Polar Flora and Fauna Has Become Highly Uncertain
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Antarctic Sessile Marine Benthos: Colonisation and Growth on Artificial Substrata Over Three Years
MARINE ECOLOGY PROGRESS SERIES Vol. 316: 1–16, 2006 Published July 3 Mar Ecol Prog Ser OPENPEN ACCESSCCESS FEATURE ARTICLE Antarctic sessile marine benthos: colonisation and growth on artificial substrata over three years David A. Bowden*, Andrew Clarke, Lloyd S. Peck, David K. A. Barnes Natural Environment Research Council, British Antarctic Survey, High Cross, Madingley Road, Cambridge CB3 0ET, UK ABSTRACT: The development of sessile invertebrate assemblages on hard substrata has been studied exten- sively in temperate and tropical latitudes. Such studies provide insights into a range of ecological processes, and the global similarity of taxa recruiting to these assem- blages affords the potential for regional-scale com- parisons. However, few data exist for high latitude assemblages. This paper presents the first regularly resur- veyed study of benthic colonisation from within the Antarctic Circle. Acrylic panels were deployed horizon- tally on the seabed at 8 and 20 m depths at each of 3 loca- tions in Ryder Bay, Adelaide Island, SW Antarctic Peninsula (67° 35’ S, 68° 10’ W). Assemblages colonising upward- and downward-facing panel surfaces were photographed in situ from February 2001 to March 2004. Assemblages were dominated by bryozoans and spiror- Bowden and co-workers present the first successful benthic bid polychaetes. Total coverage after 3 yr ranged from 6 to colonisation study from within the Antarctic Circle. They 100% on downward-facing surfaces but was <10% on all describe a system governed by extremely slow and highly upward-facing surfaces. Overall colonisation rates were seasonal growth, and a range of post-settlement disturbances in which succession is more predictable than in comparable up to 3 times slower than comparable temperate latitude temperate or tropical assemblages. -
© Terra Antartica Publication Terra Antartica 2001, 8(4), 423-434
© Terra Antartica Publication Terra Antartica 2001, 8(4), 423-434 Palaeogene Macrofossils from CRP-3 Drillhole, Victoria Land Basin, Antarctica M. TAVIANI1* & A.G. BEU2 1Istituto di Geologia Marina, Consiglio Nazionale delle Ricerche, via Gobetti 101, I-40129 Bologna - Italy 2Institute of Geological & Nuclear Sciences, P.O. Box 30 368, Lower Hutt - New Zealand Received 5 March 2001; accepted in revised form 3 July 2001 Abstract - CRP-3 cored Palaeogene strata to 823 metres below the sea floor (mbsf), before passing through Devonian bedrock (Beacon Supergroup) to a depth of 939 mbsf. Palaeogene body fossils have been identified at 239 horizons in the core. The best preserved macrofossils from the core help elucidate the taxonomy, chronology and biogeography of Cenozoic ecosystems of Antarctica, although poor preservation prevents identification to species level in most cases. The lithostratigraphic unit (LSU) of the core top (LSU 1.1) contains an almost monospecific modiolid assemblage, similar to mussel beds recovered in the bottom part of the CRP-2/2A core. These semi-infaunal mussels appear to be conspecific, apparently indicating the same age (Early Oligocene) and environment, i.e., a deep muddy shelf characterized by high turbidity and dysoxic/anoxic bottom conditions (high H2S sediment content). LSU 1.2 contains reasonably diverse assemblages representing inner/middle shelf environments dominated by epifaunal suspension feeders. LSU 2.1 contains low-diversity assemblages of suspension feeders (bivalves, brachiopods and bryzoans), probably indicating inner/middle shelf environments. LSU 3.1 contains assemblages including infaunal and epifaunal suspension feeders (bivalves, including a scallop, ?Adamussium n.sp., and solitary corals) and infaunal deposit-feeders, possibly indicating deposition on a deep muddy shelf. -
Chile: a Journey to the End of the World in Search of Temperate Rainforest Giants
