cometadata/datacite-rtg-text-other-reclassification-records huggingface dataset:
Amauronyx occidens Assing & Brachat & Meybohm 2019, spec. nov.
Creators: name: Assing, Volker
name: Brachat, Volker
name: Meybohm, Heinrich
Publisher: name: Zenodo
Year: 2019
Subjects: Biodiversity
Taxonomy
Animalia
Arthropoda
Insecta
Coleoptera
Staphylinidae
Amauronyx
Amauronyx occidens

description: Amauronyx occidens BRACHAT spec. nov.
urn:lsid:zoobank.org:act: 0545A123-B114-4014-A05D-2C5EF565D5D9
(Fig. 157)
Type material: Holotype ♂: “GR – Crete [7], NW Kandanos, Strovles, 35°22'03"N, 23°40'07"E, 410 m, stream valley, 23.XII.2018, V. Assing / Amauronyx occidens spec. nov. ♂, det. Brachat 2.2019 / Holotypus” (cBra). Paratypes (all in cBra): 1 ♀: same data as holotype; 1 ♂, 2 ♀♀: “GR – Crete [6], S Kissamos, Elos, 35°21'33"N, 23°38'17"E, 560 m, old chestnut, soil washing, 23.XII.2018, V. Assing ”.
Etymology: The specific epithet (Latin, adjective: western) alludes to the fact that this is the westernmost representative of the genus in Crete.
Description: External characters as in A. chanianus, except as follows:
Pubescence suberect. Head 0.34 mm long and 0.41 mm broad; antennal tubercles laterally with sharp lamella; frons with two intraocular foveae situated behind level of eyes, medially with convex elevation and with small median impression. Eyes composed of 4–7 ommatidia, situated behind middle of head. Antenna compact, 0.70 mm long; antennomeres I, II, and IX oblong, IV–VIII weakly transverse, and XI in the middle with transverse notch furnished with a series of depressed setae. Pronotum 0.38–0.39 mm long and 0.41–0.42 mm broad, of cordiform shape, with a pronounced median sulcus nearly reaching pronotal anterior margin. Elytra 1.25 times as long and 1.4 times as broad as pronotum, with deep discal sulcus.
♂: protrochanter ventrally with fine and short carina in the middle; mesotrochanter with a flat and apically obtuse tooth; metatrochanter with a long and narrow carina; aedeagus (Fig. 157) 0.28 mm long; internal sac with a broad, flat, and sinuous sclerite and with a long sinuous structure; parameres apically with three setae.
Comparative notes: Like the other Cretan representatives of the genus, A. occidens is reliably identified only based on the modifications of the male trochanters and on the internal structures of the aedeagus.
Distribution and natural history: This species is probably locally endemic to the extreme west of Crete. The specimens were found in two localities by washing soil from a moist stony slope with very old chestnut and from a stream valley with old chestnut at altitudes of 410 and 560 m.
description: Published as part of Assing, Volker, Brachat, Volker & Meybohm, Heinrich, 2019, Monograph of the Staphylinidae of Crete (Greece). Part II. Descriptions of new species (Insecta: Coleoptera), pp. 239-289 in Beiträge Zur Entomologie = Contributions to Entomology 69 (2) on pages 281-282, DOI: 10.21248/contrib.entomol.69.2.239-289, http://zenodo.org/record/4755240
Eozapus setchuanus
Creators: name: Wilson, Don E.
name: Reeder, DeeAnn
Publisher: name: The Johns Hopkins University Press
Year: 2005
Subjects: Biodiversity
Taxonomy
Animalia
Chordata
Mammalia
Rodentia
Dipodidae
Eozapus
Eozapus setchuanus

