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Draft ASMA Plan for Dry Valleys
Measure 18 (2015) Management Plan for Antarctic Specially Managed Area No. 2 MCMURDO DRY VALLEYS, SOUTHERN VICTORIA LAND Introduction The McMurdo Dry Valleys are the largest relatively ice-free region in Antarctica with approximately thirty percent of the ground surface largely free of snow and ice. The region encompasses a cold desert ecosystem, whose climate is not only cold and extremely arid (in the Wright Valley the mean annual temperature is –19.8°C and annual precipitation is less than 100 mm water equivalent), but also windy. The landscape of the Area contains mountain ranges, nunataks, glaciers, ice-free valleys, coastline, ice-covered lakes, ponds, meltwater streams, arid patterned soils and permafrost, sand dunes, and interconnected watershed systems. These watersheds have a regional influence on the McMurdo Sound marine ecosystem. The Area’s location, where large-scale seasonal shifts in the water phase occur, is of great importance to the study of climate change. Through shifts in the ice-water balance over time, resulting in contraction and expansion of hydrological features and the accumulations of trace gases in ancient snow, the McMurdo Dry Valley terrain also contains records of past climate change. The extreme climate of the region serves as an important analogue for the conditions of ancient Earth and contemporary Mars, where such climate may have dominated the evolution of landscape and biota. The Area was jointly proposed by the United States and New Zealand and adopted through Measure 1 (2004). This Management Plan aims to ensure the long-term protection of this unique environment, and to safeguard its values for the conduct of scientific research, education, and more general forms of appreciation. -
Authors' Response to Reviews Dear Editors, We Appreciate the Two
Authors’ Response to Reviews Dear editors, We appreciate the two reviewers’ thoughtful comments and detailed assessment of the archive. We have provided our detailed responses to the both reviewers’ questions in red, as well as the revised manuscript with associated tracked changes, below. Warwick Vincent I could not find the supplementary material (Table S1) that is referred to. Thank you for bringing this to our attention, we have uploaded the supplementary material (Table S1) with the revised manuscript. Concerning data quality: the data set is accessible via the given identifier, and is complete as a first collection that can now be updated. The data quality is variable – some images are only poorly resolved and have many imperfections (e.g. dust on the slide lens or scanner, poor color rendition), and the metadata are not always complete be-cause the exact date is unknown. The authors might note this by saying that the quality and resolution are variable, but an inclusive approach was taken to maximize the scope of the database. We agree that it is important to note the variable quality of the data and metadata and have added an explanation to the revised manuscript as suggested. Further points: The images are taken by many people and "copyright for each item re-mains with the respective contributor" – in that case, how would permission be obtained to reproduce any of these materials, for example in another publication? Unless otherwise stated, copyright for each item in the database remains with the respective contributor. If a reader wanted to gain permission to use the material in another venue, they would need to contact us or the copyright holder directly. -
Mcmurdo Dry Valleys: Exploring Antarctica As a Mars Analogue
49th Lunar and Planetary Science Conference 2018 (LPI Contrib. No. 2083) 2627.pdf MCMURDO DRY VALLEYS: EXPLORING ANTARCTICA AS A MARS ANALOGUE. Hunter Quintal1, James Head1, Ashley Palumbo1, James Dickson2, 1Department of Earth, Environmental and Planetary Sciences, Brown University, Providence, RI 02912 USA ([email protected]), 2Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125 USA. Introduction: The current martian climate is hyper- a meandering channel until it ponds in Lake Vanda arid and hypothermal, similar in many ways to the cli- (~160 m above sea level) (Fig. 1) [11]. mate of the Antarctic McMurdo Dry Valleys (MDV) [1]. This climate has persisted throughout the Amazonian (past ~3 Gyr) on Mars. Geologic evidence, including the widespread fluvial valley networks (VNs) [2] and lakes [3], suggest that the earlier Late Noachian and Early Hesperian (~3.7 Ga) climate may have been much dif- ferent than today, with abundant stable liquid water at the surface and persistent rainfall to form these fluvial and lacustrine features [4]. In contrast with this geologic evidence, recent climate models have suggested that the early climate may have been “cold and icy”, character- ized by mean annual temperatures far below the melting point of water (~225 K), an adiabatic cooling effect [5], and ice distributed across the southern highlands [6]. In Fig. 1. Schematic map view of Southfork Valley Antarctica, highlight- this climate scenario, transient or punctuated heating ing the path of the Onyx River. From [11]. McMurdo Dry Valleys Climate: We utilized events would be responsible for ice melting, liquid water Long-Term Ecological Research (LTER) data [12] to runoff, ponding at the surface, and formation of the VNs determine which climatic factors appear best correlated and lakes [7]. -
Original Unedited Manuscript
Importance of environmental factors over habitat connectivity in shaping bacterial communities in microbial mats and bacterioplankton in an Antarctic freshwater system Downloaded from https://academic.oup.com/femsec/advance-article/doi/10.1093/femsec/fiab044/6174672 by University of Waikato user on 01 April 2021 Ramoneda J.1,2, Hawes I.3, Pascual-García A.4, Mackey T.J.5,6, Sumner D.Y.5, Jungblut A.D.1* 1 Life Sciences Department, Natural History Museum, Cromwell Road, London, SW7 5BD, UK. 2 Present affiliation: Department of Environmental Microbiology, Swiss Federal Institute of Aquatic Science and Technology (Eawag), 8600 Dübendorf, Switzerland. 3 Coastal Marine Field Station, University of Waikato, 58 Cross Road, Tauranga 3110, New Zealand. 4 Theoretical Biology, Institute of Integrative Biology, ETH Zürich, Universitätstrasse 16, Zürich, Switzerland. 5 Department of Earth and Planetary Sciences, University of California–Davis, 1 Shields Avenue, Davis, CA 95618, United States of America 6Present affiliation: Department of Earth and Planetary Sciences, University of New Mexico, 221 Yale Boulevard NE, Albuquerque, NM 87131, United States * Corresponding author: Anne D. Jungblut, Life Sciences Department, Natural History Museum, Cromwell Road, 18 SW7 5BD, United Kingdom, email: [email protected]; phone: +44 (0) 20 7242 5285 Keywords: biofilm, bacterioplankton, freshwater, 16S rRNA gene, McMurdo Dry Valleys, Antarctica ORIGINAL UNEDITED MANUSCRIPT © The Author(s) 2021. Published by Oxford University Press on behalf of FEMS. All rights reserved. For permissions, please e-mail: [email protected] Abstract Freshwater ecosystems are considered hotspots of biodiversity in Antarctic polar deserts. Anticipated warming is expected to change the hydrology of these systems due to increased Downloaded from https://academic.oup.com/femsec/advance-article/doi/10.1093/femsec/fiab044/6174672 by University of Waikato user on 01 April 2021 meltwater and reduction of ice cover, with implications for environmental conditions and physical connectivity between habitats. -
Environmental Controls and Habitat Connectivity of Phototrophic Microbial Mats And
bioRxiv preprint doi: https://doi.org/10.1101/2020.07.13.200626; this version posted July 14, 2020. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-NC-ND 4.0 International license. 1 Environmental controls and habitat connectivity of phototrophic microbial mats and 2 bacterioplankton communities in an Antarctic freshwater system 3 4 Ramoneda J.1,2, Hawes I.3, Pascual-García A.4, Mackey T.J.5,6, Sumner D.Y.5, Jungblut 5 A.D.1* 6 7 1 Life Sciences Department, Natural History Museum, Cromwell Road, London, SW7 5BD, 8 UK. 9 2 Present affiliation: Group of Plant Nutrition, Department of Environmental Systems Science, 10 ETH Zürich, Eschikon 33, Lindau, Switzerland. 11 3 Coastal Marine Field Station, University of Waikato, 58 Cross Road, Tauranga 3110, New 12 Zealand. 13 4 Theoretical Biology, Institute of Integrative Biology, ETH Zürich, Universitätstrasse 16, 14 Zürich, Switzerland. 15 5 Department of Earth and Planetary Sciences, University of California–Davis, 1 Shields 16 Avenue, Davis, CA 95618, United States of America 17 6Present affiliation: Department of Earth and Planetary Sciences, University of New Mexico, 18 221 Yale Boulevard NE, Albuquerque, NM 87131 19 20 * Corresponding author: 21 Anne D. Jungblut, Life Sciences Department, Natural History Museum, Cromwell Road, 18 22 SW7 5BD, United Kingdom, email: [email protected]; phone: +44 (0) 20 7242 5285 23 24 25 Running title: Antarctic freshwater bacterial communities 26 1 bioRxiv preprint doi: https://doi.org/10.1101/2020.07.13.200626; this version posted July 14, 2020. -
