The Type Locality of Craveri's Murrelet
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The Mark of the Japanese Murrelet (Synthliboramphus Wumizusume): a Study of Song and Stewardship in Japan’S Inland Sea
Claremont Colleges Scholarship @ Claremont Pomona Senior Theses Pomona Student Scholarship 2019 The aM rk of the Japanese Murrelet (Synthliboramphus wumizusume): A study of song and stewardship in Japan’s Inland Sea Charlotte Hyde The Mark of the Japanese Murrelet (Synthliboramphus wumizusume): A study of song and stewardship in Japan’s Inland Sea Charlotte Hyde In partial fulfillment of the Bachelor of Arts Degree in Environmental Analysis, 2018-2019 academic year, Pomona College, Claremont, California Readers: Nina Karnovsky Wallace Meyer Acknowledgements I would first like to thank Professor Nina Karnovsky for introducing me to her work in Kaminoseki and for allowing me to join this incredible project, thereby linking me to a community of activists and scientists around the world. I am also so appreciative for her role as my mentor throughout my years as an undergraduate and for helping me develop my skills and confidence as a scholar and ecologist. Thank you also to my reader Wallace Meyer for his feedback on my writing and structure. I am so thankful for the assistance of Char Miller, who has worked tirelessly to give valuable advice and support to all seniors in the Environmental Analysis Department throughout their thesis journeys. Thank you to Marc Los Huertos for his assistance with R and data analysis, without which I would be hopelessly lost. I want to thank my peers in the Biology and Environmental Analysis departments for commiserating with me during stressful moments and for providing a laugh, hug, or shoulder to cry on, depending on the occasion. Thank you so much to my parents, who have supported me unconditionally throughout my turbulent journey into adulthood and who have never doubted my worth as a person or my abilities as a student. -
Ancient Murrelet Synthliboramphus Antiquus
Major: Ancient Murrelet Synthliboramphus antiquus colony attendance at Langara 233 ANCIENT MURRELET SYNTHLIBORAMPHUS ANTIQUUS COLONY ATTENDANCE AT LANGARA ISLAND ASSESSED USING OBSERVER COUNTS AND RADAR IN RELATION TO TIME AND ENVIRONMENTAL CONDITIONS HEATHER L. MAJOR1,2 1Centre for Wildlife Ecology, Department of Biological Sciences, Simon Fraser University, 8888 University Drive, Burnaby, BC V5A 1S6, Canada 2Current address: Department of Biological Sciences, University of New Brunswick, P.O. Box 5050, Saint John, NB E2L 4L5, Canada ([email protected]) Received 10 June 2016, accepted 26 July 2016 SUMMARY MAJOR, H.L. 2016. Ancient Murrelet Synthliboramphus antiquus colony attendance at Langara Island assessed using observer counts and radar in relation to time and environmental conditions. Marine Ornithology 44: 233–240. The decision to attend a colony on any given day or night is arguably the result of a trade-off between survival and reproductive success. It is often difficult to study this trade-off, as monitoring patterns of colony attendance for nocturnal burrow-nesting seabirds is challenging. Here, I 1) examined the effectiveness of monitoring Ancient Murrelet colony arrivals using marine radar, and 2) evaluated differences in colony attendance behavior in relation to time, light, and weather. I found a strong correlation between the number of Ancient Murrelets counted by observers in the colony and the number of radar targets counted, with estimated radar target counts being ~95 times higher than observer counts. My hypothesis that patterns of colony attendance are related to environmental conditions (i.e. light and weather) and that this relationship changes with time after sunset was supported. -
Biological Monitoring at Aiktak Island, Alaska in 2016
AMNWR 2017/02 BIOLOGICAL MONITORING AT AIKTAK ISLAND, ALASKA IN 2016 Sarah M. Youngren, Daniel C. Rapp, and Nora A. Rojek Key words: Aiktak Island, Alaska, Aleutian Islands, ancient murrelet, Cepphus columba, common murre, double-crested cormorant, fork-tailed storm-petrel, Fratercula cirrhata, Fratercula corniculata, glaucous-winged gull, horned puffin, Larus glaucescens, Leach’s storm-petrel, Oceanodroma furcata, Oceanodroma leucorhoa, pelagic cormorant, Phalacrocorax auritus, Phalacrocorax pelagicus, Phalacrocorax urile, pigeon guillemot, population trends, productivity, red-faced cormorant, Synthliboramphus antiquus, thick-billed murre, tufted puffin, Uria aalge, Uria lomvia. U.S. Fish and Wildlife Service Alaska Maritime National Wildlife Refuge 95 Sterling Highway, Suite 1 Homer, AK 99603 January 2017 Cite as: Youngren, S. M., D. C. Rapp, and N. A. Rojek. 