description: Eozapus setchuanus (Pousargues 1896)
[Zapus] setchuanus Pousargues 1896, Bull. Mus. Hist. Nat. Paris, 2: 13.
Type Locality: China, Sichuan Prov., Tatsienlu (Kangding).
Vernacular Names: Chinese Jumping Mouse.
Synonyms: Eozapus vicinus (Thomas 1912).
Distribution: China: Qinghai, Gansu, Ningxia, Shaanxi, Sichuan, and NW Yunnan; 3000-4000 m (Qin, 1991; Wang, 1990, 2003; Zhang and Wang, 1963; Zheng and Zhang, 1990; Zhang et al., 1997, provided distribution map).
Conservation: IUCN – Vulnerable.
Discussion: Martin (1994:5) wrote "Although distinctly more hypsodont and with lophs and lophids connecting the primary molar cusps, Eozapus retains the generalized, underived zapodid pattern of Plesiosminthus." The latter is the oldest known scistine found in late Oligocene and Miocene sediments in both Europe and North America. Reviewed by Corbet (1978 c) and Corbet and Hill (1992).
description: Published as part of Wilson, Don E. & Reeder, DeeAnn, 2005, Order Rodentia - Family Dipodidae, pp. 871-893 in Mammal Species of the World: a Taxonomic and Geographic Reference (3 rd Edition), Volume 2, Baltimore :The Johns Hopkins University Press on page 891, DOI: 10.5281/zenodo.7316535
title: Geologic map of southern Quitman Mountains and vicinity, Hudspeth County, Texas
title: Geology of southern Quitman Mountains, Hudspeth County, Texas
titleType: AlternativeTitle
Creators: name: Jones, Bill R.
Publisher: name: University of Texas at Austin. Bureau of Economic Geology
Year: 1970
Subjects: subject: Geology -- Quitman Mountains -- Maps
subject: Geology -- Texas -- Hudspeth County -- Maps

description: To obtain a print version of this publication visit: https://store.beg.utexas.edu/ and search for: GQ0039. Accompanied by 1 fold-out map : Geologic Map of Southern Quitman Mountains and Vicinity, Hudspeth County, Texas
description: The Quitman Mountains are part of a narrow mountain range that extends southeastward from near Sierra Blanca, Texas (85 miles southeast of El Paso, Texas), into northern Mexico. The range is typical of many desert mountains of the southwestern United States in that it projects abruptly above the breached bolsons that border it. Thus, the Quitman Mountains stand in stark contrast topographically and geologically to the Hueco Bolson on the west and the Red Light Bolson on the east. Quitman Gap (also called Quitman Canyon, Quitman Pass, and Can de los Lamentos) divides the range into northern and southern parts. The northern Quitmans, composed of Tertiary intrusive and volcanic rocks with intensely folded Cretaceous rocks exposed around the periphery of the igneous mass, extend about 10 miles north-northwest from Quitman Gap to Interstate Highway 10. The southern Quitman Mountains, composed primarily of intensely folded and thrust-faulted Cretaceous rocks, extend from Quitman Gap south-southeast to the Rio Grande (a distance of about 25 miles). The elevation of the range gradually diminishes southward from about 6,600 feet above sea level in the northern part to slightly less than 4,000 feet above sea level near the Rio Grande. The maximum local difference in elevation is about 2,000 feet. The highlands of the area studied are horsts flanked by grabens that are partly filled with sediment eroded from the mountains to form intermontane basins. The block faulting that created the horst and graben system followed the igneous activity and was superimposed on the earlier Laramide folds, thrust faults, and strike-slip faults characteristic of the Chihuahua tectonic belt. The Cretaceous rocks exposed in the southern Quitman Mountains consist of about 14,000 feet of marine shale, sandstone, and limestone, and nonmarine sandstone and shale. The lower 3,000 to 4,000 feet of the sequence are nonmarine rocks. Volcanic rocks overlie truncated folds in the Cretaceous sequence and consist mostly of tuffs, welded tuffs, and andesite. The bolsons are filled by relatively undisturbed Tertiary and Quaternary sediments that were deposited as interbedded conglomerates and fine-grained lacustrine-playa deposits.
title: Gravity, magnetic, and generalized geologic map of the Van Horn -- Sierra Blanca Region, Trans-Pecos Texas
title: Van Horn -- Sierra Blanca region, Trans-Pecos Texas
titleType: AlternativeTitle
Creators: name: Wiley, Michael Alan, 1935-
Publisher: name: University of Texas at Austin. Bureau of Economic Geology
Year: 1972
Subjects: subject: Geology -- Texas -- Culberson County -- Maps
subject: Geology -- Texas -- Hudspeth County -- Maps

