Entomological Investigations in Antarctica
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Hucke-Gaete, R, Torres, D. & Vallejos, V. 1997c. Entanglement of Antarctic fur seals, Arctocephalus gazella, by marine debris at Cape Shirreff and San Telmo Islets, Livingston Island, Antarctica: 1998-1997. Serie Científica Instituto Antártico Chileno 47: 123-135. Hucke-Gaete, R., Osman, L.P., Moreno, C.A. & Torres, D. 2004. Examining natural population growth from near extinction: the case of the Antarctic fur seal at the South Shetlands, Antarctica. Polar Biology 27 (5): 304–311 Huckstadt, L., Costa, D. P., McDonald, B. I., Tremblay, Y., Crocker, D. E., Goebel, M. E. & Fedak, M. E. 2006. Habitat Selection and Foraging Behavior of Southern Elephant Seals in the Western Antarctic Peninsula. American Geophysical Union, Fall Meeting 2006, abstract #OS33A-1684. INACH (Instituto Antártico Chileno) 2010. Chilean Antarctic Program of Scientific Research 2009-2010. Chilean Antarctic Institute Research Projects Department. Santiago, Chile. Kawaguchi, S., Nicol, S., Taki, K. & Naganobu, M. 2006. Fishing ground selection in the Antarctic krill fishery: Trends in patterns across years, seasons and nations. CCAMLR Science, 13: 117–141. Krause, D. J., Goebel, M. E., Marshall, G. J., & Abernathy, K. (2015). Novel foraging strategies observed in a growing leopard seal (Hydrurga leptonyx) population at Livingston Island, Antarctic Peninsula. Animal Biotelemetry, 3:24. Krause, D.J., Goebel, M.E., Marshall. G.J. & Abernathy, K. In Press. Summer diving and haul-out behavior of leopard seals (Hydrurga leptonyx) near mesopredator breeding colonies at Livingston Island, Antarctic Peninsula. Marine Mammal Science.Leppe, M., Fernandoy, F., Palma-Heldt, S. & Moisan, P 2004. Flora mesozoica en los depósitos morrénicos de cabo Shirreff, isla Livingston, Shetland del Sur, Península Antártica, in Actas del 10º Congreso Geológico Chileno. -
Desiccation Tolerance and Drought Acclimation in the Antarctic Collembolan Cryptopygus Antarcticus
Journal of Insect Physiology 54 (2008) 1432–1439 Contents lists available at ScienceDirect Journal of Insect Physiology journal homepage: www.elsevier.com/locate/jinsphys Desiccation tolerance and drought acclimation in the Antarctic collembolan Cryptopygus antarcticus Michael A. Elnitsky a,b,*, Joshua B. Benoit c, David L. Denlinger c, Richard E. Lee Jr.a a Department of Zoology, Miami University, Oxford, OH 45056, United States b Department of Biology, Mercyhurst College, Erie, PA 16546, United States c Department of Entomology, The Ohio State University, Columbus, OH 43210, United States ARTICLE INFO ABSTRACT Article history: The availability of water is recognized as the most important determinant of the distribution and Received 9 June 2008 activity of terrestrial organisms within the maritime Antarctic. Within this environment, arthropods Received in revised form 30 July 2008 may be challenged by drought stress during both the austral summer, due to increased temperature, Accepted 4 August 2008 wind, insolation, and extended periods of reduced precipitation, and the winter, as a result of vapor pressure gradients between the surrounding icy environment and the body fluids. The purpose of the Keywords: present study was to assess the desiccation tolerance of the Antarctic springtail, Cryptopygus Desiccation antarcticus, under ecologically-relevant conditions characteristic of both summer and winter along the Drought acclimation Collembola Antarctic Peninsula. In addition, this study examined the physiological changes and effects of mild Cold-hardiness drought acclimation on the subsequent desiccation tolerance of C. antarcticus.Thecollembolans À1 Cryoprotective dehydration possessed little resistance to water loss under dry air, as the rate of water loss was >20% h at 0% relative humidity (RH) and 4 8C. -
Management Plan for Antarctic Specially Protected Area No. 116 NEW COLLEGE VALLEY, CAUGHLEY BEACH, CAPE BIRD, ROSS ISLAND
