Northward Spread of Marine Nonindigenous Species Along Western North America: Forecasting Risk of Colonization in Alaskan Waters Using Environmental Niche Modeling
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Salmon Decline in Western North America: Historical Context
Salmon Decline in Western North America: Historical Context Robert T. Lackey Department of Fisheries and Wildlife Oregon State University Corvallis, Oregon 97331 Email: [email protected] Phone: (541) 737-0569 Web: http://fw.oregonstate.edu/content/robert-lackey Citation: Lackey, Robert T. 2009. Salmon in Western North America: Historical Context. In: Encyclopedia of Earth. Eds. Cutler J. Cleveland (Washington, DC, Environmental Information Coalition, National Council for Science and the Environment). http://www.eoearth.org/article/Salmon_in_western_North_America:_assessing_the_future Introduction Wild salmon in California, Oregon, Washington, Idaho, and southern British Columbia have been on a 160 year downward trend and are now at very low levels. Efforts to reverse the decline have been extensive and expensive, but have not met with much success. Salmon in the lower 48 states are well on their way to attaining a status enjoyed by some of their notable brethren — wolves, condors, grizzles, bison — wild animals that are unlikely to disappear entirely, but struggle to hang on as remnants of once flourishing species in small portions of their original range. A few entrepreneurs may be marketing the superior taste of buffalo burgers, but wild bison today are found only in Yellowstone and a few other refuges. This prediction will not surprise anyone familiar with the state of wild salmon runs. Consider the following facts: in California, Oregon, Idaho, Washington, and southern British Columbia, many runs are reduced to less than 10% of their historical numbers; some have disappeared. Many salmon runs are dominated by hatchery-bred fish. Even for the Columbia River, once the mightiest salmon-producing river south of Canada, over 80% of the total run is now comprised of hatchery-bred fish. -
Kinematics of the Northern Walker Lane: an Incipient Transform Fault Along the Pacific–North American Plate Boundary
Kinematics of the northern Walker Lane: An incipient transform fault along the Paci®c±North American plate boundary James E. Faulds Christopher D. Henry Nevada Bureau of Mines and Geology, MS 178, University of Nevada, Reno, Nevada 89557, USA Nicholas H. Hinz ABSTRACT GEOLOGIC SETTING In the western Great Basin of North America, a system of dextral faults accommodates As western North America has evolved 15%±25% of the Paci®c±North American plate motion. The northern Walker Lane in from a convergent to a transform margin in northwest Nevada and northeast California occupies the northern terminus of this system. the past 30 m.y., the northern Walker Lane has This young evolving part of the plate boundary offers insight into how strike-slip fault undergone widespread volcanism and tecto- systems develop and may re¯ect the birth of a transform fault. A belt of overlapping, left- nism. Tertiary volcanic strata include 31±23 stepping dextral faults dominates the northern Walker Lane. Offset segments of a W- Ma ash-¯ow tuffs associated with the south- trending Oligocene paleovalley suggest ;20±30 km of cumulative dextral slip beginning ward-migrating ``ignimbrite ¯are up,'' 22±5 ca. 9±3 Ma. The inferred long-term slip rate of ;2±10 mm/yr is compatible with global Ma calc-alkaline intermediate-composition positioning system observations of the current strain ®eld. We interpret the left-stepping rocks related to the ancestral Cascade arc, and faults as macroscopic Riedel shears developing above a nascent lithospheric-scale trans- 13 Ma to present bimodal rocks linked to Ba- form fault. -
Mild Osmotic Stress in Intertidal Gastropods Littorina Saxatilis and Littorina Obtusata (Mollusca: Caenogastropoda): a Proteomic Analysis
