ON CERTAIN SPECIES OF SATYRUS

1880 ◽  
Vol 12 (6) ◽  
pp. 109-115 ◽  
Author(s):  
W. H. Edwards

Conclusion.—The North American species of this genus may be divided into three Groups, with several sub-groups. Group 1 comprises Pegala and all the larger species. Group 2 Silvestris and others. characterized by their small size, and the peculiar outline of the discal band on under side of hind wings, there being two long serrations against end of cell. This division will throw Meadii into Group 1, in which the band has a rounded prominence against cell. Group 3 comprises Sthenele only.

1976 ◽  
Vol 108 (11) ◽  
pp. 1155-1165 ◽  
Author(s):  
C. D. Dondale ◽  
J. H. Redner

AbstractThe 50 known species of North American Clubiona Latreille, 1804 are rearranged in seven species-groups as follows: trivialis group (1 Holarctic, 4 Nearctic), obesa group (11 Nearctic), reclusa group (2 Holarctic, 3 Nearctic), pallidula group (1 Holarctic), abboti group (25 Nearctic), lutescens group (1 Holarctic, 1 Nearctic), maritima group (1 Nearctic). Clubiona quebecana and C. angulata are described as new species from eastern North America. C. kuratai Roddy, 1966, originally described from the female only, is synonymized under C. chippewa Gertsch, 1941, which was originally described from the male only. C. opeongo Edwards, 1958 and C. bishopi Edwards, 1958 are redescribed, the male of the former and the female of the latter not having been previously described.


Geofluids ◽  
2017 ◽  
Vol 2017 ◽  
pp. 1-13 ◽  
Author(s):  
Qin Ge ◽  
Xing Liang ◽  
Menggui Jin ◽  
Jing Li ◽  
Yan Liu

The hydrogeochemical and stable isotope compositions of aquitard porewater samples from three boreholes were investigated to determine the origin, salinization, and hydrochemical evolution of water in the North Jiangsu coastal plain, China. Three porewater groups were identified based on the water-bearing subsystems. The total dissolved solids (TDS) of porewater samples highly varied from 0.03 to 26.1 g/L. Molar Cl/Br ratios and δ18O and δ2H data indicate that the source of Group 1 salinized porewater was the Holocene seawater, whereas Group 3 salinized samples were probably related to the remnant palaeoseawater of the Late Pleistocene. Group 2 samples had low salinity (TDS < 1 g/L) and undetectable Br− concentrations, which were probably recharged during a colder period and without evidence of seawater involvement. The salinized porewater was likely diluted by freshwater, as evidenced by its depleted isotopes and low salinity relative to standard seawater. The ionic ratios and ionic deltas indicate that considerable water-rock interactions (e.g., cation exchange and mineral weathering) also accounted for the hydrochemical constituents of porewaters, and cation exchange seems to be more noticeable at low salinity.


Blood ◽  
2004 ◽  
Vol 104 (11) ◽  
pp. 3762-3762
Author(s):  
Julie Bergeron ◽  
Xiaoduan Weng ◽  
Louise Robin ◽  
Harold J. Olney ◽  
Denis Soulières

