Changes of Arthropod Diversity Across an Altitudinal Ecoregional Zonation in Northwestern Argentina
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
The Biology of Casmara Subagronoma (Lepidoptera
insects Article The Biology of Casmara subagronoma (Lepidoptera: Oecophoridae), a Stem-Boring Moth of Rhodomyrtus tomentosa (Myrtaceae): Descriptions of the Previously Unknown Adult Female and Immature Stages, and Its Potential as a Biological Control Candidate Susan A. Wineriter-Wright 1, Melissa C. Smith 1,* , Mark A. Metz 2 , Jeffrey R. Makinson 3 , Bradley T. Brown 3, Matthew F. Purcell 3, Kane L. Barr 4 and Paul D. Pratt 5 1 USDA-ARS Invasive Plant Research Laboratory, Fort Lauderdale, FL 33314, USA; [email protected] 2 USDA-ARS Systematic Entomology Lab, Beltsville, MD 20013-7012, USA; [email protected] 3 USDA-ARS Australian Biological Control Laboratory, CSIRO Health and Biosecurity, Dutton Park QLD 4102, Australia; jeff[email protected] (J.R.M.); [email protected] (B.T.B.); [email protected] (M.F.P.) 4 USDA-ARS Center for Medical, Agricultural and Veterinary Entomology, Gainesville, FL 32608, USA; [email protected] 5 USDA-ARS, Western Regional Research Center, Invasive Species and Pollinator Health Research Unit, 800 Buchanan Street, Albany, CA 94710, USA; [email protected] * Correspondence: [email protected]; Tel.: +1-954-475-6549 Received: 27 August 2020; Accepted: 16 September 2020; Published: 23 September 2020 Simple Summary: Rhodomyrtus tomentosa is a perennial woody shrub throughout Southeast Asia. Due to its prolific flower and fruit production, it was introduced into subtropical areas such as Florida and Hawai’i, where it is now naturalized and invasive. In an effort to find sustainable means to control R. tomentosa, a large-scale survey was mounted for biological control organisms. -
Taiga Plains
ECOLOGICAL REGIONS OF THE NORTHWEST TERRITORIES Taiga Plains Ecosystem Classification Group Department of Environment and Natural Resources Government of the Northwest Territories Revised 2009 ECOLOGICAL REGIONS OF THE NORTHWEST TERRITORIES TAIGA PLAINS This report may be cited as: Ecosystem Classification Group. 2007 (rev. 2009). Ecological Regions of the Northwest Territories – Taiga Plains. Department of Environment and Natural Resources, Government of the Northwest Territories, Yellowknife, NT, Canada. viii + 173 pp. + folded insert map. ISBN 0-7708-0161-7 Web Site: http://www.enr.gov.nt.ca/index.html For more information contact: Department of Environment and Natural Resources P.O. Box 1320 Yellowknife, NT X1A 2L9 Phone: (867) 920-8064 Fax: (867) 873-0293 About the cover: The small photographs in the inset boxes are enlarged with captions on pages 22 (Taiga Plains High Subarctic (HS) Ecoregion), 52 (Taiga Plains Low Subarctic (LS) Ecoregion), 82 (Taiga Plains High Boreal (HB) Ecoregion), and 96 (Taiga Plains Mid-Boreal (MB) Ecoregion). Aerial photographs: Dave Downing (Timberline Natural Resource Group). Ground photographs and photograph of cloudberry: Bob Decker (Government of the Northwest Territories). Other plant photographs: Christian Bucher. Members of the Ecosystem Classification Group Dave Downing Ecologist, Timberline Natural Resource Group, Edmonton, Alberta. Bob Decker Forest Ecologist, Forest Management Division, Department of Environment and Natural Resources, Government of the Northwest Territories, Hay River, Northwest Territories. Bas Oosenbrug Habitat Conservation Biologist, Wildlife Division, Department of Environment and Natural Resources, Government of the Northwest Territories, Yellowknife, Northwest Territories. Charles Tarnocai Research Scientist, Agriculture and Agri-Food Canada, Ottawa, Ontario. Tom Chowns Environmental Consultant, Powassan, Ontario. Chris Hampel Geographic Information System Specialist/Resource Analyst, Timberline Natural Resource Group, Edmonton, Alberta. -
Report-VIC-Croajingolong National Park-Appendix A
Croajingolong National Park, Victoria, 2016 Appendix A: Fauna species lists Family Species Common name Mammals Acrobatidae Acrobates pygmaeus Feathertail Glider Balaenopteriae Megaptera novaeangliae # ~ Humpback Whale Burramyidae Cercartetus nanus ~ Eastern Pygmy Possum Canidae Vulpes vulpes ^ Fox Cervidae Cervus unicolor ^ Sambar Deer Dasyuridae Antechinus agilis Agile Antechinus Dasyuridae Antechinus mimetes Dusky Antechinus Dasyuridae Sminthopsis leucopus White-footed Dunnart Felidae Felis catus ^ Cat Leporidae Oryctolagus cuniculus ^ Rabbit Macropodidae Macropus giganteus Eastern Grey Kangaroo Macropodidae Macropus rufogriseus Red Necked Wallaby Macropodidae Wallabia bicolor Swamp Wallaby Miniopteridae Miniopterus schreibersii oceanensis ~ Eastern Bent-wing Bat Muridae Hydromys chrysogaster Water Rat Muridae Mus musculus ^ House Mouse Muridae Rattus fuscipes Bush Rat Muridae Rattus lutreolus Swamp Rat Otariidae Arctocephalus pusillus doriferus ~ Australian Fur-seal Otariidae Arctocephalus forsteri ~ New Zealand Fur Seal Peramelidae Isoodon obesulus Southern Brown Bandicoot Peramelidae Perameles nasuta Long-nosed Bandicoot Petauridae Petaurus australis Yellow Bellied Glider Petauridae Petaurus breviceps Sugar Glider Phalangeridae Trichosurus cunninghami Mountain Brushtail Possum Phalangeridae Trichosurus vulpecula Common Brushtail Possum Phascolarctidae Phascolarctos cinereus Koala Potoroidae Potorous sp. # ~ Long-nosed or Long-footed Potoroo Pseudocheiridae Petauroides volans Greater Glider Pseudocheiridae Pseudocheirus peregrinus -
Modeling the Boundaries of Plant Ecotones of Mountain Ecosystems
Article Modeling the Boundaries of Plant Ecotones of Mountain Ecosystems Yulia Ivanova 1,* and Vlad Soukhovolsky 2 1 Institute of Biophysics, Siberian Branch, Russian Academy of Sciences, Federal Research Center “Krasnoyarsk Science Center SB RAS”, Academgorodok 50-50, 600036 Krasnoyarsk, Russia 2 V.N. Sukachev Institute of Forest, Siberian Branch, Russian Academy of Sciences, Federal Research Center “Krasnoyarsk Science Center SB RAS”, Academgorodok 50-28, 600036 Krasnoyarsk, Russia; [email protected] * Correspondence: [email protected]; Tel.: +7-391-249-4328; Fax: +7-391-243-3400 Academic Editors: Isabel Cañellas and Timothy A. Martin Received: 30 August 2016; Accepted: 5 November 2016; Published: 12 November 2016 Abstract: The ecological second-order phase transition model has been used to describe height-dependent changes in the species composition of mountain forest ecosystems. Forest inventory data on the distribution of various tree species in the Sayan Mountains (south Middle Siberia) are in good agreement with the model proposed in this study. The model was used to estimate critical heights for different altitudinal belts of vegetation, determine the boundaries and extents of ecotones between different vegetation belts, and reveal differences in the ecotone boundaries between the north- and south-facing transects. An additional model is proposed to describe ecotone boundary shifts caused by climate change. Keywords: ecotone; boundaries of ecotones; mountain forest ecosystems; biodiversity 1. Introduction Any plant community has its own species composition and spatial structure. Within the space occupied by the community, it may be regarded as uniform and characterized by spatially invariable parameters. The boundaries of a community are determined by the effects of external modifying factors (such as temperature) on the plants and competitive interactions between the species that are not characteristic of this community but are present in the neighboring one [1,2]. -
2.2 Ecosystems of the World E
Ecotoxicology and Climate Edited by P. Bourdeau, J. A. Haines, W. Klein and C. R. Krishna Murti @ 1989 SCOPE. Published by John Wiley & Sons Ltd 2.2 Ecosystems of the World E. F. BRUENIG 2.2.1 DEFINITION An ecosystem is a community of organisms and their physical and chemical environment interacting as an ecological unit. It represents all biological and abiotic components, including man, within a defined and delimited biotope, and is characterized by distinct ecological biocoenotic features of structure and functioning. The ecosystem relates to many different scales. At the lowest end of the scale, the ecosystem may comprise a rock, a fallen tree, or a certain layer in a plant community (pico-ecosystem, as described by Ellenberg, 1973). At the largest end of the scale it relates to life support media and covers oceanic, terrestrial, limnic, or urban ecosystem categories (mega-ecosystem). The present description is restricted to terrestrial ecosystems and focuses in particular on potential natural vegetation. Centred on the plant formation, it classes natural forests and woodlands in hot and cold climates at macro-ecosystem level. The description is structured by classifying the forests and woodlands at micro- ecosystem (formation group) level according to major physiognomic, pheno- logical, and growth features in relation to the site and environmental conditions. These units correspond roughly to the bioclimatic life zones of Holdridge (1967). The description is patterned on the serial structure of the physiognomic- ecological classification of plant formations of the earth (Miiller-Dombois and Ellenberg, 1974, pp. 466-488) commonly quoted as the UNESCO Classification. 2.2.2 NATURAL VEGETATIONAL ZONES 2.2.2.1 Latitudinal Zonation The characteristic features of the zonal vegetation in each latitudinal zone are primarily determined and shaped by climate. -
BAREA ASBOLAEA, First for Britain, ADVENTIVE?
