Bathyergus Suillus – Cape Dune Mole-Rat
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Research Project Summmary Main Research
Research project summmary Main research fields: zoology and reproductive physiology specialization fields: Animal reproduction, Behavioural ecology, Behavioural physiology, sociobiology. My research interests focus mainly on the sociobiology of African rodent moles (Bathyergidae) and in particular the extrinsic and intrinsic factors that have led to the evolution of sociality in this remarkable endemic African family. My research group is fundamentally interested in elucidating the modes and mechanisms that are responsible for reproductive suppression in the non-reproductive females of the various species. Research is currently being directed at the neuroendocrine and molecular levels to elucidate the extent, nature and location of GnRH suppression. We are also interested in the photic and thermic input in the control of reproduction in seasonally reproducing mole-rats and the potential lack of a role in aseasonally breeding bathyergids. Long term population studies on social mole-rats from mesic and xeric environments are underway. These studies are providing empirical data on the spatial distribution of colonies, longevities, factors restricting and promoting dispersal, vagility, foraging methods and lifetime reproductive success. We are interested in the genetic relatedness of colonies and also the type of paternal skew operational in the social genera. This work is being carried out in collaboration with Dr Chris Faulkes at Queen Mary and Westfield College, London. Students currently under supervision MSc (research) 1. Ms. Kemba Butler Neuroendocrinology of induced ovulation in the highveld mole-rat (Cryptomys hottentotus pretoriae) 2. Mr. Andre Prins What makes a good helper? A behavioural study of cooperation in Damaraland mole-rats (Fukomys damarensis). 3. Mr. Josh Sarli Seasonal Reproductive Cycle and Parasite Burden of Two Small Mammals from Saudi Arabia. -
GEOG 101 PLACE NAME LIST for EXAM THREE
GEOG 101 PLACE NAME LIST for EXAM THREE Each exam will have a place name location map section based on the list below, plus countries and political units. Consult the appropriate maps in the atlas and textbook to locate these places. The atlas has a detailed INDEX. Exam III will focus on place names from Asia and Oceania. This section of the exam will be in the form of a matching question. You will match the names to numbers on a map. ________________________________________________________________________________ I. CONTINENTS Australia Asia ________________________________________________________________________________ II. OCEANS Pacific Indian Arctic ________________________________________________________________________________ III. ASIA Seas/Gulfs/Bays/Lakes: Caspian Sea Sea of Japan Arabian Sea South China Sea Red Sea Aral Sea Lake Baikal East China Sea Bering Sea Persian Gulf Bay of Bengal Sea of Okhotsk ________________________________________________________________________________ Islands: New Guinea Taiwan Sri Lanka Singapore Maldives Sakhalin Sumatra Borneo Java Honshu Philippines Luzon Mindanao Cyprus Hokkaido ________________________________________________________________________________ Straits/Canals: Str. of Malacca Bosporas Dardanelles Suez Canal Str. of Hormuz ________________________________________________________________________________ Rivers: Huang Yangtze Tigris Euphrates Amur Ob Mekong Indus Ganges Brahmaputra Lena _______________________________________________________________________________ Mountains, Plateaus, -
Sea-Level Rise for the Coasts of California, Oregon, and Washington: Past, Present, and Future
Sea-Level Rise for the Coasts of California, Oregon, and Washington: Past, Present, and Future As more and more states are incorporating projections of sea-level rise into coastal planning efforts, the states of California, Oregon, and Washington asked the National Research Council to project sea-level rise along their coasts for the years 2030, 2050, and 2100, taking into account the many factors that affect sea-level rise on a local scale. The projections show a sharp distinction at Cape Mendocino in northern California. South of that point, sea-level rise is expected to be very close to global projections; north of that point, sea-level rise is projected to be less than global projections because seismic strain is pushing the land upward. ny significant sea-level In compliance with