Abstract Introduction: Increasing multi-ethnicity is likely to make α-thalassemia more prevalent in western metropolitan areas. The current prevalence of α-thalassemia in regions outside the traditional thalassemia areas with the associated risk for HbH disease and hydrops foetalis is unknown. Genetic counseling for reproductive risks due to α-globin gene mutations requires adequate and precise genotyping. Objectives: To determine by multiplex polymerase chain reaction (m-PCR) the prevalence and genotypes of α-thalassemia among non selected, consecutive cases of unexplained microcytosis identified in a clinical hematology laboratory. To evaluate if differences or variations in erythrocytic indices are indicative of α-thalassemia. Methods: During a period of 3 months, α-globin genotype was determined by m-PCR on all non repetitive microcytic (MCV <80fL) blood samples from adults with normal ferritin and normal hemoglobin HPLC analysis (Variant I, Bio-Rad). A previously described m-PCR analysis allowed the detection of α-globin gene deletions and specifically identified each of the following 7 deletions when present: −α3.7, −α4.2, −−SEA, −−FIL, −−MED, −−THAI and −α(20.5). Results: 516 microcytic blood samples were evaluated of which 197 had normal ferritin and Hb HPLC analysis and were submitted for m-PCR. Among 196 interpretable m-PCRs, 148 did not have α-globin gene deletion(s) (group 1) and 48 α-thalassemia cases (24,5%) were identified: 28 cases of single α-globin gene deletion (group 2) and 20 cases of 2 α-globin gene deletions (group 3). In group 3, 6 cases showed deletions in cis. Results on differences between the groups are presented in Table 1. Even though some differences were statistically different, none was clinically useful and diagnostic. Conclusion: A significant proportion (24,5%) of cases with microcytosis not likely explained by iron deficiency, inflammation or a hemoglobinopathy are caused by α-globin gene deletion(s). This laboratory survey, despite a short period of sample collection (3 months) identified 6 carriers of a 2 gene deletion in cis that may have a severe impact on reproductive decisions and potential future utilisation of resources. These findings are likely to be reproducible in other North American cosmopolitan cities where α-thalassemia is not endemic but likely to be of increasing prevalence due to immigration. The availability, precision and reliability of diagnostic methods such as m-PCR and the increasing ethnic diversity of North-American cities point to an emerging need to develop genetic counseling programs based on the molecular diagnosis of α-thalassemia. Erythrocytic parameters with their standard deviation in the different α-globin genotype groups RBC (x1012/L) MCH (pg) Hb (g/dL) Mentzer† RDW MCV (fL) † calculated for samples with Hb>90 g/L *indicates values that are significantly different from data of other groups. RBC: Red Blood Cells, MCH: Mean Corpuscular Hemoglobin, Hb: Hemoglobin, RDW: Red Cells Distribution Width, MCV: Mean Corpuscular Volume group 1 (normal genotype) 4,27±0,75 * 25±1,5 107±20 * 17,4±2,4 * 17,0±3,1 * 76,6±3,2 group 2 (single α-globin gene deletion) 4,70±0,85 25,2±1,5 118±22 16,2±2,9 * 15,1±2,1 76,9±3,5 group 3 (double α-globin gene deletion) 5,20±0,57 23,2±1,3 * 120±9 14,1±2,1 * 14,8±2,8 72,4±3,0 *


1981 ◽  
Vol 59 (9) ◽  
pp. 1553-1577 ◽  
Author(s):  
Ernest Small

Numerical taxonomic analyses (particularly agglomerative clustering and ordination) were conducted on 55 species of Medicago, using 75 mostly vegetative and fruiting characters. The material studied represents all conservatively accepted species of the genus, as well as 14 "problematical" species of which many are often considered to belong to the genus Trigonella, rather than to Medicago. Although the characters employed are substantially the same as those used by recent monographers who evaluated the genus by traditional subjective procedures, the present numerical examination suggests many relationships not previously appreciated.As a result of the analyses, it was judged appropriate to recognize 12 groupings. These are group 1: M. sativa (alfalfa) and 11 allied species; group 2: M. lupulina and M. secundiflora; group 3: eight problematical species which have troubled taxonomists with respect to whether they should be placed in Medicago or Trigonella; groups 4–8: each made up of a single divergent species, respectively: M. carstiensis, M. radiata, M. orbicularis, M. heyniana, and M. arborea; groups 9–12 four subgroupings of a larger group of 28 annual species. In the main, the composition of the seven polytypic groups is similar to those of taxa accepted by recent monographers, although some realignments of particular species are suggested by the present study. Groups 1 and 2 are much more similar to each other than indicated in recent treatments. Medicago arborea was discovered to be much more dissimilar to all other species examined than thought previously. Medicago hybrida of group 1 was found to be a "master link" between species traditionally placed in Medicago, and many placed in Trigonella (group 3).The 12 groupings in turn fall into three assemblages that could be recognized as subgenera, or even as genera. These are A: groups 1, 2, 9, 10, 11, and 12; B: groups 3–7, inclusive; and C: M. arborea. Further research is suggested before formal categorization is undertaken.