BAREA ASBOLAEA, First for Britain, ADVENTIVE? DISCOVERY My wife Helen and I started trapping in 1999 after attending and being enthralled at a Cornwall Wildlife Trust moth meeting. We are lucky in that we both share our passion for moths. We live and trap at Buryas Bridge, a small hamlet just west of Penzance in Cornwall. Local habitat is a steep sided valley with many mature Sycamore and a some Ash. A few Oak and Beech etc struggle with the occasional gales of salt laden wind from the North coast, some 8 miles away. Surrounding farm land is very non intensive beef rearing. Over the years we have had the occasional exciting catches such as a Eublemma Purpurina and Spoladia Recurvalis. We have now discovered our most notable catch has lain hidden in our records under a mistaken identity and we have to date caught over 180 of them! Around 2006 we started looking more seriously at our micros. Among them was a very similar moth to D. Pastinacella, the Parsnip moth. Our book sources were quickly exhausted so we turned to friend Frank Johns. His mothing experience extends over 50 years. He has a very good library and the nearest match for our moth seemed to be D. Pimpinellae. Although Frank, and ourselves were not really happy with the identity because this species had only been recorded in Cornwall once before in 1904, and the food plant is not known to grow here. Frank also consulted Phil Boggis, former county recorder who also thought D. Pimpellae to be the nearest match, but he also was not sure about it. -
Sharp Altitudinal Gradients in Magellanic Sub-Antarctic Streams: Patterns Along a Fluvial System in the Cape Horn Biosphere Rese
Author's personal copy Polar Biol DOI 10.1007/s00300-015-1746-4 ORIGINAL PAPER Sharp altitudinal gradients in Magellanic Sub-Antarctic streams: patterns along a fluvial system in the Cape Horn Biosphere Reserve (55°S) 1,2,3,6 1,2,3,4 1,2,3,5,6 Tamara Contador • James H. Kennedy • Ricardo Rozzi • Jaime Ojeda Villarroel1,2,3,6 Received: 17 July 2014 / Revised: 20 June 2015 / Accepted: 22 June 2015 Ó Springer-Verlag Berlin Heidelberg 2015 Abstract Magellanic Sub-Antarctic streams run through Antarctic watershed is characterized by a sharp thermal steep, low-altitude mountainous gradients characterized by gradient, in which cumulative degree-days (°C) per year a topography that supports a mosaic of evergreen, mixed, sharply increase through a relatively short altitudinal gra- and deciduous forests, peat lands, and scrublands. Here, the dient (0–600 m above sea level). With the results from this macroinvertebrate fauna and their ecological interactions study, we can now study thermal tolerances of altitude- are poorly known. This study linked the distribution, restricted species or project changes in their distributions community composition, and functional feeding structure and voltinism patterns according to climate change sce- of benthic macroinvertebrates with physicochemical and narios. Ecosystems at higher latitudes and altitudes are thermal patterns along the altitudinal gradient of a Mag- experiencing some of the fastest rates of warming on the ellanic Sub-Antarctic watershed. Invertebrates were col- planet, and Magellanic Sub-Antarctic watersheds could be lected during the austral summers of 2008, 2009, and 2010 considered as ‘‘sentinel systems,’’ providing early warning at five different altitudes. -
Mangrove Assessment in Manamoc Island for Coastal Retreat Mitigation
Journal of Marine and Island Cultures, v7n1 — Martinez & Buot Mangrove assessment in Manamoc Island for coastal retreat mitigation Mylene R. Martinez Inocencio E. Buot Jr. (corresponding author) School of Environmental Science and Management, University of the Philippines Los Baños, College, Laguna School of Environmental Science and Management, University of Institute of Biological Sciences, College of Arts and Sciences, the Philippines Los Baños, College, Laguna University of the Philippines Los Baños, College, Laguna [email protected] Faculty of Management and Development Studies, University of the Philippines Open University, Los Baños, Laguna Publication Information: Received 5 April 2018, Accepted 11 May 2018, Available online 30 June 2018 DOI: 10.21463/jmic.2018.07.1.05 Abstract Manamoc Island is experiencing coastline retreat and is in urgent need of economical mitigating measures. This study explored the role of mangroves in the mitigation of coastal retreat in Manamoc Island. Assessment of