Management Plan For Antarctic Specially Protected Area No. 116 NEW COLLEGE VALLEY, CAUGHLEY BEACH, CAPE BIRD, ROSS ISLAND 1. Description of values to be protected In 1985, two areas at Cape Bird, Ross Island were designated as SSSI No. 10, Caughley Beach (Recommendation XIII-8 (1985)) and SPA No. 20, New College Valley (Recommendation XIII-12 (1985)), following proposals by New Zealand that these areas should be protected because they contained some of the richest stands of moss and associated microflora and fauna in the Ross Sea region of Antarctica. This is the only area on Ross Island where protection is specifically given to plant assemblages and associated ecosystems. At that time, SPA No. 20 was enclosed within SSSI No. 10, in order to provide more stringent access conditions to that part of the Area. In 2000, SSSI No. 10 was incorporated with SPA No. 20 by Measure 1 (2000), with the former area covered by SPA No. 20 becoming a Restricted Zone within the revised SPA No. 20. The boundaries of the Area were revised from the boundaries in the original recommendations, in view of improved mapping and to follow more closely the ridges enclosing the catchment of New College Valley. Caughley Beach itself was adjacent to, but never a part of, the original Area, and for this reason the entire Area was renamed as New College Valley, which was within both of the original sites. The Area was redesignated by Decision 1 (2002) as Antarctic Specially Protected Area (ASPA) No. 116 and a revised Management Plan was adopted through Measure 1 (2006). -
The Antarctic Crustal Profile Seismic Project, Ross Sea, Antarctica ALAN K
200,000 years are obviously affected to a lesser degree than argon (40Ar) to excess argon (40ArE) and are, therefore, taken younger samples containing a lower proportion of radiogenic to be a truer representation of the actual age of that particu- _______________________ lar sample. Still, it must be noted that all the 40Ar/ 39Ar ages pro- 40Ar139Ar ages for Mount Erebus as determined in this study duced from Mount Erebus are maximum ages owing to the uncertainty of complete removal (through sample preparation) of all excess argon. 48±9a Excess argon—Too Old Summit phenocrysts Evaluation of these new data Summit phenocrysts -10 179±16a Excess argon—Too Old Summit phenocrysts #2 49±27a Excess argon—Too Old is still in progress; however, it is Summit phenocrysts #2 30-40 641±27a Excess argon—Too Old apparent that our new age deter- Summit (bomb) glass 100 101±16a Excess argon—Too Old minations are significantly Lower Hut flow <1 24±4b Acceptable younger than those previously Three Sisters cones -4 26±2b Acceptable obtained by the conventional Three Sisters cones 11 1±8b Contamination? K/Ar method. The evolution and 36±4 Hoopers Shoulder <1 b Acceptable growth of Mount Erebus may Hoopers Shoulder cone 32±5b Acceptable have been much faster than pre- a Hoopers Shoulder cone -5 94±15 Excess argon viously thought. 42±4b Contamination? Cape Evans This research was supported Cape Evans -5 32±6b Acceptable Cape Royds -2 735b Acceptable by National Science Foundation Cape Royds -20 153±32a Excess argon grant OPP 91-18056. -
The Antarctic Mite, Alaskozetes Antarcticus, Shares Bacterial Microbiome Community Membership but Not Abundance Between Adults and Tritonymphs
Polar Biology (2019) 42:2075–2085 https://doi.org/10.1007/s00300-019-02582-5 ORIGINAL PAPER The Antarctic mite, Alaskozetes antarcticus, shares bacterial microbiome community membership but not abundance between adults and tritonymphs Christopher J. Holmes1 · Emily C. Jennings1 · J. D. Gantz2,3 · Drew Spacht4 · Austin A. Spangler1 · David L. Denlinger4 · Richard E. Lee Jr.3 · Trinity L. Hamilton5 · Joshua B. Benoit1 Received: 14 January 2019 / Revised: 3 September 2019 / Accepted: 4 September 2019 / Published online: 16 September 2019 © Springer-Verlag GmbH Germany, part of Springer Nature 2019 Abstract The Antarctic mite (Alaskozetes antarcticus) is widely distributed on sub-Antarctic islands and throughout the Antarctic Peninsula, making it one of the most abundant terrestrial arthropods in the region. Despite the impressive ability of A. ant- arcticus to thrive in harsh Antarctic conditions, little is known about the biology of this species. In this study, we performed 16S rRNA gene sequencing to examine the microbiome of the fnal immature instar (tritonymph) and both male and female adults. The microbiome included a limited number of microbial classes and genera, with few diferences in community membership noted among the diferent stages. However, the abundances of taxa that composed the microbial community difered between adults and tritonymphs. Five classes—Actinobacteria, Flavobacteriia, Sphingobacteriia, Gammaproteobac- teria, and Betaproteobacteria—comprised ~ 82.0% of the microbial composition, and fve (identifed) genera—Dermacoccus, Pedobacter, Chryseobacterium, Pseudomonas, and Flavobacterium—accounted for ~ 68.0% of the total composition. The core microbiome present in all surveyed A. antarcticus was dominated by the families Flavobacteriaceae, Comamonadaceae, Sphingobacteriaceae, Chitinophagaceae and Cytophagaceae, but the majority of the core consisted of operational taxonomic units of low abundance. -