a rise will pose enor- 2008 executive order, mous risks to the California state agencies have A been incorporating projec- valuable infrastructure, devel- opment, and wetlands that line tions of sea-level rise into much of the 1,600 mile shore- their coastal planning. This line of California, Oregon, and study provides the first Washington. For example, in comprehensive regional San Francisco Bay, two inter- projections of the changes in national airports, the ports of sea level expected in San Francisco and Oakland, a California, Oregon, and naval air station, freeways, Washington. housing developments, and sports stadiums have been Global Sea-Level Rise built on fill that raised the land Following a few thousand level only a few feet above the years of relative stability, highest tides. The San Francisco International Airport (center) global sea level has been Sea-level change is linked and surrounding areas will begin to flood with as rising since the late 19th or to changes in the Earth’s little as 40 cm (16 inches) of sea-level rise, a early 20th century, when climate. -
Coastal Erosion in Cape Cod, Massachusetts: Finding Sustainable Solutions Michael D
University of Massachusetts Amherst ScholarWorks@UMass Amherst Student Showcase Sustainable UMass 2015 Coastal Erosion in Cape Cod, Massachusetts: Finding Sustainable Solutions Michael D. Roberts University of Massachusetts - Amherst, [email protected] Lauren Bullard University of Massachusetts - Amherst Shaunna Aflague University of Massachusetts - Amherst Kelsi Sleet University of Massachusetts - Amherst Follow this and additional works at: https://scholarworks.umass.edu/ sustainableumass_studentshowcase Part of the Environmental Policy Commons, and the Environmental Studies Commons Roberts, Michael D.; Bullard, Lauren; Aflague, Shaunna; and Sleet, Kelsi, "Coastal Erosion in Cape Cod, Massachusetts: indF ing Sustainable Solutions" (2015). Student Showcase. 6. Retrieved from https://scholarworks.umass.edu/sustainableumass_studentshowcase/6 This Article is brought to you for free and open access by the Sustainable UMass at ScholarWorks@UMass Amherst. It has been accepted for inclusion in Student Showcase by an authorized administrator of ScholarWorks@UMass Amherst. For more information, please contact [email protected]. Coastal Erosion in Cape Cod 1 Coastal Erosion in Cape Cod, Massachusetts: Finding Sustainable Solutions Michael Roberts, Lauren Bullard, Shaunna Aflague, and Kelsi Sleet NRC 576 Water Resources Management and Policy Fall 2014 Coastal Erosion in Cape Cod 2 ABSTRACT The Massachusetts Office of Coastal Zone Management (CZM) and the Cape Cod Planning Commission have identified coastal erosion, flooding, and shoreline change as the number one risk affecting the heavily populated 1,068 square kilometers that constitute Cape Cod (CZM, 2013 and Cape Cod Commission 2010). This paper investigates natural and anthropogenic causes for coastal erosion and their relationship with established social and economic systems. Sea level rise, climate change, and other anthropogenic changes increase the rate of coastal erosion. -
THE CAPE MAY PENINSULA Is Not Like the Rest of New Jersey
U.S. Fish & Wildlife Service THE CAPE MAY PENINSULA Is Not Like the Rest of New Jersey Fall migration of monarch butterflies Photographs: USFWS Unique Ecosystems Key Migratory Corridor If you have noticed something The Cape May Peninsula is well-known “different” about the Cape May as a migratory route for raptors such Peninsula, particularly in regard to as the sharp-shinned hawk (Accipiter its vegetation types, of course you striatus), osprey (Pandion haliaetus), are right! The Cape May Peninsula and northern harrier (Circus cyaneus), is not like the rest of New Jersey. The as well as owl species in great numbers. primary reason is climatic: nestled at The peninsula’s western beaches within Piping plover chick low elevation between the Atlantic Delaware Bay provide the largest Ocean and the Delaware Bay, the spawning area for horseshoe crabs peninsula enjoys approximately 225 (Limulus polyphemus) in the world frost-free days at its southern tip and, as a result, sustain a remarkable compared to 158 days at its northern portion of the second largest spring end. The vegetation, showing strong concentration of migrating shorebirds characteristics of the Pinelands flora in in North America. The increasingly the northern portion of the peninsula, rare red knot (Calidris canutus; a displays closer affinities to the mixed candidate for federal listing) as well hardwood forest of our country’s as the sanderling (C. alba), least southern Coastal Plain. Southern tree sandpiper (C. minutilla), dowitcher species such as the swamp chestnut oak (Limnodromus spp.), and ruddy (Quercus michauxii) and loblolly pine turnstone (Arenaria interpres) are (Pinus taeda) reach their northernmost some of the many bird species that distribution in Cape May County, while feed on horseshoe crab eggs to gain the common Pinelands trees such as weight for migration to their summer Swamp pink pitch pine (P. -