Eliot Barden Kew Diploma Course 53 July 2017 Chile: A Journey to the end of the world in search of Temperate Rainforest Giants Valdivian Rainforest at Alerce Andino Author May 2017 1 Eliot Barden Kew Diploma Course 53 July 2017 Table of Contents 1. Title Page 2. Contents 3. Table of Figures/Introduction 4. Introduction Continued 5. Introduction Continued 6. Aims 7. Aims Continued / Itinerary 8. Itinerary Continued / Objective / the Santiago Metropolitan Park 9. The Santiago Metropolitan Park Continued 10. The Santiago Metropolitan Park Continued 11. Jardín Botánico Chagual / Jardin Botanico Nacional, Viña del Mar 12. Jardin Botanico Nacional Viña del Mar Continued 13. Jardin Botanico Nacional Viña del Mar Continued 14. Jardin Botanico Nacional Viña del Mar Continued / La Campana National Park 15. La Campana National Park Continued / Huilo Huilo Biological Reserve Valdivian Temperate Rainforest 16. Huilo Huilo Biological Reserve Valdivian Temperate Rainforest Continued 17. Huilo Huilo Biological Reserve Valdivian Temperate Rainforest Continued 18. Huilo Huilo Biological Reserve Valdivian Temperate Rainforest Continued / Volcano Osorno 19. Volcano Osorno Continued / Vicente Perez Rosales National Park 20. Vicente Perez Rosales National Park Continued / Alerce Andino National Park 21. Alerce Andino National Park Continued 22. Francisco Coloane Marine Park 23. Francisco Coloane Marine Park Continued 24. Francisco Coloane Marine Park Continued / Outcomes 25. Expenditure / Thank you 2 Eliot Barden Kew Diploma Course 53 July 2017 Table of Figures Figure 1.) Valdivian Temperate Rainforest Alerce Andino [Photograph; Author] May (2017) Figure 2. Map of National parks of Chile Figure 3. Map of Chile Figure 4. Santiago Metropolitan Park [Photograph; Author] May (2017) Figure 5. -
Article Is Available On- 2012
The Cryosphere, 14, 2673–2686, 2020 https://doi.org/10.5194/tc-14-2673-2020 © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License. Clouds damp the radiative impacts of polar sea ice loss Ramdane Alkama1, Patrick C. Taylor2, Lorea Garcia-San Martin1, Herve Douville3, Gregory Duveiller1, Giovanni Forzieri1, Didier Swingedouw4, and Alessandro Cescatti1 1European Commission – Joint Research Centre, Via Enrico Fermi, 2749, 21027 Ispra (VA), Italy 2NASA Langley Research Center, Hampton, Virginia, USA 3Centre National de Recherches Météorologiques, Météo-France/CNRS, Toulouse, France 4EPOC, Université de Bordeaux, Allée Geoffroy Saint-Hilaire, Pessac 33615, France Correspondence: Ramdane Alkama ([email protected]) and Patrick C. Taylor ([email protected]) Received: 19 November 2019 – Discussion started: 19 December 2019 Revised: 19 June 2020 – Accepted: 6 July 202 – Published: 21 August 2020 Abstract. Clouds play an important role in the climate sys- 1 Introduction tem: (1) cooling Earth by reflecting incoming sunlight to space and (2) warming Earth by reducing thermal energy loss to space. Cloud radiative effects are especially important Solar radiation is the primary energy source for the Earth in polar regions and have the potential to significantly alter system and provides the energy driving motions in the atmo- the impact of sea ice decline on the surface radiation budget. sphere and ocean, the energy behind water phase changes, Using CERES (Clouds and the Earth’s Radiant Energy Sys- and the energy stored in fossil fuels. Only a fraction (Loeb tem) data and 32 CMIP5 (Coupled Model Intercomparison et al., 2018) of the solar energy arriving to the top of the Project) climate models, we quantify the influence of polar Earth atmosphere (short-wave radiation; SW) is absorbed at clouds on the radiative impact of polar sea ice variability. -
Reproductive Success in Antarctic Marine Invertebrates
University of Southampton Research Repository ePrints Soton Copyright © and Moral Rights for this thesis are retained by the author and/or other copyright owners. A copy can be downloaded for personal non-commercial research or study, without prior permission or charge. This thesis cannot be reproduced or quoted extensively from without first obtaining permission in writing from the copyright holder/s. The content must not be changed in any way or sold commercially in any format or medium without the formal permission of the copyright holders. When referring to this work, full bibliographic details including the author, title, awarding institution and date of the thesis must be given e.g. AUTHOR (year of submission) "Full thesis title", University of Southampton, name of the University School or Department, PhD Thesis, pagination http://eprints.soton.ac.uk UNIVERSITY OF SOUTHAMPTON FACULTY OF SCIENCE School of Ocean and Earth Science Reproductive Success in Antarctic Marine Invertebrates By Laura Joanne Grange (BSc. Hons) Thesis for the degree of Doctor of Philosophy July 2005 Dedicated to my Mum, Dad, Sam and my one and only Mike. UNIVERSITY OF SOUTHAMPTON ABSTRACT FACULTY OF SCIENCE SCHOOL OF OCEAN AND EARTH SCIENCE Doctor of Philosophy REPRODUCTIVE SUCCESS IN ANTARCTIC MARINE INVERTEBRATES By Laura Joanne Grange The nearshore Antarctic marine environment is unique, characterised by low but constant temperatures that contrast with an intense peak in productivity. As a result of this stenothermal environment, energy input has a profound ecological effect. These conditions have developed over several millions of years and have resulted in an animal physiology that is highly stenothermal and sometimes closely coupled with the seasonal food supply, e.g. -
