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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. -
Naturkunde-Museum Bamberg (NKMB)
Jahresbericht 2008 der Generaldirektion der Staatlichen Naturwissenschaftlichen Sammlungen Bayerns Herausgegeben von: Prof. Dr. Gerhard Haszprunar Generaldirektor Der Staatlichen Naturwissenschaftlichen Sammlungen Bayerns Menzinger Straße 71, 80638 München München November 2009 Zusammenstellung und Endredaktion: Dr. Eva Maria Natzer (Generaldirektion) Unterstützung durch: Maria-Luise Kaim (Generaldirektion) Susanne Legat (Generaldirektion) Dr. Jörg Spelda (Generaldirektion) Druck: Digitaldruckzentrum, Amalienstrasse, München Inhaltsverzeichnis Bericht des Generaldirektors ...................................................................................................5 Wissenschaftliche Publikationen ................................................................................................7 Drittmittelübersicht ...................................................................................................................36 Organigramm ............................................................................................................................51 Generaldirektion .....................................................................................................................52 Personalvertretung ....................................................................................................................54 Museen Museum Mensch und Natur (MMN) ........................................................................................55 Museum Reich der Kristalle (MRK) ........................................................................................61 -
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. -
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). -
Abstract Volume
ABSTRACT VOLUME August 11-16, 2019 1 2 Table of Contents Pages Acknowledgements……………………………………………………………………………………………...1 Abstracts Symposia and Contributed talks……………………….……………………………………………3-225 Poster Presentations…………………………………………………………………………………226-291 3 Venom Evolution of West African Cone Snails (Gastropoda: Conidae) Samuel Abalde*1, Manuel J. Tenorio2, Carlos M. L. Afonso3, and Rafael Zardoya1 1Museo Nacional de Ciencias Naturales (MNCN-CSIC), Departamento de Biodiversidad y Biologia Evolutiva 2Universidad de Cadiz, Departamento CMIM y Química Inorgánica – Instituto de Biomoléculas (INBIO) 3Universidade do Algarve, Centre of Marine Sciences (CCMAR) Cone snails form one of the most diverse families of marine animals, including more than 900 species classified into almost ninety different (sub)genera. Conids are well known for being active predators on worms, fishes, and even other snails. Cones are venomous gastropods, meaning that they use a sophisticated cocktail of hundreds of toxins, named conotoxins, to subdue their prey. Although this venom has been studied for decades, most of the effort has been focused on Indo-Pacific species. Thus far, Atlantic species have received little attention despite recent radiations have led to a hotspot of diversity in West Africa, with high levels of endemic species. In fact, the Atlantic Chelyconus ermineus is thought to represent an adaptation to piscivory independent from the Indo-Pacific species and is, therefore, key to understanding the basis of this diet specialization. We studied the transcriptomes of the venom gland of three individuals of C. ermineus. The venom repertoire of this species included more than 300 conotoxin precursors, which could be ascribed to 33 known and 22 new (unassigned) protein superfamilies, respectively. Most abundant superfamilies were T, W, O1, M, O2, and Z, accounting for 57% of all detected diversity. -
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. -
Assessment of Mitochondrial Genomes for Heterobranch Gastropod Phylogenetics
Assessment of mitochondrial genomes for heterobranch gastropod phylogenetics Rebecca M Varney University of Alabama Bastian Brenzinger Staatliche Naturwissenschaftliche Sammlungen Bayerns Manuel António E. Malaquias Universitetsmuseet i Bergen Christopher P. Meyer Smithsonian Institution Michael Schrödl Staatliche Naturwissenschaftliche Sammlungen Bayerns Kevin Kocot ( [email protected] ) The University of Alabama https://orcid.org/0000-0002-8673-2688 Research article Keywords: Heterobranchia, Gastropoda, mitochondrial genome, mitogenomic Posted Date: December 10th, 2020 DOI: https://doi.org/10.21203/rs.3.rs-30542/v3 License: This work is licensed under a Creative Commons Attribution 4.0 International License. Read Full License Version of Record: A version of this preprint was published on January 21st, 2021. See the published version at https://doi.org/10.1186/s12862-020-01728-y. Page 1/19 Abstract Background Heterobranchia is a diverse clade of