2004 ◽  
Vol 136 (3) ◽  
pp. 323-405 ◽  
Author(s):  
Matthew J. Yoder

AbstractThe species of the genus Entomacis Foerster in North America north of Mexico are revised. Nineteen species (12 new), including 8 species of the Holarctic-wide perplexa species group, are keyed, described, and figured. These taxa are E. ambigua (Brues), E. apopkaensissp. nov., E. arcticasp. nov., E. cellariasp. nov., E. cepasp. nov., E. eorariasp. nov., E. floridana (Ashmead), E. grandiclavasp. nov., E. longii (Ashmead), E. mellipetiola (Ashmead), E. parambiguasp. nov., and perplexa group members E. californica (Ashmead), E. microbipunctatasp. nov., E. notioxerasp. nov., E. oulasp. nov., E. parvasp. nov., E. perplexa (Haliday), E. sapratasp. nov., and E. subemarginata (Ashmead). Hemilexodes canadensis (Harrington) is synonymized under Entomacis mellipetiola (Ashmead) (syn. nov.). The status of Entomacis latipennis (Ashmead), E. filiformis (Ashmead), and Hemilexis jessei Mann is reviewed. New character complexes, particularly chaetotaxy, are emphasized for Diapriidae species taxonomy.


2021 ◽  
Vol 36 (Supplement_1) ◽  
Author(s):  
T Shimura ◽  
K Yumoto ◽  
M Sugishima ◽  
Y Mio

Abstract Study question Why do some direct-cleaved human zygotes still lead to a live birth? Summary answer Direct-cleaved zygotes which have undergone the 2-cell stage can lead to a live birth, while zygotes cleaved from 1-cell to ≥ 3-cell do not. What is known already In recent years, zygotes that develop from 2-cell to 3-cell within 5 hours after the first cleavage have been evaluated as “direct-cleaved” zygotes, because normal cleavage takes approximately 12 hours to complete. It was reported that their implantation rate was significantly lower than zygotes with normal cleavage pattern, and eliminating direct-cleaved zygotes from transfer could improve the implantation rate. However, some direct-cleaved zygotes at the first cleavage could still lead to a live birth. Few reports have examined the difference between a cleavage from 1-cell to ≥ 3-cell and 2-cell to ≥ 3-cell within 5 hours after the first cleavage. Study design, size, duration A retrospective study involving 2,077 cycles of IVF/ICSI between July 2012 and July 2019. A total of 5,991 normally fertilized zygotes (2PN/2PB) were included. Of those, 3,508 were evaluated as usable good/fair quality embryos on Day2/3, and the rest (n = 2,483) were evaluated as poor quality and rejected from transfer or cryopreservation after 7 days of culture. Of 3,508 usable embryos, 884 were selected based on the availability of results of live birth for this study. Participants/materials, setting, methods Time-lapse imaging (5 slices along Z-axis every 10 minutes) was performed in EmbryoScopeTM. Zygotes were morphokinetically analyzed in detail and classified into four groups by their cleavage patterns: Group1 (1-cell→2-cell); Group 2 (1-cell→3-cell); Group 3 (1-cell→2-cell→≥3-cell within 5 hours after the first cleavage); and Group 4 (1-cell→2-cell→≥5-cell). The proportion, mean maternal age and live birth rate of each group were examined. Main results and the role of chance The proportion of Groups 1-4 was 83.6% (n = 739), 3.8% (n = 34), 5.9% (n = 52), and 6.7% (n = 59), respectively. 0f 884 zygotes examined in this study, the mean maternal age was significantly higher in Group 2 and 4 than in Group 1 (P &lt; 0.05; 37.4±4.9 in Group1, 39.1±5.2 in Group 2, 38.6±6.0 in Group 3, and 38.7±5.1 in Group 4). The rate of confirmed gestational sac was significantly lower in Group 2 and 4 than in Group 1 [P &lt; 0.01; 36.3% (n = 268/739), 0% (n = 0/34), 25.0% (n = 13/52), and 18.6% (n = 11/59) in Groups 1-4, respectively]. Furthermore, the live birth rate was significantly higher in Group 1 than in Groups 2, 3 and 4 [P &lt; 0.01; 28.4% (n = 210/739), 0% (n = 0/34), 13.5% (n = 7/52), and 15.3% (n = 9/59) in Groups 1-4, respectively]. Above all, while zygotes in Group 2 showed no pregnancy and live birth at all, zygotes in Group 3 showed a live birth rate of 13.5%. However, they had a significantly higher miscarriage rate (42.9%, n = 6) compared to zygotes in Group 1 (19.5%, n = 55). Limitations, reasons for caution It is very difficult to capture cleavage patterns by routine observations because the timings of developmental events are different between embryos. A time-lapse imaging and culturing system is essential to solve this problem, however, it cannot visualize the distribution of chromosomes, and no chromosomal analysis was conducted in this study. Wider implications of the findings This study revealed that zygotes previously classified as “direct-cleaved” and eliminated from transfer included viable zygotes which could lead to a live birth. Therefore, it is crucial to optimize the use of time-lapse imaging of human zygotes in order to precisely evaluate the first cleavage. Trial registration number not applicable