2017. Biological monitoring at Aiktak Island, Alaska in 2016. U.S. Fish and Wildl. Serv. Rep., AMNWR 2017/02. Homer, Alaska. Tufted puffins flying along the southern coast of Aiktak Island, Alaska. TABLE OF CONTENTS Page INTRODUCTION ........................................................................................................................................... 1 STUDY AREA ............................................................................................................................................... 1 METHODS ................................................................................................................................................... -
A Review of the Fossil Seabirds from the Tertiary of the North Pacific
Paleobiology,18(4), 1992, pp. 401-424 A review of the fossil seabirds fromthe Tertiaryof the North Pacific: plate tectonics,paleoceanography, and faunal change Kenneth I. Warheit Abstract.-Ecologists attempt to explain species diversitywithin Recent seabird communities in termsof Recent oceanographic and ecological phenomena. However, many of the principal ocean- ographic processes that are thoughtto structureRecent seabird systemsare functionsof geological processes operating at many temporal and spatial scales. For example, major oceanic currents,such as the North Pacific Gyre, are functionsof the relative positions of continentsand Antarcticgla- ciation,whereas regional air masses,submarine topography, and coastline shape affectlocal processes such as upwelling. I hypothesize that the long-termdevelopment of these abiotic processes has influencedthe relative diversityand communitycomposition of North Pacific seabirds. To explore this hypothesis,I divided the historyof North Pacific seabirds into seven intervalsof time. Using published descriptions,I summarized the tectonicand oceanographic events that occurred during each of these time intervals,and related changes in species diversityto changes in the physical environment.Over the past 95 years,at least 94 species of fossil seabirds have been described from marine deposits of the North Pacific. Most of these species are from Middle Miocene through Pliocene (16.0-1.6 Ma) sediments of southern California, although species from Eocene to Early Miocene (52.0-22.0 Ma) deposits are fromJapan, -
Allocation of Growth in Food-Stressed Atlantic Puffin Chicks
The Auk 113(4):830-841, 1996 ALLOCATION OF GROWTH IN FOOD-STRESSED ATLANTIC PUFFIN CHICKS HILDE STOL •JYAN • AND TYCHO ANKER-NILSSEN NorwegianInstitute for NatureResearch, Tungasletta 2, N-7005 Trondheim,Norway ABSTt•CT.--In long-lived seabirdsthat lay a single-eggclutch, allocation of growth to certain body parts may be advantageousfor the chick if food is limited. To investigatethis, 40 Atlantic Puffin (Fraterculaarctica) hatchlings were distributedin sevengroups that were raisedon differentamounts of food to 38 daysof age.When food intakewas reduced,growth rateswere depressedfor all charactersmeasured (i.e. body massand length of the wing, 2nd primary, forearm, head + bill, culmen, skull, tarsus,and middle toe). Head and wing parts grew preferentiallyrelative to the other characters,and onsetof growth was delayedin the primaries.All chicksaccumulated significant amounts of subcutaneousfat, whereasinternal fat depositswere presentonly in the chicksthat receivedthe mostfood. Received14 July1995, accepted20 March 1996. ONEWAY that parent birds adjustfor variation The wide variation in chick growth rates in food availability is to vary clutch size (Lack among speciesof alcids has been attributed to 1954,1966, 1968). In long-livedspecies that lay constraintson feeding ecology, such as spe- a single-eggclutch, alteration of chick growth cialized foraging behaviors,unpredictable and rate apparentlyis the only strategyavailable to patchy food distributions, and great distances adjust for variation in food. Slow growth re- between feeding and nesting sites (Lack 1968; duces daily energy requirements and allows Ricklefs 1968, 1984;Ashmole 1971;Sealy 1973; food to be delivered at a lower rate (Lack 1968; Nelson 1977; Birkhead and Harris 1985). Thus, Ricklefs 1968, 1979; Harris 1977; Nelson 1977; chicks of pelagic alcids often face the problem Drent and Daan 1980). -
Chevron-Shaped Accumulations Along the Coastlines of Australia As Potential Tsunami Evidences?
