Mcmurdo Dry Valleys, Southern Victoria Land
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Osl Dating of High-Elevation Alluvial Sediments: Mcmurdo Dry
OSL DATING OF HIGH-ELEVATION ALLUVIAL SEDIMENTS: MCMURDO DRY VALLEYS, ANTARCTICA A Thesis Submitted to the Graduate Faculty of the North Dakota State University of Agriculture and Applied Science By Meridith Ann Ramsey In Partial Fulfillment of the Requirements for the Degree of MASTER OF SCIENCE Major Program: Environmental and Conservation Science November 2014 Fargo, North Dakota North Dakota State University Graduate School Title OSL DATING OF HIGH-ELEVATION ALLUVIAL SEDIMENTS: MCMURDO DRY VALLEYS, ANTARCTICA By Meridith Ann Ramsey The Supervisory Committee certifies that this disquisition complies with North Dakota State University’s regulations and meets the accepted standards for the degree of MASTER OF SCIENCE SUPERVISORY COMMITTEE: Kenneth Lepper Chair Adam Lewis Lisa Montplaisir Approved: 04/16/2015 Eakalak Khan Date Department Chair ABSTRACT High-elevation alluvial fans in the McMurdo Dry Valleys are a record of short-term, occasional melting events along the margins of the East Antarctic Ice Sheet. Sediment samples were dated from five fans using Optically Stimulated Luminescence (OSL) dating. OSL dates the time since quartz grains were last exposed to sunlight; all sample preparation takes place in a dark room. Thirteen samples were dated for this thesis, the ages were stratigraphically consistent and ranged from 1.1 ka to 105.9 ka. Clusters of fan activity occurred between 1.1 and 3.1 ka and 8.1 and 11.1 ka. The melting events appear to be linked to insolation, with periods of fan activity occurring usually at times of increased mean annual insolation. The alluvial fans show promise as a possible archive for climate proxies in this region of Antarctica. -
Methylmercury Fate in the Hypersaline Environment of the Great Salt Lake: a Critical Review of Current Knowledge
Utah State University DigitalCommons@USU All Graduate Plan B and other Reports Graduate Studies 12-2013 Methylmercury Fate in the Hypersaline Environment of the Great Salt Lake: A Critical Review of Current Knowledge Danielle Barandiaran Utah State University Follow this and additional works at: https://digitalcommons.usu.edu/gradreports Part of the Soil Science Commons Recommended Citation Barandiaran, Danielle, "Methylmercury Fate in the Hypersaline Environment of the Great Salt Lake: A Critical Review of Current Knowledge" (2013). All Graduate Plan B and other Reports. 332. https://digitalcommons.usu.edu/gradreports/332 This Thesis is brought to you for free and open access by the Graduate Studies at DigitalCommons@USU. It has been accepted for inclusion in All Graduate Plan B and other Reports by an authorized administrator of DigitalCommons@USU. For more information, please contact [email protected]. METHYLMERCURY FATE IN THE HYPERSALINE ENVIRONMENT OF THE GREAT SALT LAKE: A CRITICAL REVIEW OF CURRENT KNOWLEDGE By Danielle Barandiaran A paper submitted in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE in Soil Science Approved: Astrid Jacobson Jeanette Norton Major Professor Committee Member - Paul Grossl Teryl Roper Committee Member Department Head UTAH STATE UNIVERSITY Logan, Utah 2013 Copyright © Danielle Barandiaran 2013 All Rights Reserved iii ABSTRACT Methylmercury Fate in the Hypersaline Environment of the Great Salt Lake: A Critical Review of Current Knowledge by Danielle Barandiaran, Master of Science Utah State University, 2013 Major Professor: Dr. Astrid R. Jacobson Department: Plants, Soils & Climate Methylmercury (MeHg) is a highly potent neurotoxic form of the environmental pollutant Mercury (Hg). -