The Antarctic Treaty
The Antarctic Treaty Measures adopted at the Thirty-fourth Consultative Meeting held at Buenos Aires, 20 June – 1 July 2011 Presented to Parliament by the Secretary of State for Foreign and Commonwealth Affairs by Command of Her Majesty January 2014 Cm 8809 £31.50 © Crown copyright 2014 You may re-use this information (excluding logos) free of charge in any format or medium, under the terms of the Open Government Licence. To view this licence, visit http://www.nationalarchives.gov.uk/doc/open-government-licence or email. [email protected] Where we have identified any third party copyright information you will need to obtain permission from the copyright holders concerned. Any enquiries regarding this publication should be sent to us at Treaty Section, Foreign and Commonwealth Office, King Charles Street, London, SW1A 2AH. ISBN: 9780101880923 Printed in the UK by The Stationery Office Limited on behalf of the Controller of Her Majesty’s Stationery Office ID P002619602 01/14 36734 19585 Printed on paper containing 30% recycled fibre content minimum. MEASURES ADOPTED AT THE THIRTY-FOURTH ANTARCTIC TREATY CONSULTATIVE MEETING Buenos Aires, Argentina 20 June – 1 July 2011 The Measures1 adopted at the Thirty-fourth Antarctic Treaty Consultative Meeting are reproduced below from the Final Report of the Meeting. In accordance with Article IX, paragraph 4, of the Antarctic Treaty, the Measures adopted at Consultative Meetings become effective upon approval by all Contracting Parties whose representatives were entitled to participate in the meeting at which they were adopted (i.e. all the Consultative Parties). The full text of the Final Report of the Meeting, including the Decisions and Resolutions adopted at that Meeting and colour copies of the maps found in this command paper, is available on the website of the Antarctic Treaty Secretariat at www.ats.aq/documents. -
View East Toward Ross Island and Mcmurdo Sound
This dissertation has been microfilmed exactly as received 69-22,155 JONES, Lois Marilyn, 1934- THE APPLICATION OF STRONTIUM ISOTOPES AS NATURAL TRACERS: THE ORIGIN OF THE SALTS IN THE LAKES AND SOILS OF SOUTHERN VICTORIA LAND, ANTARCTICA. The Ohio State University, Ph.D., 1969 Geology University Microiilms, Inc., Ann Arbor, Michigan THE APPLICATION OP STRONTIUM ISOTOPES AS NATURAL TRACERS: THE ORIGIN OF THE SALTS IN THE LAKES AND SOILS OF SOUTHERN VICTORIA LAND, ANTARCTICA DISSERTATION Presented in Partial Fullfillment of the Requirements for the Degree Doctor of Philosophy in the Graduate School of The Ohio State University by Lois Marilyn Jones, B. Sc,, M. Sc The Ohio State University 1969 Approved by Adviser Department of Geology PLEASE NOTE: Several pages contain colored illustrations. Filmed in the best possible way. UNIVERSITY MICROFILMS ACKNOWLEDGMENTS I wish to express my gratitude to Professor Gunter Faure, whose advice, discussions, and encour agement have been indispensible in bringing this study to a satisfactory conclusion. This study also could not have been possible without the generosity of numerous people who willingly contributed valuable samples utilized in this investi gation. Dr. Derry D. Koob contributed the excellent series of samples from depth profiles of Lakes Vanda and Bonney and the sample from Don Juan Pond. Mr. R. E. Behling and Dr. K. R. Everett contributed the samples of soil from the vicinity of the Meserve Glacier and from Taylor Valley, as well as samples of salts and meltwater. Mr. H. J. E. Montigny collected the soils and water samples from the floor of Wright Valley and the extensive suites of rock samples from the basement complex of the valley. -
Mcmurdo Dry Valleys, Southern Victoria Land
