Extreme Arthropods Exploring Evolutionary Adaptations to Polar and Temperate Deserts
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One of Five West Coast, Low-Latitude Deserts of the World, the Namib Extends Along the Entire Namibian Coastline in an 80-120 Km Wide Belt
N A M I B I A G 3 E 0 O 9 1 L - O Y G E I V C R A U S L NAMIB DESERT Source: Roadside Geology of Namibia One of five west coast, low-latitude deserts of the world, the Namib extends along the entire Namibian coastline in an 80-120 km wide belt. Its extreme aridity is the result of the cold, upwelling Benguela Current, which flows up the west coast of Africa as far as Angola, and because of its low temperatures induces very little evaporation and rainfall (<50 mm per year). It does, however, create an up to 50 km wide coastal fog belt providing sufficient moisture for the development of a specialist flora and fauna, many of which are endemic to the Namib. In addition, the lagoons at Walvis Bay and Sandwich Harbour are designated wetlands of international importance, because of their unique setting and rich birdlife, including flamingo, white pelican and Damara tern. Larger mammals like the famed desert elephant, black rhino, lion, cheetah and giraffe can be found along the northern rivers traversing the Skeleton Coast National Park. Geomorphologically, the Namib includes a variety of landscapes, including classic sand dunes, extensive gravel plains, locally with gypcrete and calcrete duricrusts, elongated salt pans, ephemeral watercourses forming linear oases, inselbergs and low mountain ranges. Along the coast, wind-swept sandy beaches alternate with rocky stretches, in places carved into striking rock formations (e.g. Bogenfels Arch). Designated a UNESCO World Heritage Site in 2013, the “Namib Sand Sea“ between Lüderitz and the Kuiseb River encompasses such well-known landmarks as Sossusvlei and Sandwich Harbour, while the fabled Skeleton Coast north of the Ugab River is notorious for its numerous ship wrecks. -
Eretmoptera Murphyi Schaeffer (Diptera: Chironomjdae), an Apparently Parthenogenetic Antarctic Midge
ERETMOPTERA MURPHYI SCHAEFFER (DIPTERA: CHIRONOMJDAE), AN APPARENTLY PARTHENOGENETIC ANTARCTIC MIDGE P. S. CRANSTON Entomology Department, British Museum (Natural History), Cromwell Road, London SWl SBD ABSTRACT. Chironomid midges are amongst the most abundant and diverse holo metabolous insects of the Antarctic and sub-Antarctic. Eretmoptera murphyi Schaeffer, 1914, has been enigmatic to systematists since the first discovery of adult females on South Georgia. The rediscovery of the species as a suspected introduction to Signy Island (South Orkney Islands) allows the description of the immature stages for the first time and the redescription of the female, the only sex known. E. murphyi larvae are terrestrial, living in damp moss and peat, and the brachypterous adult is probably parthenogenetic. Eretmoptera appears to have an isolated position amongst the terrestrial Orthocladiinae: the close relationship with the marine Clunio group of genera suggested by previous workers is not supported. INTRODUCTION In the Antarctic and sub-Antarctic regions, the Chironomidae (non-biting midges) are the commonest, most diverse and most widely distributed group ofhoi ometa bolo us insects. For example, Belgica antarctica Jacobs is the most southerly distributed free-living insect (Wirth and Gressitt, 1967; Usher and Edwards, 1984) and the podonomine genus Parochlus is found throughout the sub-Antarctic islands. Recently, Sublette and Wirth (1980) reported 22 species in 18 genera belonging to 6 subfamilies of Chironomidae from New Zealand's sub-Antarctic islands. One sub-Antarctic midge that has remained rather enigmatic since its discovery is Eretmoptera murphyi. Two females of this brachypterous chironomid were collected by R. C. Murphy from South Georgia in 1913 and described, together with other insects, by Schaeffer (1914). -
Sand Dunes Computer Animations and Paper Models by Tau Rho Alpha*, John P
