Table A1. Thermal information for invertebrate species observed on Salt Spring Island, BC. Species name refers to the species identified in Salt Spring plots. If thermal information was unavailable for that species, information for a congeneric from same region is provided (species in parentheses). Response types were defined as; optimum - the temperature where a functional trait is maximized; critical - the mean temperature at which individuals lose some essential function (e.g. growth); lethal - temperature where a predefined percentage of individuals die after a fixed duration of exposure (e.g., LT50). Population refers to the location where individuals were collected for temperature experiments in the referenced study. Distribution and zonation information retrieved from (Invertebrates of the Salish Sea, EOL) or reference listed in entry below. Other abbreviations are: n/g - not given in paper, n/d - no data for this species (or congeneric from the same geographic region). Invertebrate species Response Type Temp. Medium Exposure Population Zone NE Pacific Distribution Reference (°C) time Amphipods n/d for NE low- many spp. worldwide (Gammaridea) Pacific spp high Balanus glandula max HSP critical 33 air 8.5 hrs Charleston, OR high N. Baja – Aleutian Is, Berger and Emlet 2007 production AK survival lethal 44 air 3 hrs Vancouver, BC Liao & Harley unpub Chthamalus dalli cirri beating optimum 28 water 1hr/ 5°C Puget Sound, WA high S. CA – S. Alaska Southward and Southward 1967 cirri beating lethal 35 water 1hr/ 5°C survival lethal 46 air 3 hrs Vancouver, BC Liao & Harley unpub Emplectonema gracile n/d low- Chile – Aleutian Islands, mid AK Littorina plena n/d high Baja – S. -
Grade 3 Unit 2 Overview Open Ocean Habitats Introduction
G3 U2 OVR GRADE 3 UNIT 2 OVERVIEW Open Ocean Habitats Introduction The open ocean has always played a vital role in the culture, subsistence, and economic well-being of Hawai‘i’s inhabitants. The Hawaiian Islands lie in the Pacifi c Ocean, a body of water covering more than one-third of the Earth’s surface. In the following four lessons, students learn about open ocean habitats, from the ocean’s lighter surface to the darker bottom fl oor thousands of feet below the surface. Although organisms are scarce in the deep sea, there is a large diversity of organisms in addition to bottom fi sh such as polycheate worms, crustaceans, and bivalve mollusks. They come to realize that few things in the open ocean have adapted to cope with the increased pressure from the weight of the water column at that depth, in complete darkness and frigid temperatures. Students fi nd out, through instruction, presentations, and website research, that the vast open ocean is divided into zones. The pelagic zone consists of the open ocean habitat that begins at the edge of the continental shelf and extends from the surface to the ocean bottom. This zone is further sub-divided into the photic (sunlight) and disphotic (twilight) zones where most ocean organisms live. Below these two sub-zones is the aphotic (darkness) zone. In this unit, students learn about each of the ocean zones, and identify and note animals living in each zone. They also research and keep records of the evolutionary physical features and functions that animals they study have acquired to survive in harsh open ocean habitats. -
Vegetative Ecology of a Montane Mire, Crater Lake National
AJ ABSTRACT OF THE THESIS OF Susan Cornelia Seyer for the degree of Master of Science in Botany and Plant Pathology presented on December 14, 1979 Title: VEGETATIVE ECOLOGY OF A MONTANE MIRE, CRATER LAKE NATIONAL PARK, OREGON Redacted for Privacy Abstract approved: Jerry F. Franklin Mires, or peat-producing ecosystems, dominated by sedges, shrubs, and brown mosses, are common features in Cascade subalpine regions, occurring where moisture accumulates in small basins or on poorly-drained slopes. Although descriptions and classifications have been developed for mire vegetation in much of the world, there is little information of even a descriptive nature for these montane mires in Oregon and Washington. This thesis reports on phytosocia- logical structure, env'ironental relations, and successional trends in one such mire in the Oregon Cascade mountains. To characterize the general phytosociological structure of the mire vegetation at Sphagnum Bog, Crater Lake National Park, quantitative species cover data were used in conjunction with a Braun-Blanquet tabular analysis and two-dimensional stand ordinations, reciprocal averaging and a Bray-Curtis polar ordination. Defined community types correspond to physiognomic types as follows: Carex rostrata (reedswamp); Eleocharis pauciflora-Carex limosa, Eleocharis pauciflora/bryophytes (low sedge fens); Carex sichensis (tall sedge fen); Vaccinium/ Aulacomnium palustre, Vaccinium occidentala/Carex sitchensis (shrub thickets; Alnus incana/Brachythacium sp. and Salix barclayi (marginal carrs).Phases were defined when appropriate. A vegetation map was made to illustrate the locations and extent of the variouscommunities. Comparisons with other montane mires in thearea determined that the physiognomic units defined are repeatable when appropriate habitat conditions are present, and that they usually includemany of the same characteristic species, the dominant mosses being particularly constant. -
Does the Acorn Barnacle Balanus Glandula Exhibit Predictable Gradients in Metabolic Performance Across the Intertidal Zone?