CORE Metadata, citation and similar papers at core.ac.uk Provided by Saint PetersburgFULL State University COMMUNICATION PHYSIOLOGY Mild osmotic stress in intertidal gastropods Littorina saxatilis and Littorina obtusata (Mollusca: Caenogastropoda): a proteomic analysis Olga Muraeva1, Arina Maltseva1, Marina Varfolomeeva1, Natalia Mikhailova1,2, and Andrey Granovitch1 1 Department of Invertebrate Zoology, Faculty of Biology, Saint Petersburg State University, Universitetskaya nab. 7–9, St. Petersburg, 199034, Russian Federation; 2 Center of Cell Technologies, Institute of Cytology RAS, Tikhoretsky prospect, 4, St. Petersburg, 194064, Russian Federation Address correspondence and requests for materials to Arina Maltseva, [email protected] Abstract Salinity is a crucial abiotic environmental factor for marine animals, affecting their physiology and geographic ranges. Deviation of environmental salin- ity from the organismal optimum range results in an osmotic stress in osmo- conformers, which keep their fluids isotonic to the environment. The ability to overcome such stress is critical for animals inhabiting areas with considerable salinity variation, such as intertidal areas. In this study, we compared the reac- tion to mild water freshening (from 24 to 14 ‰) in two related species of inter- tidal snails, Littorina saxatilis and L. obtusata, with respect to several aspects: survival, behavior and proteomic changes. Among these species, L. saxatilis is Citation: Muraeva, O., Maltseva, A., Varfolomeeva, M., Mikhailova, N., more tolerant to low salinity and survives in estuaries. We found out that the Granovitch, A. 2017. Mild osmotic response of these species was much milder (with no mortality or isolation re- stress in intertidal gastropods Littorina saxatilis and Littorina obtusata (Mollusca: action observed) and involved weaker proteomic changes than during acute Caenogastropoda): a proteomic analysis. -
Persistence of Pressure Patterns Over North America and the North Pacific Since AD 1500
ARTICLE Received 13 Jan 2014 | Accepted 5 Aug 2014 | Published 11 Sep 2014 DOI: 10.1038/ncomms5912 Persistence of pressure patterns over North America and the North Pacific since AD 1500 Erika K. Wise1 & Matthew P. Dannenberg1 Changes in moisture delivery to western North America are largely controlled by interrelated, synoptic-scale atmospheric pressure patterns. Long-term records of upper-atmosphere pressure and related circulation patterns are needed to assess potential drivers of past severe droughts and evaluate how future climate changes may impact hydroclimatic systems. Here we develop a tree-ring-based climate field reconstruction of cool-season 500 hPa geopotential height on a 2° Â 2° grid over North America and the North Pacific to AD 1500 and examine the frequency and persistence of preinstrumental atmospheric pressure patterns using Self-Organizing Maps. Our results show extended time periods dominated by a set of persistent upper-air pressure patterns, providing insight into the atmospheric conditions leading to periods of sustained drought and pluvial periods in the preinstrumental past. A striking shift from meridional to zonal flow occurred at the end of the Little Ice Age and was sustained for several decades. 1 Department of Geography, University of North Carolina at Chapel Hill, Chapel Hill, North Carolina 27599, USA. Correspondence and requests for materials should be addressed to E.K.W. (email: [email protected]). NATURE COMMUNICATIONS | 5:4912 | DOI: 10.1038/ncomms5912 | www.nature.com/naturecommunications 1 & 2014 Macmillan Publishers Limited. All rights reserved. ARTICLE NATURE COMMUNICATIONS | DOI: 10.1038/ncomms5912 he position of the mid-latitude storm track, which Pressure anomalies in the upper atmosphere can persist for represents the primary large-scale moisture-delivery path- years to decades and influence temperature, precipitation and Tway to North America, is closely connected to the strength storm tracks over North America9. -
Chapter 15 Comparative Phylogeography of North- Western North America: a Synthesis
Chapter 15 Comparative phylogeography of north- western North America: a synthesis S. J. Brunsfeld,* J. Sullivan,†D. E. Soltis‡and P. S. Soltis§ Introduction Phylogeography is concerned with the principles and processes that determine the geographic distributions of genealogical lineages, within and among closely related species (Avise et al. 1987;Avise 2000).Although this field of study is very new (only a little more than a decade has passed since the term ‘phylogeography’was first coined; see Avise et al. 1987),the scientific literature in this research area is now voluminous. To date, most phylogeographic investigations of natural populations have focused on muticellular animals (Hewitt 1993; Patton et al. 1994; daSilva & Patton 1998; Eizirik et al. 1998;Avise 2000; Hewitt 2000; Schaal & Olsen 2000; Sullivan et al. 2000). This bias is due in large part to the ready availability of population-level genetic markers afforded by the animal mitochondrial genome. The more slowly evolving chloroplast genome,in contrast,often does not provide sufficient variation to reconstruct phylogeny at the populational level (Soltis et al. 1997; Schaal et al. 1998; Schaal & Olsen 2000). Phylogeographic data have accumulated so rapidly for animal taxa that it has been possible to compare phylogeographic structure among codistributed species. In fact, one of the most profound recent contributions of molecular phylogeography is the construction of regional phylogeographic perspec- tives that permit comparisons of phylogeographic structure among codistributed species, and subsequent integration of genealogical data with independent biogeo- graphic and systematic data. Probably the best-known regional phylogeographic analysis for North America involves animals from the southeastern USA (reviewed in Avise 2000). -
