CERATOZETIDAE OF THE WESTERN NORTH AMERICAN ARCTIC

1985 ◽  
Vol 117 (11) ◽  
pp. 1287-1366 ◽  
Author(s):  
Valerie M. Behan-Pelletier

AbstractThe Ceratozetidae of arctic western North America, represented by 12 species in 9 genera, are discussed. A new genus, Cyrtozetes, and species, Cyrtozetes denaliensis, are proposed, and Trichoribates copperminensis Hammer, T. polaris Hammer, Svalbardia paludicola Thor, Iugoribates gracilis Sellnick, Diapterobates notatus (Thorell) both adults and immatures, D. variabilis Hammer, Sphaerozetes arcticus Hammer, Fuscozetes sellnicki Hammer, Melanozetes longisetosus Hammer, and Ceratozetes spitsbergensis Thor and C. parvulus Sellnick are redescribed. Immatures of T. polaris, S. paludicola, F. sellnicki, and M. longisetosus are described. Distribution records of Ceratozetes gracilis (Michael) in the western North American arctic are listed. The new combination, Cyrtozetes shiranensis (Aoki and Fujikawa), is proposed.

1986 ◽  
Vol 118 (10) ◽  
pp. 991-1057 ◽  
Author(s):  
Valerie M. Behan-Pelletier

AbstractRepresentatives of the oribatid mite family Ceratozetidae of subarctic western North America, including 14 species in eight genera, are treated. A new genus Laminizetes, and eight new species, Diapterobates siccatus, Trichoribates ogilviensis, Laminizetes fortispinosus, Ceratozetes inupiaq, C. kutchin, C. fjellbergi, Sphaerozetes firthensis, and Melanozetes tanana, are proposed, and Dentizetes rudentiger Hammer, Diapterobates humeralis (Hermann), Neogymnobates luteus (Hammer), Trichoribates striatus Hammer, Sphaerozetes castaneus Hammer, and Melanozetes meridianus Sellnick are redescribed. Immatures of Dentizetes rudentiger and Sphaerozetes firthensis are described. A key to the adults of the 31 species of Ceratozetidae recorded from the western North American arctic and subarctic is given. Relationships among the 12 genera in the Ceratozetidae recorded from the North American arctic and subarctic are discussed.


1979 ◽  
Vol 111 (2) ◽  
pp. 127-141 ◽  
Author(s):  
K.G.A. Hamilton

AbstractKeys are provided to the five genera and 12 species of Philaenini in North America. Philaenus (Stål) is redefined to include only two species, one of which, spumarius L., 1758 (= rubra Capanni, 1894, = aurata Capanni, 1894, new synonymies) is represented in North America by three introduced subspecies: quadrimaculatus (Sch.) in eastern and western continental America, spumarius s.s. in Newfoundland, and tesselatus (Mel.) from one locality in southern Ontario. Philaenus parallels Stearns is removed to Paraphilaenus Vilb. as its sole Nearctic representative (new combination) and Philaenus lineatus (L.) belongs to the distinctive genus Neophilaenus Hpt. Philaronia Ball is represented in North America by five species: abjecta (Uhl.), canadensis (Wal.), fuscovaria (Stål) new combination, pauca n. sp. and superba n. sp. Philaenarcys new genus includes three species: bilineata (Say), 1831, new combination (= Ptyelus basivitta Wlk., 1851, new synonymy), killa n. sp., and spartina n. sp.


Forests ◽  
2021 ◽  
Vol 12 (6) ◽  
pp. 751
Author(s):  
Francesco Dovana ◽  
Paolo Gonthier ◽  
Matteo Garbelotto