Warren J. Baker Endowment for Excellence in Project-Based Learning Robert D. Koob Endowment for Student Success FINAL REPORT Final reports will be published on the Cal Poly Digital Commons website(http://digitalcommons.calpoly.edu). I. Project Title Does the acorn barnacle Balanus glandula exhibit predictable gradients in metabolic performance across the intertidal zone? II. Project Completion Date 2/2019 III. Student(s), Department(s), and Major(s) (1) Kali Horn, Biological Sciences Department, M.S. Biological Sciences IV. Faculty Advisor and Department Kristin Hardy, Biological Sciences Department V. Cooperating Industry, Agency, Non-Profit, or University Organization(s) NA VI. Executive Summary Using funding from the Baker-Koob endowment, I successfully completed an experiment looking at metabolic variation in the common acorn barnacle, Balanus glandula, across tidal heights. We characterized the temperature profile across the zone as well to have data explicitly describing the abiotic variability from the upper intertidal zone to the low. Myself and many undergraduates collected barnacles from the top middle and bottom of the B.glandula distribution and ran the individuals through a suite of experiments to characterize the ‘metabolic phenotype’ . We defined the metabolic phenotype with a comprehensive suite of biochemical (e.g., citrate synthase and lactate dehydrogenase activity), physiological (VO2, aerobic scope) and behavioral (feeding rate) indices of metabolism. After removal from the intertidal zone, barnacles were placed in our intermittent respirometry system to calculate an average oxygen consumption rate over a 24h period. During the first two hours of the experiment, I conducted a behavioral observation to determine overall activity and feeding rate. -
Fossil Mosses: What Do They Tell Us About Moss Evolution?
Bry. Div. Evo. 043 (1): 072–097 ISSN 2381-9677 (print edition) DIVERSITY & https://www.mapress.com/j/bde BRYOPHYTEEVOLUTION Copyright © 2021 Magnolia Press Article ISSN 2381-9685 (online edition) https://doi.org/10.11646/bde.43.1.7 Fossil mosses: What do they tell us about moss evolution? MicHAEL S. IGNATOV1,2 & ELENA V. MASLOVA3 1 Tsitsin Main Botanical Garden of the Russian Academy of Sciences, Moscow, Russia 2 Faculty of Biology, Lomonosov Moscow State University, Moscow, Russia 3 Belgorod State University, Pobedy Square, 85, Belgorod, 308015 Russia �[email protected], https://orcid.org/0000-0003-1520-042X * author for correspondence: �[email protected], https://orcid.org/0000-0001-6096-6315 Abstract The moss fossil records from the Paleozoic age to the Eocene epoch are reviewed and their putative relationships to extant moss groups discussed. The incomplete preservation and lack of key characters that could define the position of an ancient moss in modern classification remain the problem. Carboniferous records are still impossible to refer to any of the modern moss taxa. Numerous Permian protosphagnalean mosses possess traits that are absent in any extant group and they are therefore treated here as an extinct lineage, whose descendants, if any remain, cannot be recognized among contemporary taxa. Non-protosphagnalean Permian mosses were also fairly diverse, representing morphotypes comparable with Dicranidae and acrocarpous Bryidae, although unequivocal representatives of these subclasses are known only since Cretaceous and Jurassic. Even though Sphagnales is one of two oldest lineages separated from the main trunk of moss phylogenetic tree, it appears in fossil state regularly only since Late Cretaceous, ca. -
Contemporary Status, Distribution, and Trends of Mixedwoods in the Northern United States1 Lance A
881 ARTICLE Contemporary status, distribution, and trends of mixedwoods in the northern United States1 Lance A. Vickers, Benjamin O. Knapp, John M. Kabrick, Laura S. Kenefic, Anthony W. D’Amato, Christel C. Kern, David A. MacLean, Patricia Raymond, Kenneth L. Clark, Daniel C. Dey, and Nicole S. Rogers Abstract: As interest in managing and maintaining mixedwood forests in the northern United States (US) grows, so does the importance of understanding their abundance and distribution. We analyzed Forest Inventory and Analysis data for insights into mixedwood forests spanning 24 northern US states from Maine south to Maryland and westward to Kansas and North Dakota. Mixedwoods, i.e., forests with both hardwoods and softwoods present but neither exceeding 75%–80% of composition, comprise more than 19 million hectares and more than one-quarter of the northern US forest. They are most common in the Adirondack – New England, Laurentian, and Northeast ecological provinces but also occur elsewhere in hardwood-dominated ecological provinces. These mixtures are common even within forest types nominally categorized as either hardwood or softwood. The most common hardwoods within those mixtures were species of Quercus and Acer,and the most common softwoods were species of Pinus, Tsuga,andJuniperus. Although mixedwoods exhibited stability in total area during our analysis period, hardwood saplings were prominent, suggesting widespread potential for eventual shifts to hardwood dominance in the absence of disturbances that favor regeneration of the softwood component. Our analyses sug- gest that while most mixedwood plots remained mixedwoods, harvesting commonly shifts mixedwoods to either hard- wood- or softwood-dominated cover types, but more specific information is needed to understand the causes of these shifts. -