A NEWS BULLETIN Published Quarterly by the NEW ZEALAND ANTARCTIC SOCIETY (INC)
A NEWS BULLETIN published quarterly by the NEW ZEALAND ANTARCTIC SOCIETY (INC) An English-born Post Office technician, Robin Hodgson, wearing a borrowed kilt, plays his pipes to huskies on the sea ice below Scott Base. So far he has had a cool response to his music from his New Zealand colleagues, and a noisy reception f r o m a l l 2 0 h u s k i e s . , „ _ . Antarctic Division photo Registered at Post Ollice Headquarters. Wellington. New Zealand, as a magazine. II '1.7 ^ I -!^I*"JTr -.*><\\>! »7^7 mm SOUTH GEORGIA, SOUTH SANDWICH Is- . C I R C L E / SOUTH ORKNEY Is x \ /o Orcadas arg Sanae s a Noydiazarevskaya ussr FALKLAND Is /6Signyl.uK , .60"W / SOUTH AMERICA tf Borga / S A A - S O U T H « A WEDDELL SHETLAND^fU / I s / Halley Bav3 MINING MAU0 LAN0 ENOERBY J /SEA uk'/COATS Ld / LAND T> ANTARCTIC ••?l\W Dr^hnaya^^General Belgrano arg / V ^ M a w s o n \ MAC ROBERTSON LAND\ '■ aust \ /PENINSULA' *\4- (see map betowi jrV^ Sobldl ARG 90-w {■ — Siple USA j. Amundsen-Scott / queen MARY LAND {Mirny ELLSWORTH" LAND 1, 1 1 °Vostok ussr MARIE BYRD L LAND WILKES LAND ouiiiv_. , ROSS|NZJ Y/lnda^Z / SEA I#V/VICTORIA .TERRE , **•»./ LAND \ /"AOELIE-V Leningradskaya .V USSR,-'' \ --- — -"'BALLENYIj ANTARCTIC PENINSULA 1 Tenitnte Matianzo arg 2 Esptrarua arg 3 Almirarrta Brown arc 4PttrtlAHG 5 Otcipcion arg 6 Vtcecomodoro Marambio arg * ANTARCTICA 7 Arturo Prat chile 8 Bernardo O'Higgins chile 1000 Miles 9 Prasid«fTtB Frei chile s 1000 Kilometres 10 Stonington I. -
Microbial Dispersal Limitation to Isolated Soil Habitats in the Mcmurdo Dry Valleys
bioRxiv preprint doi: https://doi.org/10.1101/493411; this version posted December 13, 2018. The copyright holder for this preprint (which was not certified by peer review) is the author/funder. All rights reserved. No reuse allowed without permission. 1 Microbial dispersal limitation to isolated soil habitats in the McMurdo Dry Valleys 2 of Antarctica 3 4 Stephen D.J. Archer1,2, Kevin C. Lee2, Tancredi Caruso3, Teruya Maki4, Charles K. Lee5, 5 Don A. Cowan6, Fernando T. Maestre7, Stephen B. Pointing1,8 6 7 1 Yale-NUS College, National University of Singapore, Singapore 138527 8 2 Institute for Applied Ecology New Zealand, Auckland University of Technology, Auckland 9 1142, New Zealand 10 3 School of Biological Sciences and Global Institute for Food Security, Queen's University 11 Belfast, Belfast BT9 7BL, Northern Ireland, UK 12 4 Department of Chemical Engineering, Kanazawa University, Kanazawa 920-1192, Japan 13 5 International Centre for Terrestrial Antarctic Research, University of Waikato, Hamilton 14 3240, New Zealand 15 6 Centre for Microbial Ecology and Genomics, University of Pretoria, Pretoria 0002, South 16 Africa 17 7 Departamento de Biología y Geología, Física y Química Inorgánica, Escuela Superior de 18 Ciencias Experimentales y Tecnología, Universidad Rey Juan Carlos, C/ Tulipán s/n, 28933 19 Móstoles, Spain 20 8 Department of Biological Sciences, National University of Singapore, Singapore 117558 21 1 bioRxiv preprint doi: https://doi.org/10.1101/493411; this version posted December 13, 2018. The copyright holder for this preprint (which was not certified by peer review) is the author/funder. All rights reserved. -
(Bio)Chemical Complexity in Icy Satellites, with a Focus on Europa