Phlebiopsis gigantea (Fr.) Jülich is a well-known generalist conifer wood saprobe and a biocontrol fungus used in several world countries to prevent stump infection by tree pathogenic Heterobasidion fungal species. Previous studies have reported the presence of regional and continental genetic differentiation in host-specific fungi, but the presence of such differentiation for generalist wood saprobes such as P. gigantea has not been often studied or demonstrated. Additionally, little information exists on the distribution of this fungus in western North America. The main purposes of this study were: (I) to assess the presence of P. gigantea in California, (II) to explore the genetic variability of P. gigantea at the intra and inter-continental levels and (III) to analyze the phylogeographic relationships between American and European populations. Seven loci (nrITS, ML5–ML6, ATP6, RPB1, RPB2, GPD and TEF1-α) from 26 isolates of P. gigantea from coniferous forests in diverse geographic distribution and from different hosts were analyzed in this study together with 45 GenBank sequences. One hundred seventy-four new sequences were generated using either universal or specific primers designed in this study. The mitochondrial ML5–ML6 DNA and ATP6 regions were highly conserved and did not show differences between any of the isolates. Conversely, DNA sequences from the ITS, RPB1, RPB2, GPD and TEF1-α loci were variable among samples. Maximum likelihood analysis of GPD and TEF1-α strongly supported the presences of two different subgroups within the species but without congruence or geographic partition, suggesting the presence of retained ancestral polymorphisms. RPB1 and RPB2 sequences separated European isolates from American ones, while the GPD locus separated western North American samples from eastern North American ones. This study reports the presence of P. gigantea in California for the first time using DNA-based confirmation and identifies two older genetically distinct subspecific groups, as well as three genetically differentiated lineages within the species: one from Europe, one from eastern North America and one from California, with the latter presumably including individuals from the rest of western North America. The genetic differentiation identified here among P. gigantea individuals from coniferous forests from different world regions indicates that European isolates of this fungus should not be used in North America (or vice versa), and, likewise, commercially available eastern North American P. gigantea isolates should not be used in western North America forests. The reported lack of host specificity of P. gigantea was documented by the field survey and further reinforces the need to only use local isolates of this biocontrol fungus, given that genetically distinct exotic genotypes of a broad generalist microbe may easily spread and permanently alter the microbial biodiversity of native forest ecosystems.


2021 ◽  
Vol 2 (2) ◽  
pp. 395-412
Author(s):  
Patrick Martineau ◽  
Hisashi Nakamura ◽  
Yu Kosaka

Abstract. The wintertime influence of tropical Pacific sea surface temperature (SST) variability on subseasonal variability is revisited by identifying the dominant mode of covariability between 10–60 d band-pass-filtered surface air temperature (SAT) variability over the North American continent and winter-mean SST over the tropical Pacific. We find that the El Niño–Southern Oscillation (ENSO) explains a dominant fraction of the year-to-year changes in subseasonal SAT variability that are covarying with SST and thus likely more predictable. In agreement with previous studies, we find a tendency for La Niña conditions to enhance the subseasonal SAT variability over western North America. This modulation of subseasonal variability is achieved through interactions between subseasonal eddies and La Niña-related changes in the winter-mean circulation. Specifically, eastward-propagating quasi-stationary eddies over the North Pacific are more efficient in extracting energy from the mean flow through the baroclinic conversion during La Niña. Structural changes of these eddies are crucial to enhance the efficiency of the energy conversion via amplified downgradient heat fluxes that energize subseasonal eddy thermal anomalies. The enhanced likelihood of cold extremes over western North America is associated with both an increased subseasonal SAT variability and the cold winter-mean response to La Niña.


1964 ◽  
Vol 21 (5) ◽  
pp. 933-939 ◽  
Author(s):  
Richard H. Rosenblatt

A new species, Pholis clemensi, referred to the family Pholidae, is named and described from 12 specimens taken in southern British Columbia waters and the Strait of Juan de Fuca. Pholis clemensi is compared with other members of the genus, and a key is given to the North American species.


Zootaxa ◽  
2019 ◽  
Vol 4683 (3) ◽  
pp. 301-335 ◽  
Author(s):  
FRANK E. ETZLER