Measure 18 (2015) Management Plan for Antarctic Specially Managed Area No. 2 MCMURDO DRY VALLEYS, SOUTHERN VICTORIA LAND Introduction The McMurdo Dry Valleys are the largest relatively ice-free region in Antarctica with approximately thirty percent of the ground surface largely free of snow and ice. The region encompasses a cold desert ecosystem, whose climate is not only cold and extremely arid (in the Wright Valley the mean annual temperature is –19.8°C and annual precipitation is less than 100 mm water equivalent), but also windy. The landscape of the Area contains mountain ranges, nunataks, glaciers, ice-free valleys, coastline, ice-covered lakes, ponds, meltwater streams, arid patterned soils and permafrost, sand dunes, and interconnected watershed systems. These watersheds have a regional influence on the McMurdo Sound marine ecosystem. The Area’s location, where large-scale seasonal shifts in the water phase occur, is of great importance to the study of climate change. Through shifts in the ice-water balance over time, resulting in contraction and expansion of hydrological features and the accumulations of trace gases in ancient snow, the McMurdo Dry Valley terrain also contains records of past climate change. The extreme climate of the region serves as an important analogue for the conditions of ancient Earth and contemporary Mars, where such climate may have dominated the evolution of landscape and biota. The Area was jointly proposed by the United States and New Zealand and adopted through Measure 1 (2004). This Management Plan aims to ensure the long-term protection of this unique environment, and to safeguard its values for the conduct of scientific research, education, and more general forms of appreciation. -
Mcmurdo Dry Valleys
McMurdoMcMurdo DryDry ValleysValleys Long Term Ecological Research he McMurdo Dry Valleys (MCM) Long Term Ecological Education and Outreach TT Research (LTER) Program is an interdisciplinary and From Internet web journals about life in Antarctica, to assisting multidisciplinary study of the aquatic and terrestrial ecosystems high school in an ice-free region of Antarctica. MCM joined the National students with Science Foundation's LTER Network in 1993. chemical analysis of Site Description stream samples, The McMurdo Dry Valleys (77°30'S 163°00'E) on the shore of to an interactive McMurdo Sound, 2,200 miles (3,500 km) due south of New educational CD Zealand, form the for high school Taylor Valley largest relatively teachers based ice-free area on MCM (approximately research, 2 4,800 km ) on the scientists at Antarctic MCM strive to This children’s book describes McMurdo Dry Valleys research and features artwork by elementary school children from continent. These engage the countries all over the world that have been involved in research in the dry valleys of the Antarctic. public's interest in science and ecology. MCM researcher Diane McKnight has also published a children's book, The Lost Seal, which describes a true encounter MCM LTER ice-free areas of Antarctica between researchers and a live seal in www.mcmlter.org display a sharp contrast to the dry valleys. The story features most other ecosystems in artwork by children from four countries Byrd Polar Research the world, which exist and introduces readers to Antarctic Center under far more moderate environmental conditions. science. On the web at: 108 Scott Hall The average temperature is -19˚C, maximum: 11.8˚C, www.mcmlter.org/lostseal. -
Aspects of Nutrient Behavior in Lake Vanda
Aspects of nutrient behavior in Lake Vanda CANFIELD DONALD E. and WILLIAM J. GREEN School of Interdisciplinary Studies Miami University Oxford, Ohio 45056 Lake Vanda, located in Wright Valley, Antarctica, has been the subject of considerable limnological attention over the past 20 years. The major ion chemistry and physical limnology of the lake have been discussed by numerous authors including (An- gino, Armitage, and Tash (1965); Green and Canfield (in prepa- ration-a); Ragotzkie and Likens (1964); Toni and Yamagata .14 .1 .1 30 1 3 5 79t1 13 15 17 19 (1981); and Wilson (1964). The origin of the lakes salts continues Time to be a somewhat perplexing issue and has been debated by several of the above authors, as well as by Cartwright and Harris Figure 1. Phosphorus concentration vs. time for the Onyx River. (1981). Notably absent from the literature, however, is a detailed ["p. gil" denotes micrograms per