CHEVRON-SHAPED ACCUMULATIONS ALONG THE COASTLINES OF AUSTRALIA AS POTENTIAL TSUNAMI EVIDENCES? Dieter Kelletat Anja Scheffers Geographical Department, University of Duisburg-Essen Universitätsstr. 15 D-45141 Essen, Germany e-mail: [email protected] ABSTRACT Along the Australian coastline leaf- or blade-like chevrons appear at many places, sometimes similar to parabolic coastal dunes, but often with unusual shapes including curvatures or angles to the coastline. They also occur at places without sandy beaches as source areas, and may be truncated by younger beach ridges. Their dimensions reach several kilometers inland and altitudes of more than 100 m. Vegetation development proves an older age. Judging by the shapes of the chevrons at some places, at least two generations of these forms can be identified. This paper dis- cusses the distribution patterns of chevrons (in particular for West Australia), their various appearances, and the possible genesis of these deposits, based mostly on the interpretations of aerial photographs. Science of Tsunami Hazards, Volume 21, Number 3, page 174 (2003) 1. INTRODUCTION The systematic monitoring of tsunami during the last decades has shown that they are certainly not low frequency events: on average, about ten events have been detected every year – or more than 1000 during the last century (Fig. 1, NGDC, 2001) – many of which were powerful enough to leave imprints in the geological record. Focusing only on the catastrophic events, we find for the last 400 years (Fig. 2, NGDC, 2001) that 92 instances with run up of more than 10 m have occurred, 39 instances with more than 20 m, and 14 with more than 50 m, or – statistically and without counting the Lituya Bay events – one every 9 years with more than 20 m run up worldwide. -
USGS Geologic Investigations Series I-2761, Molokai and Lanai
Molokai and Lanai Molokai and Lanai are the least populated and smallest of the main Hawaiian Islands. Both are relatively arid, except for the central mountains of each island and northeast corner of Molokai, so flooding are not as common hazards as on other islands. Lying in the center of the main Hawaiian Islands, Molokai and Lanai are largely sheltered from high annual north and northwest swell and much of south-central Molokai is further sheltered from south swell by Lanai. On the islands of Molokai and Lanai, seismicity is a concern due to their proximity to the Molokai 71 Seismic Zone and the active volcano on the Big Island. Storms and high waves associated with storms pose a threat to the low-lying coastal terraces of south Molokai and northeast Lanai. Molokai and Lanai Index to Technical Hazard Maps 72 Tsunamis tsunami is a series of great waves most commonly caused by violent Amovement of the sea floor. It is characterized by speed (up to 590 mph), long wave length (up to 120 mi), long period between successive crests (varying from 5 min to a few hours,generally 10 to 60 min),and low height in the open ocean. However, on the coast, a tsunami can flood inland 100’s of feet or more and cause much damage and loss of life.Their impact is governed by the magnitude of seafloor displacement related to faulting, landslides, and/or volcanism. Other important factors influenc- ing tsunami behavior are the distance over which they travel, the depth, topography, and morphology of the offshore region, and the aspect, slope, geology, and morphology of the shoreline they inundate. -
Journal of Avian Biology JAV-00487 Smith, N