Geologic, Climatic, and Vegetation History of California
GEOLOGIC, CLIMATIC, AND VEGETATION HISTORY OF CALIFORNIA Constance I. Millar I ntroduction The dawning of the “Anthropocene,” the era of human-induced climate change, exposes what paleoscientists have documented for decades: earth’s environment—land, sea, air, and the organisms that inhabit these—is in a state of continual flux. Change is part of global reality, as is the relatively new and disruptive role humans superimpose on environmental and climatic flux. Historic dynamism is central to understanding how plant lineages exist in the present—their journey through time illuminates plant ecology and diversity, niche preferences, range distributions, and life-history characteristics, and is essential grounding for successful conservation planning. The editors of the current Manual recognize that the geologic, climatic, and vegetation history of California belong together as a single story, reflecting their interweaving nature. Advances in the sci- ences of geology, climatology, and paleobotany have shaken earlier interpretations of earth’s history and promoted integrated understanding of the origins of land, climate, and biota of western North America. In unraveling mysteries about the “what, where, and when” of California history, the respec- tive sciences have also clarified the “how” of processes responsible for geologic, climatic, and vegeta- tion change. This narrative of California’s prehistory emphasizes process and scale while also portraying pic- tures of the past. The goal is to foster a deeper understanding of landscape dynamics of California that will help toward preparing for changes coming in the future. This in turn will inform meaningful and effective conservation decisions to protect the remarkable diversity of rock, sky, and life that is our California heritage. -
Lead-Alpha Ages of the Mesozoic Batholiths of Western North America
Lead-Alpha Ages of the Mesozoic Batholiths of Western North America £y ESPER S. LARSEN, Jr., DAVID GOTTFRIED, HOWARD W. JAFFE, and CLAUDE L. WARING INVESTIGATIONS OF WESTERN BATHOLITHS GEOLOGICAL SURVEY BULLETIN 1070-B This report concerns work done on behalf of the U. S. Atomic Energy Commission and is published with the permission of the Commission UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1958 UNITED STATES DEPARTMENT OF THE INTERIOR FRED A. SEATON, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director Larsen, Esper Signius, 1879- Lead-alpha ages of the Mesozoic batholiths of western North America. By Esper S. Larsen, Jr. [and others] Washington, U. S. Govt. Print. Off., 1958» iv, 35-62 p. map, diagr., tables. 23 cm. (U. S. Geological Survey. Bulletin 1070-B. Investigations of western batholiths) Bibliography : p. 61-62i 1. Geology, Stratigraphic Mesozoic. 2. Petrology North Amer ica Coast Range. 3. Batholiths. i. Title. (Series: TJ. S. Geological Survey. Bulletin 1070-B. Series: U. S. Geological Sur vey. Investigations of western batholiths) 552.39 For sale by the Superintendent of Documents, U. S. Government Printing Office Washington 25, D. C. - Price 15 cents (paper cover) CONTENTS Page ___u___-______--j____-i_---_-_-_ ---- -___---__ _-- 35 Introduction. __________ __ _______ ________ _ ____ 35 Method........___________ 37 Age determinations _______________--__---_-_-__ _____________ 41 Batholithic rocks from Baja California, Oaxaca, and Guerrero, Mexico.._____________-_-_---_------------------------_ -__ 41 Southern California and related batholiths 48 Sierra Nevada and related batholiths _.__ _ ______ __ 49 Idaho batholith....___________-_ ________________ 50 Coast Range batholith __________________________ ___________ 51 Comparison with other age determinations ___________ _____ 58 Significance of the data__ ___.__.,_ _.__ ___________ __ 58 References____________________-------_---_ ___________________ 61 ILLUSTRATIONS Page FIGURE 5. -
Bark Beetles in Western North America: an Annotated Bibliography for Natural Resource Managers