description: To obtain a print version of this publication visit: https://store.beg.utexas.edu/ and search for: GQ0040. Accompanied by 1 fold-out map : Gravity, Magnetic and Generalized Geologic Map of the Van Horn-Sierra Blanca Region, Trans-Pecos Texas
description: The Van Horn-Sierra Blanca region lies athwart part of the boundary between two contrasting geologic provinces. The contrast between these two provinces, splendidly displayed by Holocene landforms in the present map area, has a history that dates back to at least Late Precambrian time. This remarkable contrast led R. T. Hill (1902) to suggest the possibility of a transcontinental fracture zone passing near Van Horn and along the boundary of the provinces. Later workers called Hill's frac ture zone the Texas lineament (Ransome, 1915) or the Texas direction of wrench faulting (Moody and Hill, 1956). Where it is exposed in the region, the Rim Rock fault (fig. 1) seems to form part of the boundary between the provinces. Numerous workers have suggested a long-enduring history of strike-slip movement along the Hillside fault (fig. 1). The Van Horn-Sierra Blanca region has been mapped in detail geologically, but because nearly half of the total area of the region is covered by late Cenozoic basin-fill and because subsurface control is sparse, it has not been possible to understand the region in detail in three dimensions. This report summarizes the methods and results of a ground magnetometer and gravimeter survey undertaken in an attempt to obtain a clearer understanding of the tectonic history of the region and of the structural significance of the Hillside and Rim Rock faults.
Additional file 3: Figure S2. of The carotenoid biosynthetic and catabolic genes in wheat and their association with yellow pigments
Creators: name: Colasuonno, Pasqualina
name: Lozito, Maria
name: Marcotuli, Ilaria
name: Nigro, Domenica
name: Giancaspro, Angelica
name: Mangini, Giacomo
name: Vita, Pasquale De
name: Mastrangelo, Anna
name: Pecchioni, Nicola
name: Houston, Kelly
name: Simeone, Rosanna
name: Gadaleta, Agata
name: Blanco, Antonio
Publisher: name: Figshare
Year: 2017
Subjects: subject: Biochemistry
subject: Medicine
subject: Microbiology
subject: FOS: Biological sciences
subject: Cell Biology
subject: Genetics
subject: Molecular Biology
subject: Ecology
subject: Immunology
subject: FOS: Clinical medicine
subject: Developmental Biology
subject: Cancer
subject: Infectious Diseases
subject: FOS: Health sciences
subject: Plant Biology
subject: Virology
subject: Computational Biology

description: Frequency distributions of yellow index and yellow pigment content. (DOCX 28 kb)
Amauronyx askifouicus Assing & Brachat & Meybohm 2019, spec. nov.
Creators: name: Assing, Volker
name: Brachat, Volker
name: Meybohm, Heinrich
Publisher: name: Zenodo
Year: 2019
Subjects: Biodiversity
Taxonomy
Animalia
Arthropoda
Insecta
Coleoptera
Staphylinidae
Amauronyx
Amauronyx askifouicus