mangroves through standard vegetation analysis was done in relation to the topography and coastal dynamics prevalent in Manamoc Island. Time series analysis of sand and mangrove cover change was carried out to determine the role of mangroves in coastal retreat mitigation. Cluster analysis revealed five clusters named after the dominant species: Cluster I – Avicennia marina (Forsk.) Vierh.; Cluster II – Bruguiera sexangula (Lour.) Poir.; Cluster III – Rhizophora apiculata Blume and Rhizophora mucronata Lam.; Cluster IV – Rhizophora mucronata Lam.; and Cluster V – Sonneratia alba J. Smith. The clustering pattern followed that of typical mangrove zonation landward, middleward, and seaward although with a relatively short width. Canonical correspondence analysis (CCA) indicated that environmental factors like soil texture, pH, N, and P influenced mangrove distribution in Manamoc Island. -
Classification of Wetlands and Deepwater Habitats of the United States
FGDC–STD-004-2013 Second Edition Classification of Wetlands and Deepwater Habitats of the United States Adapted from Cowardin, Carter, Golet and LaRoe (1979) Wetlands Subcommittee Federal Geographic Data Committee August 2013 Federal Geographic Data Committee Established by Office of Management and Budget Circular A-16, the Federal Geographic Data Committee (FGDC) promotes the coordinated development, use, sharing, and dissemination of geographic data. The FGDC is composed of representatives from the Departments of Agriculture, Commerce, Defense, Energy, Housing and Urban Development, the Interior, State, and Transportation; the Environmental Protection Agency (EPA); the Federal Emergency Management Agency (FEMA); the Library of Congress; the National Aeronautics and Space Administration (NASA); the National Archives and Records Administration; and the Tennessee Valley Authority. Additional Federal agencies participate on FGDC subcommittees and working groups. The Department of the Interior chairs the committee. FGDC subcommittees work on issues related to data categories coordinated under the circular. Subcommittees establish and implement standards for data content, quality, and transfer; encourage the exchange of information and the transfer of data; and organize the collection of geographic data to reduce duplication of effort. Working groups are established for issues that transcend data categories. For more information about the committee, or to be added to the committee’s newsletter mailing list, please contact: Federal Geographic Data Committee Secretariat c/o U.S. Geological Survey 590 National Center Reston, Virginia 22092 Telephone: (703) 648-5514 Facsimile: (703) 648-5755 Internet (electronic mail): [email protected] Anonymous FTP: ftp://fgdc.er.usgs.gov/pub/gdc/ World Wide Web: http://fgdc.er.usgs.gov/fgdc.html This standard should be cited as: Federal Geographic Data Committee. -
British Lepidoptera (/)
British Lepidoptera (/) Home (/) Anatomy (/anatomy.html) FAMILIES 1 (/families-1.html) GELECHIOIDEA (/gelechioidea.html) FAMILIES 3 (/families-3.html) FAMILIES 4 (/families-4.html) NOCTUOIDEA (/noctuoidea.html) BLOG (/blog.html) Glossary (/glossary.html) Family: OECOPHORIDAE (2T 18G +1EX 25S +2EX+1CI) Ref: MBGBI4.1 Suborder:Glossata Infraorder:Heteroneura Superfamily:Gelechioidea As treated in MBGBI4.1 Oecophoridae was a large and diverse family with no apparent morphological features identifying a moth as belonging to this family and excluding all others. It has now been broken up so that the current concept of the family only contains the subfamilies Oecophorinae and Philobotinae of MBGBI4.1. These two now are considered together in Subfamily: Oecophorinae and split at Tribe level (Oecophorini and Philobotini). All British species are now in Subfamily: Oecophorinae. MBGBI4.1's Subfamily Chimabachinae is now Family 29: Chimabachidae. Subfamily Amphisbatinae is now Family 30: Lypusidae. Subfamily Carcininae is now Family 31: Peleopodidae. Subfamily Depressariinae is now Family 32 Depressariidae. Subfamily Stathmopodinae is now Family 42: Stathmopodidae. ws: 7-30mm Body held horizontally at rest with wings tectiform or flat and overlapping and antennae alongside body below wings Head smooth, Ocelli absent, Proboscis well-developed Antennae at least 3/5 fw length; scape usually with pecten Labial palps moderate to long, usually upcurved Fw lanceolate to to broadly ovate or subquadrate, Hw lanceolate to ovate Hindtibia hairy Keyed as: 1. hw cilia longer than hw breadth > head smooth-scaled > hindtibia without long bristles > head with scales broader than shaft of antenna > hw oval not produced at apex OR 2. hw cilia shorter than hw breadth > frenulum present > proboscis developed, scaled > hindtibia evenly long-haired > hw oval or broad oblong, not produced at apex (This will key to all families formerly contained in Oecophordae except Stahmopodidae. -