The Collembola of Antarctica1
Pacific Insects Monograph 25: 57-74 20 March 1971 THE COLLEMBOLA OF ANTARCTICA1 By K. A. J. Wise2 Abstract: Subsequent to an earlier paper on Antarctic Collembola, further references and specimen locality records are given, and a new classification is used. Named species and definite distributions are combined in a definitive list of the Collembola of Antarctica. One new synonymy. Hypogastrura viatica (=H. antarctica), is recorded. Collections additional to those reported by Wise (1967) are recorded here, together with further information on some of the species, including one new synonymy. References in the synonymic lists are only those additional to the ones published in my previous paper. As in that paper, S. Orkney Is. and S. Sandwich Is. records are included here, but are excluded from the list of species in Antarctica. In addition to the Bishop Museum collections, specimens from collections of other institutions are recorded as follows: U.S. National Museum, Smithsonian Institution (USNM), British Museum (Nat. Hist.) (BMNH), British Antarctic Survey Biological Unit (BAS), and Canterbury University Antarctic Biology Unit (CUABU). The arrangement of figures and legends are as in Wise (1967). In specimen data a figure at the beginning of a group is the number of micro-slide specimens; a figure at the end, after the col lector's name, is the collector's site number. Classification Classification of the Antarctic species previously (Wise 1967) followed that of Salmon (1964) which radically changed some of the earlier classifications, separating some of the Suborder Arthropleona as distinct families in a new suborder, Neoarthropleona. Since then, Massoud (1967) has published a sound revision of the Neanuridae, in which he has sunk the Suborder Neoarthro pleona establishing the families recorded therein by Salmon as subfamilies or tribes in the Family Neanuridae. -
Responses of Invertebrates to Temperature and Water Stress A
Author's Accepted Manuscript Responses of invertebrates to temperature and water stress: A polar perspective M.J. Everatt, P. Convey, J.S. Bale, M.R. Worland, S.A.L. Hayward www.elsevier.com/locate/jtherbio PII: S0306-4565(14)00071-0 DOI: http://dx.doi.org/10.1016/j.jtherbio.2014.05.004 Reference: TB1522 To appear in: Journal of Thermal Biology Received date: 21 August 2013 Revised date: 22 January 2014 Accepted date: 22 January 2014 Cite this article as: M.J. Everatt, P. Convey, J.S. Bale, M.R. Worland, S.A.L. Hayward, Responses of invertebrates to temperature and water stress: A polar perspective, Journal of Thermal Biology, http://dx.doi.org/10.1016/j.jther- bio.2014.05.004 This is a PDF file of an unedited manuscript that has been accepted for publication. As a service to our customers we are providing this early version of the manuscript. The manuscript will undergo copyediting, typesetting, and review of the resulting galley proof before it is published in its final citable form. Please note that during the production process errors may be discovered which could affect the content, and all legal disclaimers that apply to the journal pertain. 1 Responses of invertebrates to temperature and water 2 stress: A polar perspective 3 M. J. Everatta, P. Conveyb, c, d, J. S. Balea, M. R. Worlandb and S. A. L. 4 Haywarda* a 5 School of Biosciences, University of Birmingham, Edgbaston, Birmingham B15 2TT, UK b 6 British Antarctic Survey, Natural Environment Research Council, High Cross, Madingley Road, 7 Cambridge, CB3 0ET, UK 8 cNational Antarctic Research Center, IPS Building, University Malaya, 50603 Kuala Lumpur, 9 Malaysia 10 dGateway Antarctica, University of Canterbury, Private Bag 4800, Christchurch 8140, New Zealand 11 12 *Corresponding author. -
Bacterial Diversity Is Strongly Associated with Historical Penguin Activity in an Antarctic Lake Sediment Profile