Go Home U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY Sand Dunes Computer animations and paper models By Tau Rho Alpha*, John P. Galloway*, and Scott W. Starratt* Open-file Report 98-131-A - This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this program has been used by the U.S. Geological Survey, no warranty, expressed or implied, is made by the USGS as to the accuracy and functioning of the program and related program material, nor shall the fact of distribution constitute any such warranty, and no responsibility is assumed by the USGS in connection therewith. * U.S. Geological Survey Menlo Park, CA 94025 Comments encouraged tralpha @ omega? .wr.usgs .gov [email protected] [email protected] (gobackward) <j (goforward) Description of Report This report illustrates, through computer animations and paper models, why sand dunes can develop different forms. By studying the animations and the paper models, students will better understand the evolution of sand dunes, Included in the paper and diskette versions of this report are templates for making a paper models, instructions for there assembly, and a discussion of development of different forms of sand dunes. In addition, the diskette version includes animations of how different sand dunes develop. Many people provided help and encouragement in the development of this HyperCard stack, particularly David M. Rubin, Maura Hogan and Sue Priest. -
Developing a Framework of Dune Accumulation in the Northern Rub Al
Developing a framework of Quaternary dune accumulation in the northern Rub’ al-Khali, Arabia. Andrew R Farranta, Geoff A T Dullerb, Adrian G Parkerc, Helen M Robertsb, Ash Partond, Robert W O Knoxa#, and Thomas Bidea. aBritish Geological Survey, Keyworth, Nottingham, NG12 5GG, UK. [email protected] [corresponding author 0115 9363184]. bAberystwyth Luminescence Research Laboratory, Department of Geography & Earth Sciences, Aberystwyth University, Aberystwyth, SY23 3DB, Wales, UK cDepartment of Social Sciences, Faculty of Humanities and Social Sciences, Oxford Brookes University, Oxford, OX3 0BP, UK dResearch Laboratory for Archaeology and the History of Art, School of Archaeology, University of Oxford, Oxford, OX1 2HU, UK #Deceased Abstract Located at the crossroads between Africa and Eurasia, Arabia occupies a pivotal position for human migration and dispersal during the Late Pleistocene. Deducing the timing of humid and arid phases is critical to understanding when the Rub’ al-Khali desert acted as a barrier to human movement and settlement. Recent geological mapping in the northern part of the Rub’ al-Khali has enabled the Quaternary history of the region to be put into a regional stratigraphical framework. In addition to the active dunes, two significant palaeodune sequences have been identified. Dating of key sections has enabled a chronology of dune accretion and stabilisation to be determined. In addition, previously published optically stimulated luminescence (OSL) dates have been put in their proper stratigraphical context, from which a record of Late Pleistocene dune activity can be constructed. The results indicate the record of dune activity in the northern Rub’ al-Khali is preservation limited and is synchronous with humid events driven by the incursion of the Indian Ocean monsoon. -
Passive Water Collection with the Integument: Mechanisms and Their Biomimetic Potential (Doi:10.1242/ Jeb.153130) Philipp Comanns
© 2018. Published by The Company of Biologists Ltd | Journal of Experimental Biology (2018) 221, jeb185694. doi:10.1242/jeb.185694 CORRECTION Correction: Passive water collection with the integument: mechanisms and their biomimetic potential (doi:10.1242/ jeb.153130) Philipp Comanns There was an error published in J. Exp. Biol. (2018) 221, jeb153130 (doi:10.1242/jeb.153130). The corresponding author’s email address was incorrect. It should be [email protected]. This has been corrected in the online full-text and PDF versions. We apologise to authors and readers for any inconvenience this may have caused. Journal of Experimental Biology 1 © 2018. Published by The Company of Biologists Ltd | Journal of Experimental Biology (2018) 221, jeb153130. doi:10.1242/jeb.153130 REVIEW Passive water collection with the integument: mechanisms and their biomimetic potential Philipp Comanns* ABSTRACT 2002). Furthermore, there are also infrequent rain falls that must be Several mechanisms of water acquisition have evolved in animals considered (Comanns et al., 2016a). living in arid habitats to cope with limited water supply. They enable Maintaining a water balance in xeric habitats (see Glossary) often access to water sources such as rain, dew, thermally facilitated requires significant reduction of cutaneous water loss. Reptiles condensation on the skin, fog, or moisture from a damp substrate. commonly have an almost water-proof skin owing to integumental This Review describes how a significant number of animals – in lipids, amongst other components (Hadley, 1989). In some snakes, excess of 39 species from 24 genera – have acquired the ability to for example, the chemical removal of lipids has been shown to – passively collect water with their integument. -