2019 ◽  
Vol 73 (4) ◽  
pp. 773
Author(s):  
Wayne E. Clark† ◽  
Horace R. Burke† ◽  
Robert W. Jones ◽  
Robert S. Anderson

Geosphere ◽  
2021 ◽  
Author(s):  
Ann E. H. Hanson ◽  
Stacia M. Gordon ◽  
Kyle T. Ashley ◽  
Robert B. Miller ◽  
Elizabeth Langdon-Lassagne

The rheology and composition of arc crust and the overall evolution of continental magmatic arcs can be affected by sediment incorporation events. The exhumed Cretaceous–Eocene North Cascades arc exposes abundant metasedimentary rocks that were incorporated into the arc during multiple events. This study uses field relationships, detrital zircon geochronology, bulk rock geochemistry, geothermometry, and quartz­in­garnet geobarometry to distinguish approximate contacts and emplacement depths for different metasedimentary units to better understand their protolith incorporation history and impact on the arc. The Skagit Gneiss Complex is one of the main deep crustal units of the North Cascades arc. It includes metasedimentary rocks with distinct detrital zircon signatures: Proterozoic–Cretaceous (Group 1) or Triassic–Cretaceous (Group 2) zircon populations. Both metasedimentary groups achieved near­ peak metamorphic conditions of 640–800 °C and 5.5–7.9 kbar; several Group 2 samples reveal the higher pressures. A third group of metasedimentary rocks, which was previously interpreted as metamorphosed equivalents of backarc sediments (Group 3), exhibited unimodal Triassic or bimodal Late Jurassic–Early Cretaceous detrital zircon signatures and achieved near­peak conditions of 570–700 °C and 8.7–10.5 kbar. The combined field and analytical data indicate that protoliths of Group 1 and Group 2 metasedimentary rocks were successively deposited in a forearc basin and underthrusted into the arc as a relatively coherent body. Group 3 backarc sediments were incorporated into the arc along a transpressional step­over zone. The incorporation of both forearc and backarc sediments was likely facilitated by arc magmatism that weakened arc crust in combination with regional transpression.