www.nature.com/scientificreports OPEN Bacterial diversity is strongly associated with historical penguin activity in an Antarctic lake Received: 27 July 2015 Accepted: 27 October 2015 sediment profile Published: 25 November 2015 Renbin Zhu1, Yu Shi2, Dawei Ma1, Can Wang1, Hua Xu2 & Haiyan Chu2 Current penguin activity in Antarctica affects the geochemistry of sediments and their microbial communities; the effects of historical penguin activity are less well understood. Here, bacterial diversity in ornithogenic sediment was investigated using high-throughput pyrosequencing. The relative abundances of dominant phyla were controlled by the amount of historical penguin guano deposition. Significant positive correlations were found between both the bacterial richness and diversity, and the relative penguin number (p < 0.01); this indicated that historical penguin activity drove the vertical distribution of the bacterial communities. The lowest relative abundances of individual phyla corresponded to lowest number of penguin population at 1,800–2,300 yr BP during a drier and colder period; the opposite was observed during a moister and warmer climate (1,400–1,800 yr BP). This study shows that changes in the climate over millennia affected penguin populations and the outcomes of these changes affect the sediment bacterial community today. Antarctic freshwater lakes are relatively simple aquatic ecosystems, with low species richness and diversity, low biomass, short food chains and limited trophic complexity1,2. However, benthic sediments represent one of the most complex microbial habitats on Earth3. Microorganisms in sediments play a significant role in biogeochemical cycles and the remineralisation of organic matter within aquatic ecosystems. For example, bacterial populations are major contributors in the transformation of organic carbon, sulphur, nitrogenous compounds, and metals, and have an important role in ecosystem food webs and nutrient cycling2,4. -
Groundwater Characteristics at Seabee Hook, Cape Hallett, Antarctica ERICA H
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Research Commons@Waikato Antarctic Science 18 (4), 487–495 (2006) © Antarctic Science Ltd Printed in the UK DOI: 10.1017/S0954102006000538 Groundwater characteristics at Seabee Hook, Cape Hallett, Antarctica ERICA H. HOFSTEE1, DAVE I. CAMPBELL1*, MEGAN R. BALKS1 and JACKIE AISLABIE2 1Department of Earth and Ocean Sciences, The University of Waikato, Private Bag 3105, Hamilton, New Zealand 2Landcare Research, Private Bag 3127, Hamilton, New Zealand *corresponding author: [email protected] Abstract: Seabee Hook is a low lying gravel spit adjacent to Cape Hallett, northern Victoria Land, in the Ross Sea region of Antarctica and hosts an Adélie penguin (Pygoscelis adeliae) rookery. Dipwells were inserted to monitor changes in depth to, and volume of, groundwater and tracer tests were conducted to estimate aquifer hydraulic conductivity and groundwater velocity. During summer (November–February), meltwater forms a shallow, unconfined, aquifer perched on impermeable ice cemented soil. Groundwater extent and volume depends on the amount of snowfall as meltwater is primarily sourced from melting snow drifts. Groundwater velocity through the permeable gravel and sand was up to 7.8 m day-1, and hydraulic conductivities of 4.7 × 10-4 m s-1 to 3.7 × 10-5 m s-1 were measured. The presence of the penguin rookery, and the proximity of the sea, affects groundwater chemistry with elevated concentrations of salts (1205 mg L-1 sodium, 332 mg L-1 potassium) and nutrients (193 mg L-1 nitrate, 833 mg L-1 ammonia, 10 mg L-1 total phosphorus) compared with groundwater sourced away from the rookery, and with other terrestrial waters in Antarctica. -
Scientific Information 2001/2002 Annual New Zealand
Scientific Information 2001/2002 Annual New Zealand Forward Plans LGP The Latitudinal Gradient Project (LGP) is aimed at increasing the understanding of the coastal marine, freshwater and terrestrial ecosystems that exist along the Victoria Land coastline in the Ross Sea region, and describing potential environmental variability that may occur in the future. Antarctica New Zealand is providing the logistical capabilities for research camps to be located at specific sites along the Victoria Land coast. Thus, the opportunity to work at particular locations in collaboration with other scientists from various disciplines and National Antarctic Programmes is provided. LGP has been formally incorporated