liter; "P" denotes phosphorus; discussion of the dynamics of nutrient behavior within the "PO4-P" is a standard oceanographic (and limnologic) unit where Vanda-Onyx system. This paper serves as a continuing report the weight of the nutrient species (i.e., phosphorus and nitrogen) is on the activities of our field party during the 1980-1981 field expressed per unit volume and the prescript PO 4, NH3, NO3, expres- season, with an emphasis on the nutrient chemistry of Lake ses the form of the nutrient species.] Vanda and the Onyx River. Lake Vanda has been classified as an ultra -oligotrophic lake (Goldman, Mason, and Hobbie 1967) and is recognized as being one of the least biologically productive and clearest lakes in the world. -
Physical and Chemical Controls on the Abundance and Composition of Stream Microbial Mats from the Mcmurdo Dry Valleys, Antarctica
PHYSICAL AND CHEMICAL CONTROLS ON THE ABUNDANCE AND COMPOSITION OF STREAM MICROBIAL MATS FROM THE MCMURDO DRY VALLEYS, ANTARCTICA by TYLER JOE KOHLER B.S., Kansas State University, 2007 M.S., University of Nebraska, 2010 A thesis submitted to the Faculty of the Graduate School of the University of Colorado in partial fulfillment of the requirement for the degree of Doctor of Philosophy Environmental Studies Program 2015 This thesis entitled: Physical and chemical controls on the abundance and composition of Dry Valley stream microbial mats written by Tyler Joe Kohler has been approved for the Environmental Studies Program Diane McKnight Patrick Kociolek Date The final copy of this thesis has been examined by the signatories, and we find that both the content and the form meet acceptable presentation standards of scholarly work in the above mentioned discipline. Kohler, Tyler Joe (Ph.D., Environmental Studies) Physical and chemical controls on the abundance and composition of stream microbial mats from the McMurdo Dry Valleys, Antarctica Thesis directed by Professor Diane M. McKnight ABSTRACT The McMurdo Dry Valleys of Antarctica are a cold, dry desert, yet perennial microbial mats are abundant in the ephemeral glacial meltwater streams that flow during austral summers. Three types of mats are present (orange, black, and green), and are primarily comprised of filamentous cyanobacteria, Nostoc, and chlorophytes, respectively. Mat types furthermore occupy distinct habitats within streams, utilizing the benthos, hyporheic zone, and water column, which expose them to different environmental conditions. Due to a lack of lateral inflows, allochthonous organic inputs, and negligible grazing activity, these streams are ideal for the controlled ecological study of microbial mats. -
A Pilot Framework and Gap Analysis Towards Developing a Fluvial Classification System in the Ross Sea Region Antarctica
PCAS 17 (2014/2015) Supervised Project A PILOT FRAMEWORK AND GAP ANALYSIS TOWARDS DEVELOPING A FLUVIAL CLASSIFICATION SYSTEM IN THE ROSS SEA REGION ANTARCTICA Lorna Louise Thurston Student ID: 12670481 Abstract: An integrated literature review has been undertaken with regards to the hydrological regime and fluvial geomorphology of the Ross Sea Region, Antarctica. The findings have been applied to develop a pilot framework for a process-based classification system of channels, ponds and lakes, and to identify gaps in knowledge that need to be addressed in order for the classification system to be developed further. The intention of the process-based classification system is that, once developed, it will be applied as a tool to help understand fluvial response to climate change and an increasing human footprint in the Ross Sea Region. In this regard, it would contribute towards a contemporary project - Assessing the Sensitivity of Dry Valleys to Change. It may also be useful for other applications, such as ecological research, and applicable to other regions of Antarctica. Several gaps in research have been identified that need to be addressed in order to integrate knowledge of the hydrological regime and fluvial morphology and subsequently develop a process-based classification system. In no particular order, these gaps include knowledge of: the spatial distribution of channel morphologies; fluvial morphological behaviour under heavily transport- and supply- limited conditions; the formation and desiccation of ponds, and their associated