Journal of Avian Biology JAV-00487 Smith, N. A. and Clarke, J. A. 2014. Systematics and evolution evolution of the Pan-Alcidae (Aves, Charadriiformes). – J. Avian Biol. doi: 10.1111/ jav.00487 Supplementary material Appendix 1 Supplementary Tables Table A1. Taxon sampling and associated morphological character and sequence incompleteness (i.e., % missing data). Totals include molecular gaps and morphological characters not scored owing to absence. Extinct taxa denoted by "†". Supraspecific taxon terminal denoted by "SST". Morphological Molecular Combined Taxon Data Sequence Data Data 1. †Aethia barnesi 93.8 100 99.8 2. Aethia cristatella 24.9 38.3 37.9 3. Aethia psittacula 12.2 38.1 37.4 4. Aethia pusilla 11.3 37.5 36.8 5. Aethia pygmaea 24.4 37.5 37.1 6. †Aethia storeri 85.3 100 99.6 7. †Alca ausonia 84.1 100 99.6 8. †Alca carolinensis 62.9 100 98.9 9. †Alca grandis 70.5 100 99.2 10. †Alca minor 84.7 100 99.6 11. †Alca olsoni 71.4 100 99.6 12. Alca torda 2.8 36.4 35.5 13. †Alca stewarti 72.8 100 99.3 14. Alle alle 10.8 33.1 32.5 15. Anous tenuirostris 26.9 61.6 60.6 16. Bartramia longicauda 12.7 53.7 52.6 17. Brachyramphus brevirostris 24.6 37.8 37.5 18. †Brachyramphus dunkeli 84.7 100 99.6 19. Brachyramphus marmoratus 5.1 37.5 36.6 20. Brachyramphus perdix 25.8 41.6 41.2 21. †Brachyramphus pliocenum 85.3 100 99.6 22. -
Chart Standardization & Paper Chart Working Group
INTERNATIONAL HYDROGRAPHIC ORGANISATION HYDROGRAPHIQUE ORGANIZATION INTERNATIONALE CHART STANDARDIZATION & PAPER CHART WORKING GROUP (CSPCWG) [A Working Group of the Hydrographic Services and Standards Committee (HSSC)] Chairman: Peter JONES Secretary: Andrew HEATH-COLEMAN UK Hydrographic Office Admiralty Way, Taunton, Somerset TA1 2DN, United Kingdom CSPCWG Letter: 03/2012 Telephone: UKHO ref: HA317/010/031-08 (Chairman) +44 (0) 1823 337900 ext 5035 (Secretary) +44 (0) 1823 337900 ext 3656 Facsimile: +44 (0) 1823 325823 E-mail: [email protected] E-mail: [email protected] [email protected] To CSPCWG Members Date 24 January 2012 Dear Colleagues, Subject: Draft revision of S-4 Section B-300 to B-330 – Round 2 Thank you to the 21 WG members who responded to Letter 03/2011; I apologise for the delay in progressing this. As usual, Andrew and I have consolidated the responses, including all the comments, into Annex A. As you will see, there was a good consensus on most of the questions we asked (even where the answer was „no‟). Some other answers were less clear cut, but usually the associated comments guided us in an outcome which we hope will be acceptable. There were lots of other helpful comments, and I have responded to all these, many of them resulting in some adjustments to the proposed text. We have now prepared a „round 2‟ version of the section, as Annex B (although because of size, we have converted this to PDF and attached as a separate document). As usual, those changes which were not challenged in the first round have now been converted to blue text. -
ALPHABETICAL LIST of CERTAIN LOCAL COMMON GEOGRAPHICAL NAMES APPEARING on MARINE CHARTS WHICH ARE GENERALLY NOT TRANSLATED. Prep
ALPHABETICAL LIST OF CERTAIN LOCAL COMMON GEOGRAPHICAL NAMES APPEARING ON MARINE CHARTS WHICH ARE GENERALLY NOT TRANSLATED. Prepared by the International Hydrographic Bureau. INTRODUCTION. We have grouped below, in an alphabetical list, a collection of geographical common names and adjectives which, in practice, are generally not translated but are retained, in any case,in a form of transcription conforming* more or less to the original orthography, and which appear on the marine charts published or reproduced by the various countries. Lists of this kind are sometimes given in the topographical atlases on the charts of which a large number of geographical names are preserved in the form and with the orthography of the country to which they belong. The list which we have prepared from documents in the possession of the International Hydrographic Bureau, by adding the signification in French and English to each term, does not constitute a dictionary or a vocabulary. We have simply sought to avoid the omission of the most important terms relating to hydrography and for which terms a translation is generally not required on the reproductions. No special rule has been followed with regard to the transcription of names, owing to the lack of any common orthographic rule applicable to the phonetic transcription of all the languages, whether they use latin characters or not. Thus, one finds in the list, for instance, the Arabic word for m ountain given indiscriminately under the form of Jebel (English orthography) or D jebel (French orthography) or also Gebei (Italian orthography) etc. In order to partially remedy this defect it will suffice to invite attention to certain approximate phonetic equivalents, such as those indicated later on in our note. -