into the SCAR programme RiSCC (Regional Sensitivity to Climate Change). Certain data collected within the LGP will be housed and made available within the RiSCC database framework. Details on how the data will be shared and the timing of when the data will be made available have yet to be decided. It is intended that publications arising from the LGP will be published in a special issue of a refereed journal. Research under the LGP will be both ship-based and land-based. At present, ship-based research, funded under the Ministry of Fisheries’ BioRoss programme and the Italian Antarctic Programme, has been scheduled for January to March 2004 with a research voyage planned using two vessels aimed at supporting near-shore and deep-water marine research. The vessels dedicated to this research are NIWA’s RV Tangaroa, and the Italian Antarctic Programme’s RV Italica. Further information about the ship-based research can be found in the BioRoss research plan and in the BioRoss call for statements of interest. -
Glacier Caves: a Globally Threatened Subterranean Biome
Francis G. Howarth. Glacier caves: a globally threatened subterranean biome. Journal of Cave and Karst Studies, v. 83, no. 2, p. 66-70. DOI:10.4311/2019LSC0132 GLACIER CAVES: A GLOBALLY THREATENED SUBTERRANEAN BIOME Francis G. Howarth1 Abstract Caves and cave-like voids are common features within and beneath glaciers. The physical environment is harsh and extreme, and often considered barren and devoid of life. However, accumulating evidence indicates that these caves may support a diverse invertebrate fauna with species endemic to each region. As glaciers continue to disappear at an alarming rate due to global warming, they take their largely unknown fauna with them. Thus, glacier caves may harbor one of the most endangered ecosystems globally, and yet their biodiversity is among the least studied or known. Faunal surveys and ecological studies are urgently needed before all examples are lost. INTRODUCTION Glacier caves are voids within and beneath glaciers that are formed mostly by surface meltwater sinking into the glacier through crevasses, moulins, and fissures (Piccini and Mecchia, 2013; Smart, 2003; Kováč, 2018; Gulley and Fountain, 2019). Glacier caves can be enlarged by geothermal melting (Kiver and Mumma, 1971; Giggenbach, 1976), as well as by pressure and friction at the contact between the ice and bedrock. These caves are created by natural phenomena during the life of the glacier and are common features in glaciers. They are best developed in montane gla- ciers in comparison to polar glaciers, largely because of the steeper gradient, greater flow rate, and seasonally warmer temperatures (Smart, 2003). The cave structure is dynamic; for example, changing shape and course as the glacier flows downslope; enlarging during warm periods; and collapsing and deforming under pressure. -
1 Compiled by Mike Wing New Zealand Antarctic Society (Inc
ANTARCTIC 1 Compiled by Mike Wing US bulldozer, 1: 202, 340, 12: 54, New Zealand Antarctic Society (Inc) ACECRC, see Antarctic Climate & Ecosystems Cooperation Research Centre Volume 1-26: June 2009 Acevedo, Capitan. A.O. 4: 36, Ackerman, Piers, 21: 16, Vessel names are shown viz: “Aconcagua” Ackroyd, Lieut. F: 1: 307, All book reviews are shown under ‘Book Reviews’ Ackroyd-Kelly, J. W., 10: 279, All Universities are shown under ‘Universities’ “Aconcagua”, 1: 261 Aircraft types appear under Aircraft. Acta Palaeontolegica Polonica, 25: 64, Obituaries & Tributes are shown under 'Obituaries', ACZP, see Antarctic Convergence Zone Project see also individual names. Adam, Dieter, 13: 6, 287, Adam, Dr James, 1: 227, 241, 280, Vol 20 page numbers 27-36 are shared by both Adams, Chris, 11: 198, 274, 12: 331, 396, double issues 1&2 and 3&4. Those in double issue Adams, Dieter, 12: 294, 3&4 are marked accordingly. Adams, Ian, 1: 71, 99, 167, 229, 263, 330, 2: 23, Adams, J.B., 26: 22, Adams, Lt. R.D., 2: 127, 159, 208, Adams, Sir Jameson Obituary, 3: 76, A Adams Cape, 1: 248, Adams Glacier, 2: 425, Adams Island, 4: 201, 302, “101 In Sung”, f/v, 21: 36, Adamson, R.G. 3: 474-45, 4: 6, 62, 116, 166, 224, ‘A’ Hut restorations, 12: 175, 220, 25: 16, 277, Aaron, Edwin, 11: 55, Adare, Cape - see Hallett Station Abbiss, Jane, 20: 8, Addison, Vicki, 24: 33, Aboa Station, (Finland) 12: 227, 13: 114, Adelaide Island (Base T), see Bases F.I.D.S. Abbott, Dr N.D.