Western Samoa
A Directory of Wetlands in Oceania In: Scott, D.A. (ed.) 1993. A Directory of Wetlands in Oceania. IWRB, Slimbridge, U.K. and AWB, Kuala Lumpur, Malaysia. A Directory of Wetlands in Oceania WESTERN SAMOA INTRODUCTION by Cedric Schuster Department of Lands and Environment Area: 2,935 sq.km. Population: 170,000. Western Samoa is an independent state in the South Pacific situated between latitudes 13° and 14°30' South and longitudes 171° and 173° West, approximately 1,000 km northeast of Fiji. The state comprises two main inhabited islands, Savai'i (1,820 sq.km) and Upolu (1,105 sq.km), and seven islets, two of which are inhabited. Western Samoa is an oceanic volcanic archipelago that originated in the Pliocene. The islands were formed in a westerly direction with the oldest eruption, the Fagaloa volcanics, on the eastern side. The islands are still volcanically active, with the last two eruptions being in 1760 and 1905-11 respectively. Much of the country is mountainous, with Mount Silisili (1,858 m) on Savai'i being the highest point. Western Samoa has a wet tropical climate with temperatures ranging between 17°C and 34°C and an average temperature of 26.5°C. The temperature difference between the rainy season (November to March) and the dry season (May to October) is only 2°C. Rainfall is heavy, with a minimum of 2,000 mm in all places. The islands are strongly influenced by the trade winds, with the Southeast Trades blowing 82% of the time from April to October and 54% of the time from May to November. -
COURSE NAME CITY STATE ALBERTVILLE GOLF & COUNTRY CLUB Albertville Alabama MOUNTAIN VIEW GOLF COURSE Alden Alabama LAKEWINDS
COURSE NAME CITY STATE ALBERTVILLE GOLF & COUNTRY CLUB Albertville Alabama MOUNTAIN VIEW GOLF COURSE Alden Alabama LAKEWINDS GOLF COURSE Alex City Alabama WILLOW POINT COUNTRY CLUB Alex City Alabama ALPINE BAY GOLF CLUB Alpine Alabama WHIPPORWHILL GOLF COURSE Altoona Alabama ANDALUSIA COUNTRY CLUB Andalusia Alabama EVANS BARNES GOLF COURSE Andalusia Alabama ANDERSON CREEK GOLF COURSE Anderson Alabama ANNISTON COUNTRY CLUB Anniston Alabama ANNISTON MUNICIPAL GOLF COURSE Anniston Alabama B & J GOLF CENTER Anniston Alabama CANE CREEK GOLF COURSE Anniston Alabama CIDER RIDGE GOLF CLUB Anniston Alabama INDIAN OAKS GOLF CLUB Anniston Alabama PINE HILL COUNTRY CLUB Anniston Alabama BROOKSIDE GOLF COURSE Arab Alabama TWIN LAKES GOLF CLUB Arab Alabama UNION SPRINGS COUNTRY CLUB Armstrong Alabama CLAY COUNTY PUBLIC GOLF COURSE Ashland Alabama ATHENS GOLF & COUNTRY CLUB Athens Alabama CANEBRAKE GOLF CLUB Athens Alabama CHRISWOOD GOLF COURSE Athens Alabama SOUTHERN GALES GOLF CLUB Athens Alabama WOODLAND GOLF COURSE Athens Alabama ATMORE COUNTRY CLUB Atmore Alabama WILLS CREEK COUNTRY CLUB Attalla Alabama AUBURN LINKS AT MILL CREEK Auburn Alabama INDIAN PINES RECREATIONAL AUTHORITY Auburn Alabama MOORE'S MILL GOLF CLUB Auburn Alabama MOORE'S MILL GOLF CLUB Auburn Alabama PIN OAKS GOLF CLUB Auburn Alabama EUFAULA COUNTRY CLUB Bakerhill Alabama LAKEPOINT RESORT GOLF COURSE Bakerhill Alabama RED EAGLE GOLF COURSE Bakerhill Alabama WARRIOR POINT GOLF CLUB Barney Alabama HOLLY HILLS COUNTRY CLUB Bay Minette Alabama BENT BROOK GOLF COURSE Bess Alabama -
Town of Seneca
TOWN OF BRISTOL Inventory of Land Use and Land Cover Prepared for: Ontario County Water Resources Council 20 Ontario Street, 3rd Floor Canandaigua, New York 14424 and Town of Bristol 6740 County Road 32 Canandaigua, New York 14424 Prepared by: Dr. Bruce Gilman Department of Environmental Conservation and Horticulture Finger Lakes Community College 3325 Marvin Sands Drive Canandaigua, New York 14424-8395 2020 Cover image: Ground level view of a perched swamp white oak forest community (S1S2) surrounding a shrub swamp that was discovered and documented on Johnson Hill north of Dugway Road. This forest community type is rare statewide and extremely rare locally, and harbors a unique assemblage of uncommon plant species. (Image by the Bruce Gilman). Acknowledgments: For over a decade, the Ontario County Planning Department has supported a working