marine, freshwater, and terrestrial gastropod molluscs. It includes such disparate taxa as nudibranchs, sea hares, bubble snails, pulmonate land snails and slugs, and a number of (mostly small-bodied) poorly known snails and slugs collectively referred to as the “lower heterobranchs.” Evolutionary relationships within Heterobranchia have been challenging to resolve and the group has been subject to frequent and signicant taxonomic revision. Mitochondrial (mt) genomes can be a useful molecular marker for phylogenetics but, to date, sequences have been available for only a relatively small subset of Heterobranchia. Results To assess the utility of mitochondrial genomes for resolving evolutionary relationships within this clade, eleven new mt genomes were sequenced including representatives of several groups of “lower heterobranchs.” Maximum likelihood analyses of concatenated matrices of the thirteen protein coding genes found weak support for most higher-level relationships even after several taxa with extremely high rates of evolution were excluded. -
Caenogastropoda
13 Caenogastropoda Winston F. Ponder, Donald J. Colgan, John M. Healy, Alexander Nützel, Luiz R. L. Simone, and Ellen E. Strong Caenogastropods comprise about 60% of living Many caenogastropods are well-known gastropod species and include a large number marine snails and include the Littorinidae (peri- of ecologically and commercially important winkles), Cypraeidae (cowries), Cerithiidae (creep- marine families. They have undergone an ers), Calyptraeidae (slipper limpets), Tonnidae extraordinary adaptive radiation, resulting in (tuns), Cassidae (helmet shells), Ranellidae (tri- considerable morphological, ecological, physi- tons), Strombidae (strombs), Naticidae (moon ological, and behavioral diversity. There is a snails), Muricidae (rock shells, oyster drills, etc.), wide array of often convergent shell morpholo- Volutidae (balers, etc.), Mitridae (miters), Buccin- gies (Figure 13.1), with the typically coiled shell idae (whelks), Terebridae (augers), and Conidae being tall-spired to globose or fl attened, with (cones). There are also well-known freshwater some uncoiled or limpet-like and others with families such as the Viviparidae, Thiaridae, and the shells reduced or, rarely, lost. There are Hydrobiidae and a few terrestrial groups, nota- also considerable modifi cations to the head- bly the Cyclophoroidea. foot and mantle through the group (Figure 13.2) Although there are no reliable estimates and major dietary specializations. It is our aim of named species, living caenogastropods are in this chapter to review the phylogeny of this one of the most diverse metazoan clades. Most group, with emphasis on the areas of expertise families are marine, and many (e.g., Strombidae, of the authors. Cypraeidae, Ovulidae, Cerithiopsidae, Triphori- The fi rst records of undisputed caenogastro- dae, Olividae, Mitridae, Costellariidae, Tereb- pods are from the middle and upper Paleozoic, ridae, Turridae, Conidae) have large numbers and there were signifi cant radiations during the of tropical taxa. -
BULLETIN Bull
Bull. Inst. r. Sci. nat. Belg. Bruxelles Bull. K. Belg. Inst. Nat. Wet. Brussel 31-XII-1983 55 I BIOLOGIE THE MARINE MICROGASTROPODS FROM THE NORTHERN COAST OF PAPUA NEW GUINEA (MOLLUSCA : GASTROPODA) I. FAMILY: OMALOGYRIDAE (WITH DESCRIPTION OF TWO NEW SPECIES) BY Willy SLEURS (With 1 plate) BULLETIN Bull. Inst. r. Sci. nat. Belg. Bruxelles Bull. K. Belg. Inst. Nat. Wet. Brussel 31-XII-1983 55 I BIOLOGIE THE MARINE MJCROGASTROPODS FROM THE NORTHERN COAST OF PAPUA NEW GUINEA (MOLLUSCA : GASTROPODA) I. FAMILY: OMALOGYRIDAE (WITH DESCRIPTION OF TWO NEW SPECIES) (1) BY Willy SLEURS (With 1 plate) ABSTRACT This publication deals with the Omalogyridae found off the Northern coast of Papua New Guinea. Three species have been recorded; two of them, Omalogyra nodicari nata sp. nov. and 0. vangoethemi sp. nov. are described as new. The validity of the genus Ammonicera VA YSSIERE, 1893 is discussed. SAMENV ATTING Deze publikatie behandelt de Omalogyridae van de noordelijke kust van Papoea Nieuw-Guinea. Drie soorten werden waargenomen, waarvan Omalogyra nodicarinata sp. nov. en 0. vangoethemi sp. nov. als nieuw worden beschreven. De geldigheid van her genus Ammonicera VA YSSIERE, 1893 wordt besproken. (1) Leopold III Biological Station, Laing Isl and, Contribution no 51. W. SLElIRS 55, :! RESUME Ce travail traite des Omalogyridae provenant de la cote nord de Papouasie Nouvelle-Guinee. T rois especes ont ere trouvees, dont deux, Omalogyra .nodicarinata sp. nov. et 0. vangoethemi sont nouvelles pour la science. La validite du genre Ammonicera VA YSSIERE, 1893 est discutee. I. INTRODUCTION This is the first of a series of forthcoming papers, concerning the marine microgastropods mainly found on Halimeda-algae and in sedi ments off the Northern coast of Papua New Guinea.