The genus Limonius Eschscholtz, 1829 was last treated as a whole by Candèze (1860). Since then, members have been placed in eight other genera: Cidnopus Thomson, 1859; Gambrinus LeConte, 1853; Elathous Reitter, 1890; Kibunea Kishii, 1966; Limoniscus Reitter, 1905; Nothodes LeConte, 1861; Pheletes Kiesenwetter, 1858; and Solskyana Dolin, 1978. Based on the examination of adult and larval characters, five genera are recognized: Elathous Reitter, 1890; Gambrinus LeConte, 1853; Limonius Eschscholtz, 1829; Pheletes Kiesenwetter, 1858; and Tetralimonius new genus. Limoniscus Reitter, 1905 and Sichuanelater Platia and Gudenzi, 2006 are new synonymies of Gambrinus LeConte, 1853; Micrathous Lane, 1971, Neoathousius Schimmel and Platia, 1991 and Solskyana Dolin, 1978 are all new synonymies of Limonius. A total of 84 new combinations are proposed: Nearctic: Elathous huguenini (Van Dyke, 1932) new combination; Gambrinus angulatus (Motschulsky, 1859) new combination; Gambrinus bicolor (Van Dyke, 1932) new combination; Gambrinus clypeatus (Motschulsky, 1859) new combination; Gambrinus confusus (LeConte, 1853) new combination; Gambrinus cribriceps (Van Dyke, 1943) new combination; Gambrinus crotchii (Horn, 1872) new combination; Gambrinus flavomarginatus (Knull, 1938) new combination; Gambrinus fulvipilis (Candèze, 1860) new combination; Gambrinus griseus (Beauvois, 1805) new combination; Gambrinus humidus (Lane, 1941) new combination; Gambrinus interstitialis (Melsheimer, 1846) new combination; Gambrinus lanchesteri (Lane, 1941) new combination; Gambrinus meridianus (Knull, 1947) new combination; Gambrinus mirus (LeConte, 1853) new combination; Gambrinus norahae (Al Dhafer, 2009) new combination; Gambrinus olentangyi (Knull, 1947) new combination; Gambrinus plebejus (Say, 1825) new combination; Gambrinus propexus (Candèze, 1860) new combination; Gambrinus rudis (Brown, 1933) new combination; Gambrinus rufihumeralis (Lane, 1941) new combination; Gambrinus seminudus (Van Dyke, 1932) new combination; Gambrinus shircki (Lane, 1965) new combination; Gambrinus sinuifrons (Fall, 1907) new combination; Gambrinus snakensis (Lane, 1965) new combination; Gambrinus stigma (Herbst, 1806) new combination; Gambrinus pictus (Van Dyke, 1932) new combination; Gambrinus ulkei (Horn, 1871) new combination; Gambrinus ursinus (Van Dyke, 1932) new combination; Gambrinus venablesi (Wickham, 1913) new combination; Limonius brevis (Van Dyke, 1932) new combination; Limonius sordidus (Van Dyke, 1932) new combination; Pheletes lecontei (Lane, 1971) new combination; Tetralimonius definitus (Ziegler, 1845) new combination; Tetralimonius humeralis (Candèze, 1860) new combination; Tetralimonius maculicollis (Motschulsky, 1860) new combination; Tetralimonius nimbatus (Say, 1825) new combination; Tetralimonius ornatulus (LeConte, 1857) new combination. Palearctic: Gambrinus elegans (Buysson, 1891) new combination; Gambrinus gibbosus (Platia and Gudenzi, 2006) new combination. Gambrinus henanensis (Schimmel, 2006) new combination; Gambrinus hinakurai (Kishii, 1998) new combination; Gambrinus katoi (Kishii, 2002) new combination; Gambrinus kawaharai (Kishii, 2002) new combination; Gambrinus kucerai (Schimmel, 2006) new combination; Gambrinus nanshanensis (Arimoto and Hiramatsu, 2013) new combination; Gambrinus naomii (Kishii, 1997) new combination; Gambrinus shaanxiensis (Schimmel, 2006) new combination; Gambrinus suturalis (Gebler, 1844) new combination; Gambrinus takabai (Kishii, 1997) new combination; Gambrinus violaceus (Müller, 1821) new combination; Gambrinus wittmeri (Chassain, 1998) new combination; Gambrinus yamato (Kishii, 1998) new combination; Gambrinus yujii (Arimoto, 2013) new combination; Gambrinus zhejiangensis (Schimmel, 2015) new combination; Limonius brancuccii (Schimmel and Platia, 1991) new combination; Limonius decorus (Gurjeva, 1975) new combination; Limonius exiguus (Schimmel and Platia, 1991) new combination; Limonius hartmanni (Schimmel, 1998) new combination; Limonius hiermeieri (Schimmel and Platia, 1991) new combination; Limonius hirtus (Dolin, 1978) new combination; Limonius hubeiensis (Kishii and Jiang, 1996) new combination; Limonius kubani (Schimmel, 1996) new combination; Limonius loebli (Schimmel and Platia, 1991) new combination; Limonius longicornis (Schimmel and Platia, 1991) new combination; Limonius macedonicus (Cate and Platia, 1989) new combination; Limonius marginellus brusteli (Leseigneur, 2004) new combination; Limonius manaliensis (Schimmel and Platia, 1991) new combination; Limonius miandamensis (Schimmel and Platia, 1991) new combination; Limonius minusculus (Schimmel and Platia, 1991) new combination; Limonius nigronitidus (Han and Lee, 2012) new combination; Limonius platiai (Mertlik, 1996) new combination; Limonius pseudopilosus (Platia and Gudenzi 1985) new combination; Limonius recticornis (Schimmel and Platia, 1991) new combination; Limonius riesei (Platia, 1988) new combination; Limonius rusticus (Schimmel and Platia, 1991) new combination; Limonius schurmanni (Platia and Gudenzi, 1998) new combination; Limonius sinensis (Schimmel and Platia, 1994) new combination; Limonius singularis (Schimmeland Platia, 1991) new combination; Limonius stapfi (Schimmel, 2007) new combination; Limonius turcicus (Platia, 2004) new combination; Limonius wittmeri (Schimmel and Platia, 1991) new combination; Tetralimonius quercus (Olivier, 1790) new combination; Tetralimonius reitteri (Gurjeva, 1976) new combination. The following 12 North American species are removed from synonymy and recognized as valid species: Gambrinus interstitialis (Melsheimer, 1846) status resurrected; Gambrinus propexus (Candèze, 1860) status resurrected; Gambrinus shircki (Lane, 1965) status resurrected; Gambrinus snakensis (Lane, 1965) status resurrected; Gambrinus ulkei (Horn, 1871) status resurrected; Limonius anceps LeConte, 1853 status resurrected; Limonius dubitans LeConte, 1853 status resurrected; Limonius infuscatus Motschulsky, 1859 status resurrected; Limonius pilosulus Candèze, 1891 status resurrected; Limonis semianeus LeConte, 1853 status resurrected. Tetralimonius humeralis (Candèze, 1860) status resurrected; Tetralimonius maculicollis (Motschulsky, 1860) status resurrected. New replacement names are proposed for three homynyms: Limonius schimmeli Etzler new name for Neoathousius ferrugineus Schimmel and Platia, 1991; Elathous malatyanus Etzler new name for Elathous bicolor Platia, 2010, not Elathous bicolor (LeConte, 1853); and Microdesmes carteri Etzler new name for Limonius angulatus Carter, 1939 (= Microdesmes angulatus). Limonius kondratieffi Al Dhafer, 2009 is a new synonymy of Elathous bicolor (LeConte, 1853). A key to genera, generic descriptions, notes on species, and definitions of important characters are provided. 