Physical Ecology of Hypolithic Communities in the Central Namib Desert: the Role of Fog, Rain, Rock Habitat, and Light Kimberley A
JOURNAL OF GEOPHYSICAL RESEARCH: BIOGEOSCIENCES, VOL. 118, 1451–1460, doi:10.1002/jgrg.20117, 2013 Physical ecology of hypolithic communities in the central Namib Desert: The role of fog, rain, rock habitat, and light Kimberley A. Warren-Rhodes,1,2 Christopher P. McKay,1 Linda Ng Boyle,3 Michael R. Wing,4 Elsita M. Kiekebusch,5 Don A. Cowan,6,7 Francesca Stomeo,7,8 Stephen B. Pointing,9 Kudzai F. Kaseke,10 Frank Eckardt,11 Joh R. Henschel,12 Ari Anisfeld,5 Mary Seely,5 and Kevin L. Rhodes 13 Received 10 May 2013; revised 7 September 2013; accepted 15 September 2013; published 24 October 2013. [1] Hypolithic microbial communities are productive niches in deserts worldwide, but many facets of their basic ecology remain unknown. The Namib Desert is an important site for hypolith study because it has abundant quartz rocks suitable for colonization and extends west to east across a transition from fog- to rain-dominated moisture sources. We show that fog sustains and impacts hypolithic ecology in several ways, as follows: (1) fog effectively replaces rainfall in the western zone of the central Namib to enable high (≥95%) hypolithic abundance at landscape (1–10 km) and larger scales; and (2) high water availability, through fog (western zone) and/or rainfall (eastern zone), results in smaller size-class rocks being colonized (mean 6.3 ± 1.2 cm) at higher proportions (e.g., 98% versus approximately 3%) than in previously studied hyperarid deserts. We measured 0.1% of incident sunlight as the lower limit for hypolithic growth on quartz rocks in the Namib and found that uncolonized ventral rock surfaces were limited by light rather than moisture. -
Cypris 2016-2017
CYPRIS 2016-2017 Illustrations courtesy of David Siveter For the upper image of the Silurian pentastomid crustacean Invavita piratica on the ostracod Nymphateline gravida Siveter et al., 2007. Siveter, David J., D.E.G. Briggs, Derek J. Siveter, and M.D. Sutton. 2015. A 425-million-year- old Silurian pentastomid parasitic on ostracods. Current Biology 23: 1-6. For the lower image of the Silurian ostracod Pauline avibella Siveter et al., 2012. Siveter, David J., D.E.G. Briggs, Derek J. Siveter, M.D. Sutton, and S.C. Joomun. 2013. A Silurian myodocope with preserved soft-parts: cautioning the interpretation of the shell-based ostracod record. Proceedings of the Royal Society London B, 280 20122664. DOI:10.1098/rspb.2012.2664 (published online 12 December 2012). Watermark courtesy of Carin Shinn. Table of Contents List of Correspondents Research Activities Algeria Argentina Australia Austria Belgium Brazil China Czech Republic Estonia France Germany Iceland Israel Italy Japan Luxembourg New Zealand Romania Russia Serbia Singapore Slovakia Slovenia Spain Switzerland Thailand Tunisia United Kingdom United States Meetings Requests Special Publications Research Notes Photographs and Drawings Techniques and Methods Awards New Taxa Funding Opportunities Obituaries Horst Blumenstengel Richard Forester Franz Goerlich Roger Kaesler Eugen Kempf Louis Kornicker Henri Oertli Iraja Damiani Pinto Evgenii Schornikov Michael Schudack Ian Slipper Robin Whatley Papers and Abstracts (2015-2007) 2016 2017 In press Addresses Figure courtesy of Francesco Versino, -
Long-Term Population Dynamics of Namib Desert Tenebrionid Beetles Reveal Complex Relationships to Pulse-Reserve Conditions