Rocky Intertidal, Mudflats and Beaches, and Eelgrass Beds
Appendix 5.4, Page 1 Appendix 5.4 Marine and Coastline Habitats Featured Species-associated Intertidal Habitats: Rocky Intertidal, Mudflats and Beaches, and Eelgrass Beds A swath of intertidal habitat occurs wherever the ocean meets the shore. At 44,000 miles, Alaska’s shoreline is more than double the shoreline for the entire Lower 48 states (ACMP 2005). This extensive shoreline creates an impressive abundance and diversity of habitats. Five physical factors predominantly control the distribution and abundance of biota in the intertidal zone: wave energy, bottom type (substrate), tidal exposure, temperature, and most important, salinity (Dethier and Schoch 2000; Ricketts and Calvin 1968). The distribution of many commercially important fishes and crustaceans with particular salinity regimes has led to the description of “salinity zones,” which can be used as a basis for mapping these resources (Bulger et al. 1993; Christensen et al. 1997). A new methodology called SCALE (Shoreline Classification and Landscape Extrapolation) has the ability to separate the roles of sediment type, salinity, wave action, and other factors controlling estuarine community distribution and abundance. This section of Alaska’s CWCS focuses on 3 main types of intertidal habitat: rocky intertidal, mudflats and beaches, and eelgrass beds. Tidal marshes, which are also intertidal habitats, are discussed in the Wetlands section, Appendix 5.3, of the CWCS. Rocky intertidal habitats can be categorized into 3 main types: (1) exposed, rocky shores composed of steeply dipping, vertical bedrock that experience high-to- moderate wave energy; (2) exposed, wave-cut platforms consisting of wave-cut or low-lying bedrock that experience high-to-moderate wave energy; and (3) sheltered, rocky shores composed of vertical rock walls, bedrock outcrops, wide rock platforms, and boulder-strewn ledges and usually found along sheltered bays or along the inside of bays and coves. -
Ectoparasitic Community of the Mahali Mole-Rat, Cryptomys Hottentotus
Fagir et al. Parasites Vectors (2021) 14:24 https://doi.org/10.1186/s13071-020-04537-w Parasites & Vectors SHORT REPORT Open Access Ectoparasitic community of the Mahali mole-rat, Cryptomys hottentotus mahali: potential host for vectors of medical importance in South Africa Dina M. Fagir1* , Nigel C. Bennett1†, Eddie A. Ueckermann2, Alexandra Howard1 and Daniel W. Hart1† Abstract Background: The endemic rodent family of Bathyergidae in Africa, particularly South Africa, are understudied as reservoirs of diseases of signifcant medical importance. Considering the diversity and wide distribution of African mole-rats in South Africa, many of these bathyergids could act as carriers of zoonoses. Methods: The present study assessed the ectoparasite community of the Mahali mole-rat (Cryptomys hottentotus mahali). We aimed to identify possible parasitic arthropods that may infest this mole-rat species and explore host preference, contributions of seasonality, host sex and body mass as well as social class and colony size on ectoparasite assemblage prevalence and abundance. Results: A limited number of ectoparasite species were found on C. h. mahali belonging to two signifcant taxa: mites (Acari) and feas, with mites being the most prevalent and abundant. We recorded the presence of X. philoxera, a fea well known as the principal reservoir of plague in the southern African region on the Mahali mole-rats. Only three mite species were collected: Androlaelaps scapularis, Androlaelaps capensis and Laelaps liberiensis. Seasonal peaks in prevalence and abundance of X. philoxera and A. scapularis were observed during summer. Xenopsylla philoxera abundance and A. scapularis loads signifcantly increased on reproductive mole-rat individuals in comparison to non- reproductive individuals. -
A Lost Biome: Part I