2020 ◽  
Vol 33 (6) ◽  
pp. 2427-2447 ◽  
Author(s):  
Nathaniel C. Johnson ◽  
Lakshmi Krishnamurthy ◽  
Andrew T. Wittenberg ◽  
Baoqiang Xiang ◽  
Gabriel A. Vecchi ◽  
...  

AbstractPositive precipitation biases over western North America have remained a pervasive problem in the current generation of coupled global climate models. These biases are substantially reduced, however, in a version of the Geophysical Fluid Dynamics Laboratory Forecast-Oriented Low Ocean Resolution (FLOR) coupled climate model with systematic sea surface temperature (SST) biases artificially corrected through flux adjustment. This study examines how the SST biases in the Atlantic and Pacific Oceans contribute to the North American precipitation biases. Experiments with the FLOR model in which SST biases are removed in the Atlantic and Pacific are carried out to determine the contribution of SST errors in each basin to precipitation statistics over North America. Tropical and North Pacific SST biases have a strong impact on northern North American precipitation, while tropical Atlantic SST biases have a dominant impact on precipitation biases in southern North America, including the western United States. Most notably, negative SST biases in the tropical Atlantic in boreal winter induce an anomalously strong Aleutian low and a southward bias in the North Pacific storm track. In boreal summer, the negative SST biases induce a strengthened North Atlantic subtropical high and Great Plains low-level jet. Each of these impacts contributes to positive annual mean precipitation biases over western North America. Both North Pacific and North Atlantic SST biases induce SST biases in remote basins through dynamical pathways, so a complete attribution of the effects of SST biases on precipitation must account for both the local and remote impacts.


2002 ◽  
Vol 76 (1) ◽  
pp. 76-94 ◽  
Author(s):  
Frederick A. Sundberg ◽  
Linda B. McCollum

Kochaspids are an informal group of ptychopariid trilobites that were both abundant and widespread in the early Middle Cambrian of North America. Based on the reassociation of pygidia and cranidia of some kochaspids, Kochiella Poulsen, 1927, is redefined and Hadrocephalites n. gen. is proposed. Hadrocephalites includes taxa previously assigned by Rasetti and Palmer to Schistometopus Resser, 1938a. Schistometopus is considered nomen dubium. Representatives of Kochiella and Hadrocephalites from the Pioche Shale and Carrara Formation of Nevada are described, including the new species Kochiella rasettii, K. brevaspis, Hadrocephalites lyndonensis, and H. rhytidodes. Other kochaspids previously assigned to Kochaspis Resser, 1935; Eiffelaspis Chang, 1963; Schistometopus; and Kochiella are discussed and some are reassigned. The type specimens of Kochiella augusta (Walcott, 1886); K. crito (Walcott, 1917b); K. chares (Walcott, 1917a); K. mansfieldi Resser, 1939; K. arenosa Resser, 1939; Hadrocephalites carina (Walcott, 1917b), and H. cecinna (Walcott, 1917b) are re-illustrated.


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