description: Amauronyx askifouicus BRACHAT spec. nov.
urn:lsid:zoobank.org:act: 7CE4D2AD-8F1E-408A-9112-5301AC6CC6AE
(Fig.158)
Type material: Holotype ♂: “GR – Crete [41], Askifou → Asigonia, 35°14'14"N, 24°14'11"E, 740 m, soil washing, 23.III.2018, V. Assing / Amauronyx askifouicus spec. nov. ♂, det. Brachat 2.2019 / Holotypus” (cBra). Paratypes: 1 ♂, 3 ♀♀: same data as holotype (cBra).
Etymology: The specific epithet is an adjective derived from the name of the plateau where the type locality is situated.
Description: External characters as in A. occidens; distinguished only by the male sexual characters:
♂: pro- and mesotrochanter with fine, metatrochanter with short oblong carina; aedeagus 0.30 mm long; internal sac with a broad, flat, and laterally triangular sclerite and with a long and slender angled structure; parameres apically with four setae.
Comparative notes: Amauronyx askifouicus is distinguished from other Cretan representatives of the genus by the distinctive modifications of the male trochanters and by the internal structures of the aedeagus.
Distribution and natural history: This species is probably locally endemic to the environs of the type locality in West Crete. The specimens were found by washing soil from a rocky north slope with old Quercus ilex at an altitude of 740 m.
description: Published as part of Assing, Volker, Brachat, Volker & Meybohm, Heinrich, 2019, Monograph of the Staphylinidae of Crete (Greece). Part II. Descriptions of new species (Insecta: Coleoptera), pp. 239-289 in Beiträge Zur Entomologie = Contributions to Entomology 69 (2) on page 282, DOI: 10.21248/contrib.entomol.69.2.239-289, http://zenodo.org/record/4755240
Hydractinia rugosa Fraser 1938
Creators: name: OLIVEIRA, OTTO M. P.
name: MIRANDA, THAÍS P.
name: ARAUJO, ENILMA M.
name: AYÓN, PATRICIA
name: CEDEÑO-POSSO, CRISTINA M.
name: CEPEDA-MERCADO, AMANCAY A.
name: CÓRDOVA, PABLO
name: CUNHA, AMANDA F.
name: GENZANO, GABRIEL N.
name: HADDAD, MARIA ANGÉLICA
name: MIANZAN, HERMES W.
name: MIGOTTO, ALVARO E.
name: MIRANDA, LUCÍLIA S.
name: MORANDINI, ANDRÉ C.
name: NAGATA, RENATO M.
name: NASCIMENTO, KARINE B.
name: JÚNIOR, MIODELI NOGUEIRA
name: PALMA, SERGIO
name: QUIÑONES, JAVIER
name: RODRIGUEZ, CAROLINA S.
name: SCARABINO, FABRIZIO
name: SCHIARITI, AGUSTÍN
name: STAMPAR, SÉRGIO N.
name: TRONOLONE, VALQUÍRIA B.
name: MARQUES, ANTONIO C.
Publisher: name: Zenodo
Year: 2016
Subjects: Biodiversity
Taxonomy
Animalia
Cnidaria
Hydrozoa
Anthoathecata
Hydractiniidae
Hydractinia
Hydractinia rugosa

description: Hydractinia rugosa Fraser, 1938b
Distribution in South America: polyp—Pacific Ocean, Colombia, at 6.78°N 77.60°W in Octavia Bay (Fraser 1938b, 1948).
Habitat: polyp—from 64 to 73m depth (Fraser 1938b).
description: Published as part of OLIVEIRA, OTTO M. P., MIRANDA, THAÍS P., ARAUJO, ENILMA M., AYÓN, PATRICIA, CEDEÑO-POSSO, CRISTINA M., CEPEDA-MERCADO, AMANCAY A., CÓRDOVA, PABLO, CUNHA, AMANDA F., GENZANO, GABRIEL N., HADDAD, MARIA ANGÉLICA, MIANZAN, HERMES W., MIGOTTO, ALVARO E., MIRANDA, LUCÍLIA S., MORANDINI, ANDRÉ C., NAGATA, RENATO M., NASCIMENTO, KARINE B., JÚNIOR, MIODELI NOGUEIRA, PALMA, SERGIO, QUIÑONES, JAVIER, RODRIGUEZ, CAROLINA S., SCARABINO, FABRIZIO, SCHIARITI, AGUSTÍN, STAMPAR, SÉRGIO N., TRONOLONE, VALQUÍRIA B. & MARQUES, ANTONIO C., 2016, Census of Cnidaria (Medusozoa) and Ctenophora from South American marine waters, pp. 1-256 in Zootaxa 4194 (1) on page 63, DOI: 10.11646/zootaxa.4194.1.1, http://zenodo.org/record/10068449
Additional file 1. of Overweight and obesity in children aged 3–13 years in urban Cameroon: a cross-sectional study of prevalence and association with socio-economic status
Creators: name: Simeon-Pierre Choukem
name: Kamdeu-Chedeu, Josiane
name: Leary, Sam
name: Mboue-Djieka, Yannick
name: Nebongo, Daniel
name: Akazong, Christoph
name: Yacouba Mapoure
name: Hamilton-Shield, Julian
name: Jean-François Gautier
name: Mbanya, Jean
Publisher: name: Figshare
Year: 2017
Subjects: subject: Medicine
subject: Sociology
subject: FOS: Sociology
subject: Developmental Biology
subject: Science Policy
subject: 60506 Virology
subject: FOS: Biological sciences
subject: Computational Biology

description: Summary of all categorical variables; whole cohort and separately for HSES and LSES. HSES = High socioeconomic status; LSES = Low socioeconomic status; IQR = inter-quartile range; *p-value from chi-squared tests, HSES vs.LSES; †of those who receive pocket money, median (IQR) = 150 (100, 200) FCFA. (DOCX 16 kb)
Napaeozapus Preble 1899
Creators: name: Wilson, Don E.
name: Reeder, DeeAnn
Publisher: name: The Johns Hopkins University Press
Year: 2005
Subjects: Biodiversity
Taxonomy
Animalia
Chordata
Mammalia
Rodentia
Dipodidae
Napaeozapus