Searching for (bio)chemical complexity in icy satellites, with a focus on Europa Contact Scientist: Olga Prieto-Ballesteros ([email protected]) Centro de Astrobiología (CSIC-INTA) Ctra. De Ajalvir km. 4, 28850 Torrejón de Ardoz. Madrid. Spain VOYAGE 2050. Searching for (bio)chemical complexity in icy satellites, with a focus on Europa TABLE OF CONTENTS TABLE OF CONTENTS 1 1. EXECUTIVE SUMMARY 2 2. THE SCIENCE QUESTION 3 2.1 BASIS OF THE STRATEGY TO SEARCH FOR LIFE IN THE SOLAR SYSTEM 3 2.2 THE SEARCH FOR COMPLEXITY 5 3. THE SPACE MISSION STRATEGY 7 3.1 MISSION DESTINATION: EUROPA 7 3.1.1 Main elements of the mission 8 3.1.2 Exploration of the plumes 10 3.2 THE MISSION IN A WORLDWIDE CONTEXT 11 4. TECHNOLOGICAL CHALLENGES 12 4.1 Europa orbiter 12 4.2 Europa lander 12 4.3 Europa ocean explorer 13 4.4 Europa jumper 14 4.5 Key Instrumentation 14 5. MEMBERS OF THE PROPOSER TEAM 16 6. REFERENCES 18 1 VOYAGE 2050. Searching for (bio)chemical complexity in icy satellites, with a focus on Europa SEARCHING FOR (BIO)CHEMICAL COMPLEXITY IN ICY SATELLITES, WITH A FOCUS ON EUROPA 1. EXECUTIVE SUMMARY Organic chemistry is ubiquitous in the Solar System. A significant repertoire of organic molecules has been detected in bodies outside the Earth (e.g., in meteorites, in cometary nuclei, on Mars or on icy moons), but none of the detected organic mixtures has enough complexity to indicate Life. There are a number of potentially habitable bodies in the solar system where water, chemical gradients and energy coexist, in particular Mars and the icy moons of the giant planets. -
Mcmurdo Dry Valleys, Southern Victoria Land
Measure 1 (2004) Annex Management Plan for Antarctic Specially Managed Area No. 2 MCMURDO DRY VALLEYS, SOUTHERN VICTORIA LAND 1. Description of values to be protected and activities to be managed The McMurdo Dry Valleys are characterized as 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 glaciers, mountain ranges, ice-covered lakes, 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 is characterized by unique ecosystems of low biodiversity and reduced food web complexity. However, as the largest ice-free region in Antarctica, the McMurdo Dry Valleys also contain relatively diverse habitats compared with other ice-free areas. -
Microclimate and Weathering Processes in the Area of Darwin
relationship between the folds reported by Burgess (in Findlay, R. H. 1978. Provisional report on the geology of the region press) and those described here cannot be determined from between the Renegar and Blue Glaciers, Antarctica. New Zealand present evidence. Antarctic Record, 1, 39-44. Skinner (1964, 1965) named the rocks at Mt. Madison the Grindley, G. W., McGregor, V. R., and Walcott, R. I. 1964. Outline Selborne Marble and distinguished them from the Shack- of the geology of the Nimrod-Beardmore-Axel Heiberg Glaciers region, Ross dependency. In Adie (Ed.), leton Limestone due to their higher metamorphic grade. He R. J. Antarctic geology. Amsterdam: North-Holland Publishing. suggested that they may be Precambrian in age, correlative with the Nimrod Group in the Miller Range (Grindley, Skinner, D. N. B. 1964, A summary of the geology of the region McGregor, and Walcott 1964). If this is the case, deforma- between Byrd and Starshot glaciers, south Victoria Land, In Adie (Ed.), Antarctic geology. Amsterdam: North-Holland tion at Mt. Madison is probably not related to the Shackle- R. J. Publishing. ton Limestone south of Byrd Glacier. Skinner, D. N. B. 1965. Petrographic criteria of the rock units To me, lithologies at Mt. Madison appear similar to those between the Byrd and Starshot Glaciers, south Victoria Land, of the Shackleton Limestone and pelitic Dick Formation Antarctica. New Zealand Journal of Geology and Geophysics, 8, (Skinner 1965), and I would suggest that the Selborne Mar- 292-303. ble is a metamorphosed equivalent of those two formations. Skinner, D. N. B. In press. Stratigraphy and structure of lower The metamorphic grade suggests an adjacent granitic pluton grade metasediments of Skelton Group, McMurdo Sound—Does north of Mt. -