Bio 308-Course Guide
COURSE GUIDE BIO 308 BIOGEOGRAPHY Course Team Dr. Kelechi L. Njoku (Course Developer/Writer) Professor A. Adebanjo (Programme Leader)- NOUN Abiodun E. Adams (Course Coordinator)-NOUN NATIONAL OPEN UNIVERSITY OF NIGERIA BIO 308 COURSE GUIDE National Open University of Nigeria Headquarters 14/16 Ahmadu Bello Way Victoria Island Lagos Abuja Office No. 5 Dar es Salaam Street Off Aminu Kano Crescent Wuse II, Abuja e-mail: [email protected] URL: www.nou.edu.ng Published by National Open University of Nigeria Printed 2013 ISBN: 978-058-434-X All Rights Reserved Printed by: ii BIO 308 COURSE GUIDE CONTENTS PAGE Introduction ……………………………………......................... iv What you will Learn from this Course …………………............ iv Course Aims ……………………………………………............ iv Course Objectives …………………………………………....... iv Working through this Course …………………………….......... v Course Materials ………………………………………….......... v Study Units ………………………………………………......... v Textbooks and References ………………………………........... vi Assessment ……………………………………………….......... vi End of Course Examination and Grading..................................... vi Course Marking Scheme................................................................ vii Presentation Schedule.................................................................... vii Tutor-Marked Assignment ……………………………….......... vii Tutors and Tutorials....................................................................... viii iii BIO 308 COURSE GUIDE INTRODUCTION BIO 308: Biogeography is a one-semester, 2 credit- hour course in Biology. It is a 300 level, second semester undergraduate course offered to students admitted in the School of Science and Technology, School of Education who are offering Biology or related programmes. The course guide tells you briefly what the course is all about, what course materials you will be using and how you can work your way through these materials. It gives you some guidance on your Tutor- Marked Assignments. There are Self-Assessment Exercises within the body of a unit and/or at the end of each unit. -
MOLLUSCA Nudibranchs, Pteropods, Gastropods, Bivalves, Chitons, Octopus
UNDERWATER FIELD GUIDE TO ROSS ISLAND & MCMURDO SOUND, ANTARCTICA: MOLLUSCA nudibranchs, pteropods, gastropods, bivalves, chitons, octopus Peter Brueggeman Photographs: Steve Alexander, Rod Budd/Antarctica New Zealand, Peter Brueggeman, Kirsten Carlson/National Science Foundation, Canadian Museum of Nature (Kathleen Conlan), Shawn Harper, Luke Hunt, Henry Kaiser, Mike Lucibella/National Science Foundation, Adam G Marsh, Jim Mastro, Bruce A Miller, Eva Philipp, Rob Robbins, Steve Rupp/National Science Foundation, Dirk Schories, M Dale Stokes, and Norbert Wu The National Science Foundation's Office of Polar Programs sponsored Norbert Wu on an Artist's and Writer's Grant project, in which Peter Brueggeman participated. One outcome from Wu's endeavor is this Field Guide, which builds upon principal photography by Norbert Wu, with photos from other photographers, who are credited on their photographs and above. This Field Guide is intended to facilitate underwater/topside field identification from visual characters. Organisms were identified from photographs with no specimen collection, and there can be some uncertainty in identifications solely from photographs. © 1998+; text © Peter Brueggeman; photographs © Steve Alexander, Rod Budd/Antarctica New Zealand Pictorial Collection 159687 & 159713, 2001-2002, Peter Brueggeman, Kirsten Carlson/National Science Foundation, Canadian Museum of Nature (Kathleen Conlan), Shawn Harper, Luke Hunt, Henry Kaiser, Mike Lucibella/National Science Foundation, Adam G Marsh, Jim Mastro, Bruce A Miller, Eva -
Bathymetric Mapping of the North Polar Seas