insects Article Long-Term Population Dynamics of Namib Desert Tenebrionid Beetles Reveal Complex Relationships to Pulse-Reserve Conditions Joh R. Henschel 1,2,3 1 South African Environmental Observation Network, P.O. Box 110040 Hadison Park, Kimberley 8301, South Africa; [email protected] 2 Centre for Environmental Management, University of the Free State, P.O. Box 339, Bloemfontein 9300, South Africa 3 Gobabeb Namib Research Institute, P.O. Box 953, Walvis Bay 13103, Namibia Simple Summary: Rain seldom falls in the extremely arid Namib Desert in Namibia, but when a certain amount falls, it causes seeds to germinate, grass to grow and seed, dry, and turn to litter that gradually decomposes over the years. It is thought that such periodic flushes and gradual decay are fundamental to the functioning of the animal populations of deserts. This notion was tested with litter-consuming darkling beetles, of which many species occur in the Namib. Beetles were trapped in buckets buried at ground level, identified, counted, and released. The numbers of most species changed with the quantity of litter, but some mainly fed on green grass and disappeared when this dried, while other species depended on the availability of moisture during winter. Several species required unusually heavy rainfalls to gradually increase their populations, while others the opposite, declining when wet, thriving when dry. All 26 beetle species experienced periods when their numbers were extremely low, but all Citation: Henschel, J.R. Long-Term had the capacity for a few remaining individuals to repopulate the area in good times. The remarkably Population Dynamics of Namib different relationships of these beetles to common resources, litter, and moisture, explain how so many Desert Tenebrionid Beetles Reveal species can exist side by side in such a dry environment. -
Genomic Platforms and Molecular Physiology of Insect Stress Tolerance
Genomic Platforms and Molecular Physiology of Insect Stress Tolerance DISSERTATION Presented in Partial Fulfillment of the Requirements for the Degree Doctor of Philosophy in the Graduate School of The Ohio State University By Justin Peyton MS Graduate Program in Evolution, Ecology and Organismal Biology The Ohio State University 2015 Dissertation Committee: Professor David L. Denlinger Advisor Professor Zakee L. Sabree Professor Amanda A. Simcox Professor Joseph B. Williams Copyright by Justin Tyler Peyton 2015 Abstract As ectotherms with high surface area to volume ratio, insects are particularly susceptible to desiccation and low temperature stress. In this dissertation, I examine the molecular underpinnings of two facets of these stresses: rapid cold hardening and cryoprotective dehydration. Rapid cold hardening (RCH) is an insect’s ability to prepare for cold stress when that stress is preceded by an intermediate temperature for minutes to hours. In order to gain a better understanding of cold shock, recovery from cold shock, and RCH in Sarcophaga bullata I examine the transcriptome with microarray and the metabolome with gas chromatography coupled with mass spectrometry (GCMS) in response to these treatments. I found that RCH has very little effect on the transcriptome, but results in a shift from aerobic metabolism to glycolysis/gluconeogenesis during RCH and preserved metabolic homeostasis during recovery. In cryoprotective dehydration (CD), a moisture gradient is established between external ice and the moisture in the body of an insect. As temperatures decline, the external ice crystals grow, drawing in more moisture which dehydrates the insect causing its melting point to track the ambient temperature. To gain a better understanding of CD and dehydration in Belgica antarctica I explore the transcriptome with RNA sequencing ii and the metabolome with GCMS. -
Uti Possidetis Juris, and the Borders of Israel
PALESTINE, UTI POSSIDETIS JURIS, AND THE BORDERS OF ISRAEL Abraham Bell* & Eugene Kontorovich** Israel’s borders and territorial scope are a source of seemingly endless debate. Remarkably, despite the intensity of the debates, little attention has been paid to the relevance of the doctrine of uti possidetis juris to resolving legal aspects of the border dispute. Uti possidetis juris is widely acknowledged as the doctrine of customary international law that is central to determining territorial sovereignty in the era of decolonization. The doctrine provides that emerging states presumptively inherit their pre-independence administrative boundaries. Applied to the case of Israel, uti possidetis juris would dictate that Israel inherit the boundaries of the Mandate of Palestine as they existed in May, 1948. The doctrine would thus support Israeli claims to any or all of the currently hotly disputed areas of Jerusalem (including East Jerusalem), the West Bank, and even potentially the Gaza Strip (though not the Golan Heights). TABLE OF CONTENTS INTRODUCTION ..................................................................................................... 