LANDSCAPE STUDY of the ISLAND of CRES Local Development LOCAL DEVELOPMENT Pilot Project ISLAND of PILOT PROJECT “ISLAND CRES of CRES”
Local development pilot project LANDSCAPE STUDY OF THE ISLAND OF CRES Local Development LOCAL DEVELOPMENT Pilot Project ISLAND OF PILOT PROJECT “ISLAND CRES OF CRES” PROJECT IMPLEMENTED BY: OTRA d.o.o. PROJECT FINANCIALLY SUPPORTED BY: Council of Europe Ministry of culture Primorje-Gorski kotar County Town of Cres ACKNOWLEDGEMENTS This document would not have been possible without cooperation and contribution of all the stakeholders involved in this project: Institutions: Ministry of culture of the Republic of Croatia │ Ministry of environmental and nature protection of the │ Republic of Croatia │ Oikon d.o.o. │ 3e projekti d.o.o. Members of the coordination team: dr. sc. Tatjana Lolić │ dr. sc. Ugo Toić │ Tanja Kremenić, mag. geogr. │ Mirna Bojić, dipl. ing. agr. │ dr. sc. Goran Andlar │ dr. sc. Biserka Dumbović-Bilušić │ mr. sc. Ksenija Petrić, dipl. ing. arh. │ Višnja Šteko, mag. ing. prosp. arch. Narrators: Inhabitants of the island of Cres and experts involved in this project LANDSCAPE STUDY OF THE ISLAND OF CRES Mentors: dr. sc. Goran Andlar, mag. ing. prosp. arch. Tanja Kremenić, mag. geogr. Miran Križanić, mag. ing. arh. Marija Borovičkić, mag. hist. art. et ethnol. et anthrop. Council of Europe consultant Alexis Gérard, krajobrazni arhitekt Executive team: Nikolina Krešo, mag. ing. prosp. arch. Marija Kušan, stud. prosp. arch. Ana Knežević, stud. prosp. arch. Anita Trojanović, stud. prosp. arch. Jure Čulić, mag. ing. prosp. arch. Mateja Leljak, mag. ing. prosp. arch. Dijana Krišto, stud. prosp. arch. Tanja Udovč, mag. ing. prosp. arch. Cres, December 2015 4 CONTENTS 1. INTRODUCTION ...................................................................................7 4.2. Landscape Unit Of The Town Of Cres ....................................... -
ANCIENT MURRELET Synthliboramphus Antiquus
Alaska Seabird Information Series ANCIENT MURRELET Synthliboramphus antiquus Conservation Status ALASKA: Highly Imperiled N. AMERICAN: High Risk GLOBAL: Least Concern Breed Eggs Incubation Fledge Nest Feeding Behavior Diet June-Aug 1-2 33-36+ d 1-4 d burrow surface dive crustaceans, fish Life History and Distribution The Ancient Murrelet (Synthliboramphus antiquus) is unique among seabirds in rearing its chicks entirely at sea. Successful mating leads to two comparatively enormous eggs, each weighing approximately one-quarter of the female's weight. Only 2-4 days after hatching, without ever having been fed, the downy youngsters leave the nest and follow the adult birds to the sea. The chicks remain with their parents for at least one month after leaving the colony. This behavior and their nocturnal habits appear to be adaptations to reduce predation on adults. Ancient Murrelets have a relatively low adult annual mortality rate. Jones Ian Copyright These murrelets normally breed in colonies on forested islands or those covered in grass or dense forbs. Alaska Seasonal Distribution Nests are usually burrows dug in soft soil, but cavities AK Region Sp S F W under tree roots and shallow holes under grass tussocks are Southeastern * U U U U also used. Crevices in rocks or among boulders are less Southcoastal * U U U U frequently occupied. Southwestern * C C C C Ancient Murrelets are pigeon-sized birds with a black Central - - - - cap, gray back, cream-colored bill, and pale blue legs and feet. During the breeding season, they have a white stripe Western + R R - over the eye and a black throat patch.