BATHYMETRIC MAPPING OF THE NORTH POLAR SEAS Report of a Workshop at the Hawaii Mapping Research Group, University of Hawaii, Honolulu HI, USA, October 30-31, 2002 Ron Macnab Geological Survey of Canada (Retired) and Margo Edwards Hawaii Mapping Research Group SCHOOL OF OCEAN AND EARTH SCIENCE AND TECHNOLOGY UNIVERSITY OF HAWAII 1 BATHYMETRIC MAPPING OF THE NORTH POLAR SEAS Report of a Workshop at the Hawaii Mapping Research Group, University of Hawaii, Honolulu HI, USA, October 30-31, 2002 Ron Macnab Geological Survey of Canada (Retired) and Margo Edwards Hawaii Mapping Research Group Cover Figure. Oblique view of new eruption site on the Gakkel Ridge, observed with Seafloor Characterization and Mapping Pods (SCAMP) during the 1999 SCICEX mission. Sidescan observations are draped on a SCAMP-derived terrain model, with depths indicated by color-coded contour lines. Red dots are epicenters of earthquakes detected on the Ridge in 1999. (Data processing and visualization performed by Margo Edwards and Paul Johnson of the Hawaii Mapping Research Group.) This workshop was partially supported through Grant Number N00014-2-02-1-1120, awarded by the United States Office of Naval Research International Field Office. Partial funding was also provided by the International Arctic Science Committee (IASC), the US Polar Research Board, and the University of Hawaii. 2 Table of Contents 1. Introduction...............................................................................................................................5 Ron Macnab (GSC Retired) and Margo Edwards (HMRG) 2. A prototype 1:6 Million map....................................................................................................5 Martin Jakobsson, CCOM/JHC, University of New Hampshire, Durham NH, USA 3. Russian Arctic shelf data..........................................................................................................7 Volodja Glebovsky, VNIIOkeangeologia, St. Petersburg, Russia 4. -
Chapter 7 Arctic Oceanography; the Path of North Atlantic Deep Water
Chapter 7 Arctic oceanography; the path of North Atlantic Deep Water The importance of the Southern Ocean for the formation of the water masses of the world ocean poses the question whether similar conditions are found in the Arctic. We therefore postpone the discussion of the temperate and tropical oceans again and have a look at the oceanography of the Arctic Seas. It does not take much to realize that the impact of the Arctic region on the circulation and water masses of the World Ocean differs substantially from that of the Southern Ocean. The major reason is found in the topography. The Arctic Seas belong to a class of ocean basins known as mediterranean seas (Dietrich et al., 1980). A mediterranean sea is defined as a part of the world ocean which has only limited communication with the major ocean basins (these being the Pacific, Atlantic, and Indian Oceans) and where the circulation is dominated by thermohaline forcing. What this means is that, in contrast to the dynamics of the major ocean basins where most currents are driven by the wind and modified by thermohaline effects, currents in mediterranean seas are driven by temperature and salinity differences (the salinity effect usually dominates) and modified by wind action. The reason for the dominance of thermohaline forcing is the topography: Mediterranean Seas are separated from the major ocean basins by sills, which limit the exchange of deeper waters. Fig. 7.1. Schematic illustration of the circulation in mediterranean seas; (a) with negative precipitation - evaporation balance, (b) with positive precipitation - evaporation balance. -
Biodiversity of the Antarctic Flora
CORE Metadata, citation and similar papers at core.ac.uk Provided by NERC Open Research Archive 1 1 Original Article 2 Diversity and biogeography of the Antarctic flora 3 4 Helen J. Peat, Andrew Clarke & Peter Convey 5 6 British Antarctic Survey, Natural Environment Research Council, High Cross, Madingley Rd, 7 Cambridge, CB3 0ET, UK. 8 E-mail: [email protected] 9 __________________________________________________________________________ 10 11 ABSTRACT 12 13 Aim To establish how well the terrestrial flora of the Antarctic has been sampled, how well 14 the flora is known, and to determine the major patterns in diversity and biogeography. 15 16 Location Antarctica south of 60°S, together with the South Sandwich Islands, but excluding 17 South Georgia, Bouvetøya and the periantarctic islands. 18 19 Methods Plant occurrence data were collated from herbarium specimens and literature 20 records, and assembled into the Antarctic Plant Database. Distributional patterns were 21 analysed using a geographic information system. Biogeographic patterns were determined 22 with a variety of multivariate statistics. 