AA lostlost biome:biome: AA taletale ofof thethe SouthSouth AfricanAfrican coastalcoastal floraflora AA lostlost biome:biome: AA taletale ofof thethe SouthSouth AfricanAfrican coastalcoastal floraflora Alastair Potts, Adriaan Grobler & Richard Cowling Linda’s House of Crazy Linda’s House of Crazy Here be dragons... A lost biome: Part I Species richness? Compared with the CFR? Lombard&Cowling 2002 Compared with the CFR? Lombard&Cowling 2002 Compared with the CFR? Compared with the CFR? Coastal Dune Flora: Global Comparison Coastal Dune Flora: Global Comparison Coastal Dune Flora: Global Comparison Coastal Dune Flora: Global Comparison Coastal Dune Flora: Global Comparison 10 x 10 m >45 species Coastal Dune Vegetation: ~1200 species (Excluding widespread “guests”) With “guests”: ~2400 species Coastal Dune endemics: ~300 species (work in progress) Why is this linear, fragmented flora so rich? Full Interglacial Full Glacial Fisher et al. 2010 Quaternary Science Reviews Cawthra et al (in prep) Coastal Dune Vegetation: <<<1% of “historic” distribution Coastal Dune Vegetation: <<<1% of “historic” distribution But... “Least Concern” A lost biome: Part II A lost biome: Part II A rose by any other name...? A summary of the overall problem (in the vegmap) The current state of “coastal dunes” Overberg Dune Strandveld Algoa Dune Strandveld Agulhas Sand Fynbos Blombos Dune Strandveld Groot Brak Dune Strandveld Albany Dune Strandveld Agulhas Limestone Fynbos Albertinia Sand Fynbos Knysna Sand Fynbos Southern Cape Dune Fynbos De Hoop Limestone Fynbos Canca Limestone Fynbos Southern Cape Dune Fynbos Algoa Sandstone Fynbos Cape Seashore Vegetation Azonal Dune Strandveld Limestone Fynbos Sand Fynbos Sandstone Fynbos Cape Seashore Vegetation Overberg Dune Strandveld Agulhas Limestone Fynbos Agulhas Sand Fynbos Algoa Sandstone Fynbos Algoa Dune Strandveld Blombos Dune Strandveld De Hoop Limetsone Fynbos Albertinia Sand Fynbos Albany Dune Strandveld Groot Brak Dune Strandveld Canca Limestone Fynbos Knysna Sand Fynbos S. -
Maine's Coastal Wetlands
Program Support from: Maine Department of Environmental Protection NOAA Coastal Services Center Maine Coastal Program, Maine State Planning Office Maine Department of Marine Resources MAINE'S COASTAL WETLANDS: I. TYPES, DISTRIBUTION, RANKINGS, FUNCTIONS AND VALUES by Alison E. Ward NOAA Coastal Management Fellow Bureau of Land & Water Quality Division of Environmental Assessment Augusta, ME September 1999 DEPLW1999 - 13 TABLE OF CONTENTS Page # ACKNOWLEDGEMENTS .........................................................................................................................ii SUMMARY..................................................................................................................................................iii INTRODUCTION ........................................................................................................................................ 1 COASTAL DEVELOPMENT..................................................................................................................... 7 NRPA PERMITTED ACTIVITY IN COASTAL WETLANDS ............................................................................... 8 NRPA PERMITTED ACTIVITY IN COASTAL WETLANDS BY REGIONAL OFFICE .......................................... 11 COASTAL WETLAND IMPACT..................................................................................................................... 14 TYPES & DISTRIBUTION OF INTERTIDAL HABITATS................................................................. 17 TYPES AND ACREAGE OF INTERTIDAL -
Micromammal Paleoecology
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by CU Scholar Institutional Repository University of Colorado, Boulder CU Scholar Anthropology Graduate Theses & Dissertations Anthropology Spring 1-1-2011 Micromammal Paleoecology: Theory, Methods, and Application to Modern and Fossil Assemblages in The rC adle of Humankind World Heritage Site, South Africa Jennifer Nicole Leichliter University of Colorado at Boulder, [email protected] Follow this and additional works at: http://scholar.colorado.edu/anth_gradetds Part of the Biological and Physical Anthropology Commons Recommended Citation Leichliter, Jennifer Nicole, "Micromammal Paleoecology: Theory, Methods, and Application to Modern and Fossil Assemblages in The Cradle of Humankind World Heritage Site, South Africa" (2011). Anthropology Graduate Theses & Dissertations. Paper 7. This Thesis is brought to you for free and open access by Anthropology at CU