University Microfilms, a XEROX Company, Ann Arbor, Michigan
I I 72-15,173 BEHLING, Robert Edward, 1941- PEDOLOGICAL DEVELOPMENT ON MORAINES OF THE MESERVE GLACIER, ANTARCTICA. The Ohio State University in cooperation with Miami (Ohio) University, Ph.D., 1971 Geology University Microfilms,A XEROX Company , Ann Arbor, Michigan PEDOLOGICAL DEVELOPMENT ON MORAINES OF THE MESERVE GLACIER, ANTARCTICA DISSERTATION Presented In Partial Fulfillment of the Requirements for the Degree Doctor of Philosophy in the Graduate School of The Ohio State University By Robert E. Behling, B.Sc., M*Sc. ***** The Ohio State University 1971 Approved by Adv Department f Geology PLEASE NOTE: Some pages have indistinct print. Filmed as received. University Microfilms, A Xerox Education Company ACKNOWLEDGEMENTS This study could not have been possible without the cooperation of faculty members of the departments of agronomy, mineralogy, and geology, I wish to thank Dr. R. P. Goldthwait as chairman of my committee, Dr. L. P. Wilding and Dr. R. T. Tettenhorst as members of my reading committee, as well as Dr. C. B. Bull and Dr. K. R. Everett for valuable assistance and criticism of the manuscript. A special thanks is due Dr. K. R. Everett for guidance during that first field season, and to Dr. F. Ugolini who first introduced me to the problems of weathering in cold deserts. Numerous people contributed to this end result through endless discussions: Dr. Lois Jones and Dr. P. Calkin receive special thanks, as do Dr. G. Holdsworth and Maurice McSaveney. Laboratory assistance was given by Mr. Paul Mayewski and R. W. Behling. Field logistic support in Antarctica was supplied by the U.S. -
The Ecology of Dunaliella in High-Salt Environments Aharon Oren
Oren Journal of Biological Research-Thessaloniki (2014) 21:23 DOI 10.1186/s40709-014-0023-y REVIEW Open Access The ecology of Dunaliella in high-salt environments Aharon Oren Abstract Halophilic representatives of the genus Dunaliella, notably D. salina and D. viridis, are found worldwide in salt lakes and saltern evaporation and crystallizer ponds at salt concentrations up to NaCl saturation. Thanks to the biotechnological exploitation of D. salina for β-carotene production we have a profound knowledge of the physiology and biochemistry of the alga. However, relatively little is known about the ecology of the members of the genus Dunaliella in hypersaline environments, in spite of the fact that Dunaliella is often the main or even the sole primary producer present, so that the entire ecosystem depends on carbon fixed by this alga. This review paper summarizes our knowledge about the occurrence and the activities of different Dunaliella species in natural salt lakes (Great Salt Lake, the Dead Sea and others), in saltern ponds and in other salty habitats where members of the genus have been found. Keywords: Dunaliella, Hypersaline, Halophilic, Great Salt Lake, Dead Sea, Salterns Introduction salt adaptation. A number of books and review papers When the Romanian botanist Emanoil C. Teodoresco have therefore been devoted to the genus [5-7]. How- (Teodorescu) (1866–1949) described the habitat of the ever, the ecological aspects of the biology of Dunaliella new genus of halophilic unicellular algae Dunaliella,it are generally neglected. A recent monograph did not was known from salterns and salt lakes around the devote a single chapter to ecological aspects, and con- Mediterranean and the Black Sea [1-3]. -
U.S. Advance Exchange of Operational Information, 2005-2006