23 24 Results Plants have been recorded from throughout the Antarctic including all latitudes 25 between 60°S and 86°S. Species richness declines with latitude along the Antarctic 26 Peninsula, but there was no evidence for a similar cline in Victoria Land and the 27 Transantarctic mountains. MDS ordinations showed that the species composition of the 28 South Orkney, South Shetland Islands and the north western Antarctic Peninsula are very 29 similar to each other, as are the floras of different regions in continental Antarctica. However 30 they also suggest that the eastern Antarctic Peninsula flora is more similar to the flora of the 31 southern Antarctic Peninsula than to the continental flora (with which it has traditionally been 32 linked). -
Differentially Expressed Genes Match Bill Morphology and Plumage Despite Largely Undifferentiated Genomes in a Holarctic Songbird
Molecular Ecology (2015) doi: 10.1111/mec.13140 Differentially expressed genes match bill morphology and plumage despite largely undifferentiated genomes in a Holarctic songbird NICHOLAS A. MASON*† and SCOTT A. TAYLOR*† *Department of Ecology and Evolutionary Biology, Cornell University, 215 Tower Rd., Ithaca, NY 14853, USA, †Fuller Evolutionary Biology Program, Laboratory of Ornithology, Cornell University, 159 Sapsucker Woods Road, Ithaca, NY 14850, USA Abstract Understanding the patterns and processes that contribute to phenotypic diversity and speciation is a central goal of evolutionary biology. Recently, high-throughput sequencing has provided unprecedented phylogenetic resolution in many lineages that have experienced rapid diversification. The Holarctic redpoll finches (Genus: Acanthis) provide an intriguing example of a recent, phenotypically diverse lineage; traditional sequencing and genotyping methods have failed to detect any genetic differences between currently recognized species, despite marked variation in plumage and mor- phology within the genus. We examined variation among 20 712 anonymous single nucleotide polymorphisms (SNPs) distributed throughout the redpoll genome in com- bination with 215 825 SNPs within the redpoll transcriptome, gene expression data and ecological niche modelling to evaluate genetic and ecological differentiation among currently recognized species. Expanding upon previous findings, we present evidence of (i) largely undifferentiated genomes among currently recognized species; (ii) substantial niche -
Gregory J. Jordan, 7 J. M. Kale Sniderman, 8 Andrew Allen
American Journal of Botany 101 ( 12 ): 2121 – 2135 , 2014 . P ALEO-ANTARCTIC RAINFOREST INTO THE MODERN OLD WORLD TROPICS: THE RICH PAST AND THREATENED FUTURE OF THE “SOUTHERN WET FOREST SURVIVORS” 1 R OBERT M. KOOYMAN , 2,3,12 P ETER W ILF , 4 V IVIANA D. BARREDA , 5 R AYMOND J. CARPENTER , 6 G REGORY J. JORDAN , 7 J. M. KALE S NIDERMAN , 8 A NDREW A LLEN , 2 T IMOTHY J. BRODRIBB , 7 D ARREN C RAYN , 9 T AYLOR S. FEILD , 9 S HAWN W . L AFFAN , 10 C HRISTOPHER H. LUSK , 11 M AURIZIO R OSSETTO , 3 AND P ETER H . W ESTON 3 2 Department of Biological Sciences, Macquarie University, North Ryde 2113, Sydney, Australia; 3 National Herbarium of NSW, Royal Botanic Gardens and Domain Trust, Mrs Macquaries Road, Sydney 2000, Australia; 4 Department of Geosciences, Pennsylvania State University, University Park, Pennsylvania 16802, USA; 5 Museo Argentino de Ciencias Naturales, CONICET, División Paleobot ánica, Av. Ángel Gallardo 470, C1405DJR Buenos Aires, Argentina; 6 School of Earth and Environmental Sciences, Benham Bldg DX 650 312, University of Adelaide, South Australia, Australia; 7 School of Biological Sciences, University of Tasmania, Private Bag 55 Hobart, 7001 Tasmania, Australia; 8 School of Earth Sciences, University of Melbourne, Melbourne 3010, Australia; 9 Australian Tropical Herbarium, School of Marine and Tropical Biology, James Cook University, Cairns, Australia; 10 Centre for Ecosystem Science, School of Biological, Earth and Environmental Sciences, University of New South Wales, Kensington 2052, Sydney, Australia; and 11 School of Science, University of Waikato, Private Bag 3105, Hamilton, New Zealand • Premise of study: Have Gondwanan rainforest fl oral associations survived? Where do they occur today? Have they survived continuously in particular locations? How signifi cant is their living fl oristic signal? We revisit these classic questions in light of signifi cant recent increases in relevant paleobotanical data.