634 I. THE DOCTRINE OF UTI POSSIDETIS JURIS ........................................................... 640 A. Development of the Doctrine ..................................................................... 640 B. Applying the Doctrine ................................................................................ 644 II. UTI POSSIDETIS JURIS AND MANDATORY BORDERS ........................................ -
Biolphilately Vol-64 No-3
Vol. 67 (1) Biophilately March 2018 5 FOG-COLLECTING BEETLES OF THE NAMIB DESERT Donald Wright, BU243 There exists in the Namib Desert of southwest Africa a group of beetles that collects moisture from the fog-laden air blowing in from the Atlantic coast. These all belong to the Family Tenebrionidae, Subfamily Pimeliinae. Those found on stamps to date include the following: Saucer Trench Beetle, Lepidochora discoidalis Gebien (Lepidochara of some) Namibia, Sc#1249c, 22 September 2012, $5.80 Onymacris paiva Haag Comoro Islands, unlisted, 28 July 2011, 2500fr SS (LR margin) (Stamperija) Fog-basking or Fog-drinking Beetle, Onymacris unguicularis Haag Comoro Islands, Sc#1078, 2 March 2009, 3000fr SS (L margin) Mozambique, Sc#1919, 30 November 2009, 175m SS (MR margin) Namibia, Sc#967a, 22 May 2000, $2 Namibia, Sc#1109, 15 February 2007, “Standard Mail” ($1.90) (with Web-footed Gecko) (perf 14×13¼) Namibia, Sc#1109a, 2008, “Standard Mail” ($1.90) (same, perf 14) Namibia, Sc#1168, 1 October 2008, “Registered Mail” ($18.20) (with False Ink Cap mushroom) Namibia, Sc#1186f, 8 February 2010, “Postcard Rate” ($4.60) Namibia, unlisted, 2010, “Standard Mail” ($2.50) (design similar to Sc#1186f) Long-legged White Namib Beetle, Stenocara eburnea Pascoe Niger, Sc#1054a, 27 July 2000, 200fr Namib Desert Beetle, Stenocara gracilipes Solier Kenya, Sc#854y, 16 November 2011, 65sh These are flightless beetles, many with fused wing covers (elytra). They are diurnal, burying themselves in their sandy habitat at night, and emerging during the day. There are 21 species of Onymacris, four of Stenocara, three of Lepidochora, and four of Physasterna. -
Analysis of the Namib and Kalahari Dune Sand Deposits in Namibia and Their Application in Potassium Silicate Synthesis a Thesis
ANALYSIS OF THE NAMIB AND KALAHARI DUNE SAND DEPOSITS IN NAMIBIA AND THEIR APPLICATION IN POTASSIUM SILICATE SYNTHESIS A THESIS SUBMITTED IN FULFILMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF SCIENCE IN CHEMISTRY OF THE UNIVERSITY OF NAMIBIA BY WILHELM PENDUKENI NUUMBEMBE 200824651 AUGUST 2016 Main Supervisor: Prof Fred Kamona Co-supervisors: Dr Veikko Uahengo & Dr Heike Wanke ABSTRACT Silica sand is a main component in the synthesis of potassium silicates that are commonly used as binding, coating, and adhesives agents. Physical and chemical properties of the sand particles such as grain size, mineralogical and geochemical compositions, determine the viability of sand in the synthesis of potassium silicates. This study analysed sand samples from dunes in the Namib and Kalahari deserts in order to 1) evaluate their suitability in potassium silicate synthesis as well as to 2) synthesize potassium silicate and characterize microstructural and chemical properties of the potassium silicate. Sand grains were analysed and characterized using the following techniques: mechanical sieves, ICP-EOS/MS spectrometry, and X-ray diffractometry. Synthesized potassium silicate was characterized using techniques of XRD, ICP-OES, and SEM-EDX. The dunes sand grain sizes range from 45 – 2000 µm, with 98 % of the Namib dune sand are distributed in the grain size range 63 – 500 µm and only 60% of the Kalahari dune sand are distributed in the similar grain size range, while the other 20 % is confined in the 45 -63 µm grain size range and the other 20 % confined in the grain size 500 - 2000 µm. Quartz is the dominant mineral in all sand samples and feldspar minerals were observed only in the Namib dune sand samples.