Scholar. It has been accepted for inclusion in Anthropology Graduate Theses & Dissertations by an authorized administrator of CU Scholar. For more information, please contact [email protected]. Micromammal Paleoecology: Theory, Methods, and Application to Modern and Fossil Assemblages in The Cradle of Humankind World Heritage Site, South Africa by Jennifer Leichliter B.A., Colorado College, 2008 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 Master’s of Anthropology Department of Anthropology 2011 This thesis entitled: Micromammal Paleoecology: Theory, Methods, and Application to Modern and Fossil Assemblages in The Cradle of Humankind World Heritage Site, South Africa written by Jennifer Nicole Leichliter has been approved for the Department Anthropology ________________________________________________ Dr. -
Northland Regional Landscape Assessment Worksheet
Northland Regional Landscape Assessment Worksheet Unit name – WAIKUKU BEACH TO TOM BOWLING BAY LOWLAND DESCRIPTION AND CHARACTERISATION Component Comment Land Types A broad tombolo of accumulated sand that has formed between the (refer to list overleaf) former island of North Cape headland and the mainland body. Beach Swamps and peat deposits have built up on this area as sands have Dune complex Coastal plain (tombolo) created pans and drainage is impeded. Wetlands Lakes and waterbodies Geology Holocene foredunes overlying eroded Pleistocene consolidated dune (including geopreservation sites) sand associated with Tom Bowling Bay and Waikuku Beach. Pleistocene-Holocene muddy and sandy interdune deposits on tombolo bordered by Pleistocene-Holocene foredune belts creating freshwater wetlands in muddy and sandy interdune deposits. NZ Geopres Inventory: Waikuku Beach (north) and Waikuku Beach (south) Miocene limestone sites – only marine middle or late Miocene fauna known north of Kawhia or East Cape. Waikuku Flat dune dammed swamp – a large area in the centre of the tombolo. Soil Types Te Kopuru sand, Ohia sand, Ruakaka peaty sandy loam, Hurewai fine sandy loam, Te Hapua fine sandy loam, Kapuwairua clay and silty clay, eroded remains of Red Hill sandy clay loam. Ecology Waikuku Beach is considered a good example of a nationally (including protected vegetation / features, threatened habitat type supporting threatened and regionally PNAP Level 1 and 2 sites) significant species . Tom Bowling Bay contains a diverse array of plant and animal taxa, including several threatened species within a nationally uncommon habitat type (dunefields). A range of wetland / peat favouring ecological units are developed around depressions and wet areas in the central part of the tombolo. -
Should North Carolina & Holden Beach Retrofit
SHOULD NORTH CAROLINA & HOLDEN BEACH RETROFIT THEIR BARRIER ISLAND INLETS? BEAUFORT BOGUE INLET INLET NEW RIVER CAPE HEADLAND LOOKOUT & SHOALS FIGURE 8 LOCKWOOD FOLLY INLET HOLDEN BEACH FORT FISHER HEADLAND CAPE FEAR ONSLOW BAY OAK ISLAND & FRYING COLOR SOUTH HEADLAND PAN SHOALS CAROLINA TOPOGRAPHY MAP (LiDAR DATA) LONG BAY) BARRIER ISLAND TYPES: ONSLOW & LONG BAYS SAND-POOR, SIMPLE BARRIER ISLANDS IN RISING SEA LEVELS THE ISLANDS MIGRATE LANDWARD OVER THE MARSH LIKE A TANK TREAD LEAVING MARSH PEAT CROPPING OUT ON THE SHOREFACE BACK-BARRIER SALT MARSHES FORM ON OVERWASH FANS & INLET FLOOD-TIDE DELTAS INLETS--OUTLETS CRITICAL ISLAND BUILDING PROCESSES THAT DEPOSIT BACK- BARRIER SHOALS, INCREASE ISLAND WIDTH, & FORM MARSH HABITAT. UPLANDS CAPE FEAR RIVER WACCAMAW DRAINAGE SYSTEM & GREEN SWAMP PALEO- SHORELINES & CAPE FORT FISHER SUB-AERIAL HEADLAND OLD CAPE FEAR RIVER CHANNEL OAK ISLAND SUBOAK-AERIAL ISLAND CAPE FEAR HEADLANDSUB-MARINE & FRYING HEADLAND PAN LONG BAY SHOALS US ACE 4.6 KM LONG & 9.1 M HIGH DAM BUILT IN 1881-1887 TO BLOCK CAPE FEAR RIVER DISCHARGE ON NE SIDE OF CAPE FEAR PSDS 6-5-2008 CAPE FEAR RIVER INLET DREDGED CHANNEL SEA LEVEL 5 m BATHYMETRIC CONTOURS IN M BELOW MEAN SEA LEVEL 10 m J. McNINCH, USACE 2004 HOLDEN BEACH, LONG BEACH, & CAPE FEAR 2016 PALEO-LOCKWOOD INTRA-COASTAL FOLLY RIVER WATERWAY CHANNEL DITCH OAK ISLAND LOCKWOOD ERODING FOLLY INLET HEADLAND CAPE FEAR RIVER DREDGED FRYING PAN CHANNEL SHOALS OAK ISLAND HEADLAND Blevins/Star News 1-21-2015 NEW RIVER SUB- MARINE HEADLAND (RIGGS, CLEARY, & SNYDER, 1995) NORTH TOPSAIL & ONSLOW BEACH ROCK HEADLAND SCARPS (CROWSON, 1980) ONSLOW BAY & LONG BAY HARDBOTTOMS THERE IS A GOOD REASON WHY SIMPLE BARRIER ISLANDS ARE SAND-POOR: THEY LACK A MAJOR SOURCE OF NEW SAND! NORTH CAROLINA’S ROCKY BEACH NORTH TOPSAIL ISLAND (M.