partnership between local towns and the Department of Environmental Conservation and Horticulture at Finger Lakes Community College that involves field research, ground truthing and digital mapping of natural land cover and cultural land use patterns. Previous studies have been completed for the Canandaigua Lake watershed, the southern Honeoye Valley, the Honeoye Lake watershed, the complete Towns of Canandaigua, Gorham, Richmond and Victor, and the woodlots, wetlands and riparian corridors in the Towns of Seneca, Phelps and Geneva. This report summarizes the latest land use/land cover study conducted in the Town of Bristol. The final report would not have been completed without the vital assistance of Terry Saxby of the Ontario County Planning Department. He is gratefully thanked for his assistance with landowner information, his patience as the fieldwork was slowly completed, and his noteworthy help transcribing the field maps to geographic information system (GIS) shape files. -
PLTA-0103 Nature Conservancy 3/19/04 4:00 PM Page 1
PLTA-0103 Nature Conservancy 3/19/04 4:00 PM Page 1 ............................................................. Pennsylvania’s Land Trusts The Nature Conservancy About Land Trusts Conservation Options Conserving our Commonwealth Pennsylvania Chapter Land trusts are charitable organizations that conserve land Land trusts and landowners as well as government can by purchasing or accepting donations of land and conservation access a variety of voluntary tools for conserving special ................................................................ easements. Land trust work is based on voluntary agreements places. The basic tools are described below. The privilege of possessing Produced by the the earth entails the Pennsylvania Land Trust Association with landowners and creating projects with win-win A land trust can acquire land. The land trust then responsibility of passing it on, working in partnership with outcomes for communities. takes care of the property as a wildlife preserve, the better for our use, Pennsylvania’s land trusts Nearly a hundred land trusts work to protect important public recreation area or other conservation purpose. not only to immediate posterity, but to the unknown future, with financial support from the lands across Pennsylvania. Governed by unpaid A landowner and land trust may create an the nature of which is not William Penn Foundation, Have You Been to the Bog? boards of directors, they range from all-volunteer agreement known as a conservation easement. given us to know. an anonymous donor and the groups working in a single municipality The easement limits certain uses on all or a ~ Aldo Leopold Pennsylvania Department of Conservation n spring days, the Tannersville Cranberry Bog This kind of wonder saved the bog for today and for to large multi-county organizations with portion of a property for conservation and Natural Resources belongs to fourth-graders. -
Great Lakes Shipping Study
UNCLASSIFIED Great Lakes Shipping Study This page intentionally left blank. National Protection and Programs Directorate Integrated Analysis Task Force Homeland Infrastructure Threat and Risk Analysis Center January 13, 2014 UNCLASSIFIED Executive Summary The Great Lakes St. Lawrence Seaway (GLSLS) system is a vast, interconnected series of navigable waterways, with intersecting modes of transportation and landscapes. The enormity and importance of the GLSLS system cannot be overstated as the region is critically dependent upon it; therefore, it is vital to understand the nature of the system, the industries that rely upon it, its economic impact, and major commodities that flow through the GLSLS. This study provides an overview of the GLSLS system, focusing on geography, system infrastructure, economic and employment data derived from the GLSLS, and detailed analysis of three key commodities: iron ore, steel, and refined petroleum products. The GLSLS, which borders eight states and spans 2,300 miles, comprises Lake Superior, Lakes Michigan and Huron, Lake Erie, Montreal-Lake Ontario, and the Saint Lawrence Seaway, as well as the channels that connect these navigable sections. U.S. and Canadian companies and industries rely on the GLSLS for low-cost, long-distance transportation of raw materials and finished goods. In 2010, U.S. and Canadian companies that depend on the GLSLS for moving cargo reported revenues of over $30 billion, more than half of which was generated in the United States. The GLSLS is also responsible for the creation of hundreds of thousands of jobs, providing direct employment for mariners, many types of port employees, and support positions within the companies, as well as creating indirect jobs that result from the spending power of the previously mentioned workers.