Altitudinal Zonation of Bryophytes on the Huon Peninsula, Papua New Guinea. a Floristic Approach, with Phytogeogra- Phic Considerations
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Hochschulschriftenserver - Universität Frankfurt am Main 61 Tropical Bryology 2: 61-90, 1990 Altitudinal zonation of Bryophytes on the Huon Peninsula, Papua New Guinea. A floristic approach, with phytogeogra- phic considerations Johannes Enroth Department of Botany, University of Helsinki, Unioninkatu 44, SF-00170, Helsinki, Finland. Abstract. The study is based on the major part of the bryophyte material collected during the Koponen-Norris expedition on the Huon Peninsula, Papua New Guinea, in 1981. Only taxa which were collected at least twice are included. Five altitudinal zones, the boundaries of which are indicated by discontinuities in the bryophyte flora, are distinguished: 0 - 300 m, 300 - 1200 m, 1200 - 2200(-2300) m, 2200(-2300) - 2800(- 2900) m, and 2800(-2900) -3400 m. These zones, each characterized by a typical species assemblage, are well in accordance with some earlier New Guinean zonation schemes based on the phanerogamic flora and vegetation. The most obvious correlations between bryophytes’ altitudinal ranges on the Huon Peninsula and their general phytogeography are: New Guinean or Western Melanesian endemics, as well as Malesian endemics, are concentrated at relatively high altitudes (zones III-V); Asian - Oceanian and Asian - Oceanian - Australian taxa, notably mosses, are relatively strongly represented at low to moderate altitudes (zones I-III); species which have their main distribution in the northern hemisphere occur at high altitudes; 'cosmopolitan' species either have wide vertical ranges or are restricted to high altitudes. Introduction Nadkarni (1978), and Johns (1982). Robbins (1959) and Royen (1980) mainly The altitudinal zonation of vegetation in dealt with the New Guinean mountain the tropics is distinct and, in many regions, vegetation. -
A Geographical Model for the Altitudinal Zonation of Mire Types in the Uplands of Western Europe: the Example of Les Monts Du Forez in Eastern France
A geographical model for the altitudinal zonation of mire types in the uplands of western Europe: the example of Les Monts du Forez in eastern France H. Cubizolle1 and G. Thebaud2 1Lyon University, EVS-ISTHME UMR 5600 CNRS, Saint-Etienne, France 2Herbarium Institute, Blaise Pascal University, Clermont-Ferrand, France _______________________________________________________________________________________ SUMMARY The geographical distribution of mires in the oceanic mountain ranges of western Europe cannot be explained without bringing together a number of physical and human factors. In Les Monts du Forez, which are granitic and metamorphic mountains covering an area of 1800 km2 and rising to an altitude of 1634 m in the east of the French Massif Central, a series of mires on long slopes reflects the effects of changing combinations of these factors with altitude. The scale of variation falls within the limits of bioclimatic levels and is manifest as: the absence of mires at foothill levels below 900 m; small mires of anthropogenic origin and remnant peat at lower mountain levels between 900 m and 1100 m; peat systems where evolution has been more or less affected by human intervention at median mountain levels between 1100 m and 1250 m; large ombrotrophic mires, often naturally convex and dating from the first half of the Holocene epoch, at upper mountain levels between 1250 m and 1450 m; and small established mires that are more or less directly linked to human intervention at sub-alpine levels above 1450 m. The role of human societies appears to dominate, with exceptions in the upper mountain levels. Human influence presents in two forms, both of which are related to the old traditional farming methods of the region: the first is destruction of mires, mostly by drainage, and the second is mire creation through modifications of the hydrology of the valley floor and the vegetation cover.