Bark Beetles in Western North America: An Annotated Bibliography for Natural Resource Managers Gregory S. Pappas University of Wyoming Laramie, WY 2013 i i Compiled by Greg Pappas, candidate for a master of science in botany and environment and natural resources at the University of Wyoming, as part of “Our Future Forests: Beyond Bark Beetles,” a project of the Medicine Bow-Routt National Forests and Ruckelshaus Institute of Environment and Natural Resources conducted in 2013. Cover photo © Joe Riis/U.S. Forest Service 2013 The Medicine Bow-Routt National Forests and Thunder Basin National Grassland cover nearly 2.9 million acres from north central Colorado to central and northeastern Wyoming. http://www.fs.usda.gov/mbr The Ruckelshaus Institute of Environment and Natural Resources at the University of Wyoming supports stakeholder-driven solutions to environmental challenges by communicating relevant research and promoting collaborative decision making. http://www.uwyo.edu/haub/ruckelshaus-institute ii ABSTRACT An unprecedented multi-species bark beetle epidemic has caused severe tree mortality across western North American forests, prompting concerns about the safety, management, and future health and development of these changing landscapes. The significant ecological and socioeconomic impacts associated with bark beetle outbreaks present issues and challenges best addressed through cooperation among community residents, policymakers, and managers. The public's perception of both the epidemic and ability of resource managers to respond effectively varies considerably depending on location and time since disturbance. A thorough understanding of this and other human aspects of bark beetle outbreaks is necessary to alleviate the potential tension between managers and stakeholders created by management actions. -
The Geology of Western North America (Abridged Version)
THE GEOLOGY OF WESTERN NORTH AMERICA (ABRIDGED VERSION) By JoAnne Nelson, British Columbia Ministry of Energy and Mines, Victoria, BC, Canada [email protected] The geological history of western North America has siliciclastic strata that are now beautifully exposed in the been, and continues to be, shaped by its position on the Canadian Rocky Mountains. The Mt. Brussilof magnesite eastern rim of the Pacific Ocean. The modern Pacific deposit is hosted by Middle Cambrian carbonate within Ocean’s basin is the successor of the original ocean which this continental shelf sequence. Equivalent platformal split Laurentia - our continent’s cratonic core - away from strata are best exposed in the southwestern United States, the rest of the Precambrian supercontinent Rodinia, an the Grand Canyon being a world-renowned example. The ocean that widened until in late Paleozoic time, it became opening of Panthalassa was not a single event in western Panthalassa, the World Ocean. Unlike the eastern side of North America: convincing Cambrian as well as late the continent, where continental collision was followed Proterozoic rift-related sequences occur, and alkalic to by re-opening of the Atlantic Ocean - the “Wilson cycle” ocean-floor basalts in the miogeocline range through - western North America has always faced the same Ordovician into Devonian age. The implied protracted active ocean basin. Its tectonic evolution has always been nature of this rift event, in contrast to the short-lived and that of an active margin, affected first by multi-episodic efficient opening of the Atlantic Ocean, continues to rifting, and then by plate-margin subduction and puzzle. -
On the Northwestern Plains of North America, Archaeological Models of Settlement Systems Are, for the Most Part, Based on the Ec
INDIGENOUS STEWARDSHIP: LESSONS FROM YESTERDAY FOR THE PARKS OF TOMORROW by Gerald A. Oetelaar and D. Joy Oetelaar 1 ABSTRACT Most researchers today acknowledge the impact of Indigenous populations on the supposed ‘natural’ or ‘pristine’ environments encountered by European explorers and naturalists travelling through the interior of North America. However, few are willing to accept the extent of this landscape management, especially in western North America. In fact, Indigenous populations created their own series of ‘parks’ through species-level, community-level and landscape-level management strategies such as the manipulation of plants, the selective harvest and displacement of resources, and the use of controlled burns. The resultant ‘parks’ were scattered across southern Alberta and were the product of disturbance and contingency guided by Indigenous perceptions of the reciprocal relationship between humans and the world around them. Using examples of managed landscapes scattered across southern Alberta, we discuss the origin of these Indigenous preserves and outline the motivation behind their stewardship. The lesson learned from this Indigenous approach to stewardship, we believe, provides guidelines for the management practices of tomorrow. 