Advance Exchange of Operational Information on Antarctic Activities for the 2005–2006 season United States Antarctic Program Office of Polar Programs National Science Foundation Advance Exchange of Operational Information on Antarctic Activities for 2005/2006 Season Country: UNITED STATES Date Submitted: October 2005 SECTION 1 SHIP OPERATIONS Commercial charter KRASIN Nov. 21, 2005 Depart Vladivostok, Russia Dec. 12-14, 2005 Port Call Lyttleton N.Z. Dec. 17 Arrive 60S Break channel and escort TERN and Tanker Feb. 5, 2006 Depart 60S in route to Vladivostok U.S. Coast Guard Breaker POLAR STAR The POLAR STAR will be in back-up support for icebreaking services if needed. M/V AMERICAN TERN Jan. 15-17, 2006 Port Call Lyttleton, NZ Jan. 24, 2006 Arrive Ice edge, McMurdo Sound Jan 25-Feb 1, 2006 At ice pier, McMurdo Sound Feb 2, 2006 Depart McMurdo Feb 13-15, 2006 Port Call Lyttleton, NZ T-5 Tanker, (One of five possible vessels. Specific name of vessel to be determined) Jan. 14, 2006 Arrive Ice Edge, McMurdo Sound Jan. 15-19, 2006 At Ice Pier, McMurdo. Re-fuel Station Jan. 19, 2006 Depart McMurdo R/V LAURENCE M. GOULD For detailed and updated schedule, log on to: http://www.polar.org/science/marine/sched_history/lmg/lmgsched.pdf R/V NATHANIEL B. PALMER For detailed and updated schedule, log on to: http://www.polar.org/science/marine/sched_history/nbp/nbpsched.pdf SECTION 2 AIR OPERATIONS Information on planned air operations (see attached sheets) SECTION 3 STATIONS a) New stations or refuges not previously notified: NONE b) Stations closed or refuges abandoned and not previously notified: NONE SECTION 4 LOGISTICS ACTIVITIES AFFECTING OTHER NATIONS a) McMurdo airstrip will be used by Italian and New Zealand C-130s and Italian Twin Otters b) McMurdo Heliport will be used by New Zealand and Italian helicopters c) Extensive air, sea and land logistic cooperative support with New Zealand d) Twin Otters to pass through Rothera (UK) upon arrival and departure from Antarctica e) Italian Twin Otter will likely pass through South Pole and McMurdo. -
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. -
Preserving the World Second Largest Hypersaline Lake Under Future Irrigation and Climate Change
Preserving the World Second Largest Hypersaline Lake under Future Irrigation and Climate Change Somayeh Shadkam1, Fulco Ludwig1, Michelle T.H. van Vliet1,2, Amandine Pastor1,2, Pavel Kabat1,2 [1] Earth System Science, Wageningen University, PO Box 47, 6700 AA Wageningen, The Netherlands [2] International Institute for Applied Systems Analysis (IIASA), Schlossplatz 1, A‐2361 Laxenburg, Austria E-mail: [email protected] Abstract. Urmia Lake, the world second largest hypersaline lake, has been largely desiccated over the last two decades resulting in socio-environmental consequences similar or even larger than the Aral Sea disaster. To rescue the lake a new water management plan has been proposed, a rapid 40% decline in irrigation water use replacing a former plan which intended to develop reservoirs and irrigation. However, none of these water management plans, which have large socio-economic impacts, have been assessed under future changes in climate and water availability. By adapting a method of environmental flow requirements (EFRs) for hypersaline lakes, we estimated annually 3.7∙109 m3 water is needed to preserve Urmia Lake. Then, the Variable Infiltration Capacity (VIC) hydrological model was forced with bias-corrected climate model outputs for both the lowest (RCP2.6) and highest (RCP8.5) greenhouse-gas concentration scenarios to estimate future water availability and impacts of water management strategies. Results showed a 10% decline in future water availability in the basin under RCP2.6 and 27% under RCP8.5. Our results showed that if future climate change is highly limited (RCP2.6) inflow can be just enough to meet the EFRs by implementing the reduction irrigation plan.