We review the fossil microtine rodent assemblages from the Lower Pleistocene deposits in eastern England, consisting mainly of marine sediments of the Norwich Crag and Cromer Forest-bed Formations. Material from 17 localities, including the ‘Weybourne Crag’ of the Norfolk Coast, the inland ‘Norwich Crag’, and the Crag of the north Suffolk coast has been studied. The taxa Mimomys pliocaenicus, M.rex, M.blanci, M.newtoni, M.pitymyoides, M .altenburgensis and Clethrionomys are recognized. Mimomys pitymyoides and M.altenburgensis are described for the first time from Britain. The type material of Mimomys reidi and M.newtoni is redescribed, and we show that M.newtoni Major 1902 is a senior synonym of M.hungaricus (Kormos), thus resolving confusion that has existed in the literature. The prior name for the species described by M. A. C. Hinton ( Monograph of the voles and lemmings (Microtnae) living and extinct . London: British Museum (Natural History) 1926) as Mimomys newtoni appears to be Mimomys blanci van der Meulen 1973. No evidence has been found for mixing of faunas of different age at a single horizon or locality. Differences in crown height are demonstrated between samples of Mimomys pliocaenicus from different localities, and differences between localities in the presence and absence of various species are tabulated. This evidence combined with current interpretations of the stratigraphy leads us to recognize three faunal groups. Group 1 faunas contain Mimomys pliocaenicus, M.reidi (type level), M.newtoni (type level), M.pitymyoides, M.blanci and Clethrionomys . They come from coastal deposits previously termed ‘Weybourne Crag’ and currently considered to date from Pre-Pastonian a to Pastonian. The faunas are clearly later than group 2 faunas, which contain Mimomys pliocaenicus, M.reidi, M.newtoni (these three species less advanced than in group 1 faunas), M.rex and M.altenburgensis (these two species lacking in group 1 faunas). Group 2 faunas come from inland ‘Norwich Crag’ localities and crags in Suffolk yielding a Chillesford type pollen assemblage, which are currently considered to date from the Bramertonian stage. Group 3 faunas contain Mimomys pliocaenicus, M.reidi and M.blanci and are from coastal deposits at Covehithe and Easton Bavents associated with Baventian stage clays. The evidence from the microtine rodents confirms the relative position of the Bramertonian and Pre-Pastonian a stages, but does not yet allow conclusions to be drawn on the relative age of group 3 faunas or the deposits in which they occur. The fauna of the Pastonian stage still requires clarification, since it is not possible to allocate unambiguously to this stage any of the material described here. The British Lower Pleistocene assemblages are broadly similar to material from Tegelen, The Netherlands (Tiglian TC4-6) and to material from superimposed loess levels at Stranzendorf, Austria. The British assemblages are characterized by the presence of Mimomys pliocaenicus and the absence of species with unrooted teeth, indicating that they belong to the Mimomys superzone of the biostratigraphic system of A. J. van der Meulen ( Quaternaria 17, 1-144, 1973) corresponding to the Villanyian stage. On the basis of microtine evidence we suggest limits to the correlation of the Pre-Pastonian and Bramertonian stages with the Netherlands chronostratigraphy. These limits are earlier than suggested by other lines of evidence. Correlation of the Pre-Pastonian with part of the Eburonian and the Bramertonian with part of the Tiglian is thought to merit consideration.


2019 ◽  
Author(s):  
ahmet camtosun ◽  
Ibrahim Topcu

Abstract Background: We investigated the association of the blood parameters such as neutrophil, platelet accounts and neutrophil/lymphocyte ratio (NLR) with tumor type, tumor size and Fuhrman grade in nonmetastatic renal cell carcinoma (RCC) cases. Methods: A total of 343 patients with nonmetastatic (T1- 4N0M0) RCC were included into the study. The patients were divided into four groups: clear cell (group-1), papillary (group-2), chromophobes (group-3) and other pathologies (group-4). In each grouping systems, the NLR, white blood cell (WBC), platelet (PLT), mean corpuscular hemoglobin (MCH), and mean corpuscular volume (MCV) values were compared. Results: There were 222 patients with clear cell (group-1), 62 papillary (group-2), 16 chromophobes (group-3) and 43 patients with other pathologies (group-4). There was a significant difference between the groups in group-1 and group-3 in terms of white blood cell (WBC), platelet (PLT), lymphocyte and neutrophil count. However, there was no significant difference between the groups by the surveys in terms of Neutrophil / Lymphocyte Ratio (NLR) values. There was no significantly difference between survival and NLR either. Conclusion: NLR is a cheap and easy parameter to calculate but is not suitable to predict tumor prognosis and survival yet. NLR cut-off value is the biggest problem for now. But evidences show, we are too close to overcome this problem.


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