2 The establishment of Canada’s first national park in 1885 was, at least partially, motivated by a desire to attract tourists to the west but the current policies and practices of Canada’s protected areas are clearly aimed at conservation and restoration using measures of biodiversity to assess the ecological integrity of the ecosystem. Thus, management efforts are directed at maintaining ecosystems in as natural a state as possible, the latter being determined primarily by climate as modified locally by topography, drainage and soil parent material. -
Biological Evaluation Sensitive Plants and Fungi Tahoe National Forest American River Ranger District Big Hope Fire Salvage and Restoration Project
BIOLOGICAL EVALUATION SENSITIVE PLANTS AND FUNGI TAHOE NATIONAL FOREST AMERICAN RIVER RANGER DISTRICT BIG HOPE FIRE SALVAGE AND RESTORATION PROJECT Prepared by: KATHY VAN ZUUK Plant Ecologist/Botanist TNF Nonnative Invasive Plant Coordinator February 27, 2014 A Portion of the American Wildfire Area along Foresthill Divide Road 1 TABLE OF CONTENTS Topic Page Executive Summary 4 Introduction 6 Consultation to Date 6 Current Management Direction 8 Alternative Descriptions 9 Existing Environment 11 Description of Affected Sensitive Species Habitat Effects Analysis and 20 Determinations Reasonably Foreseeable Actions/Time Frames for the Analysis/ List of 20 Assumptions Effects to Species without potential habitat in the Project Area 22 • Lemmon’s milk-vetch, Astragalus lemmonii 22 • Modoc Plateau milk-vetch, Astragalus pulsiferae var. coronensis 22 • Sierra Valley Ivesia, Ivesia aperta var. aperta 22 • Dog Valley Ivesia, Ivesia aperta var. canina 23 • Plumas Ivesia, Ivesia sericoleuca 23 • Webber’s Ivesia, Ivesia webberi 23 • Wet-cliff Lewisia, Lewisia cantelovii 24 • Long-petaled Lewisia, Lewisia longipetala 24 • Follett’s mint, Monardella follettii 24 • Layne’s butterweed, Packera layneae 24 • White bark pine, Pinus albicaulis 25 • Sticky Pyrrocoma, Pyrrocoma lucida 25 Effects to Species with potential habitat in the Project Area 26 • Webber’s Milkvetch, Astragalus webberi 26 • Carson Range rock cress, Boechera rigidissima var. demota 27 • Triangle-lobe moonwort, Botrychium ascendens 27 • Scalloped moonwort, Botrychium crenulatum 27 • Common moonwort, Botrychium lunaria 27 • Mingan moonwort, Botrychium minganense 27 • Mountain moonwort, Botrychium montanum 28 • Bolander’s candle moss, Bruchia bolanderi 29 • Clustered Lady’s Slipper Orchid, Cypripedium fasciculatum 29 • Mountain Lady’s Slipper Orchid, Cypripedium montanum 30 • Starved Daisy, Erigeron miser 31 • Donner Pass Buckwheat, Eriogonum umbellatum var. -
Rough Periwinkles at Emersion Presence Or Absence of Response in Gene Expression of Aspartate Aminotransferase?
Rough periwinkles at emersion Presence or absence of response in gene expression of aspartate aminotransferase? CH-14 Cecilia Helmerson Degree project for Master of Science (Two Years) in Marine Sciences and Biology Degree course in Marine ecology 45 hec Spring and Autumn 2014 Department of Biological and Environmental Sciences University of Gothenburg Examiner: Kerstin Johannesson Department of Biological and Environmental Sciences University of Gothenburg Supervisors: Marina Panova and Olga Ortega Martinez Department of Biological and Environmental Sciences University of Gothenburg Illustration: Cecilia Helmerson 2014 Index ABSTRACT ............................................................................................................................................................ 4 1. INTRODUCTION ............................................................................................................................................. 5 2. MATERIALS AND METHODS ................................................................................................................... 7 2.1 SAMPLING AND ACCLIMATION ....................................................................................................................................... 7 2.2 EMERSION EXPERIMENT .................................................................................................................................................. 8 2.3 DISSECTION AND EXTRACTION ..................................................................................................................................