description: Napaeozapus Preble 1899
Napaeozapus Preble 1899, N. Amer. Fauna, 15: 33.
Type Species: Zapus insignis Miller 1891
Species and subspecies: 1 species:
Species Napaeozapus insignis (Miller 1891)
Discussion: For verification of the absence of cheek pouches in Napaeozapus see Klingener (1971). Documented in fossil record from the middle Pleistocene (R. A. Martin, 1994; McKenna and Bell, 1997).
description: Published as part of Wilson, Don E. & Reeder, DeeAnn, 2005, Order Rodentia - Family Dipodidae, pp. 871-893 in Mammal Species of the World: a Taxonomic and Geographic Reference (3 rd Edition), Volume 2, Baltimore :The Johns Hopkins University Press on page 891, DOI: 10.5281/zenodo.7316535
title: Geologic map of the Squaw Creek Quadrangle, Gillespie and Mason Counties, Texas
title: Squaw Creek Quadrangle, Gillespie and Mason Counties, Texas
titleType: AlternativeTitle
title: Geology of the Squaw Creek Quadrangle, Gillespie and Mason Counties, Texas
titleType: AlternativeTitle
Creators: name: Barnes, Virgil E. (Virgil Everett), 1903-1998
Publisher: name: University of Texas at Austin. Bureau of Economic Geology
Year: 1952
Subjects: subject: Geology -- Texas -- Gillespie County -- Maps
subject: Geology -- Texas -- Mason County -- Maps

description: To obtain a print version of this publication visit: https://store.beg.utexas.edu/ and search for: GQ0001. Accompanied by 1 fold-out plate, with text : Geologic Map of Squaw Creek Quadrangle, Gillespie and Mason Counties, Texas
description: The Squaw Creek quadrangle is partly within the Llano region and partly within the Edwards Plateau province. The Edwards Plateau is continuous along the southern border of the quadrangle, but erosion has dissected it until long fingers extend northward, the most important being between Mormon and Squaw Creeks and east of Squaw Creek. The geology of the Squaw Creek quadrangle is shown on a planimetric map, and the only topographic map available is the reconnaissance 30-minute Kerrville quadrangle. Elevations ranging between 1,721 and 2,207 feet were determined during traversing for control, but neither the highest nor the lowest elevation was reached. However, it is estimated that the relief within the quadrangle is about 620 feet, ranging between about 1,600 and 2,220 feet in elevation. The quadrangle is almost entirely within the Llano River drainage basin and is drained by Squaw Creek and Threadgill Creek and its tributaries Mormon and Dry Mormon Creeks. The water reaches Llano River by way of Beaver Creek. A small area in the northeastern corner of the quadrangle is drained by Pecan Spring Branch and reaches Llano River through Marshall Creek and Hickory Creek. An extremely small area in the southeastern corner of the quadrangle drains into Pecan Creek and reaches Pedernales River by way of Live Oak Creek. Squaw Creek quadrangle is high on the southern side of the Llano uplift, and rocks of Cambrian and Ordovician age outcrop in the northern part of the quadrangle. Faults in these rocks are related to the Ouachita orogeny. The Cretaceous rocks are essentially horizontal, dipping northward perhaps a few feet per mile. A small fault in the Cretaceous is exposed in a road cut 3 miles east of Doss. Broader discussions of the stratigraphic, structural, economic, and geophysical problems of the region cannot be given in the space available. References cited below deal with some of these problems. This publication on the Squaw Creek quadrangle is one of a series of similar publications, an index to which is shown on the opposite page. The reader is referred to this index map to locate other quadrangles mentioned in the present text.
title: Geologic map of the Palo Alto Creek Quadrangle, Gillespie County, Texas
title: Geology of the Palo Alto Creek Quadrangle, Gillespie County, Texas
titleType: AlternativeTitle
title: Palo Alto Creek Quadrangle, Gillespie County, Texas
titleType: AlternativeTitle
Creators: name: Barnes, Virgil E. (Virgil Everett), 1903-1998
Publisher: name: University of Texas at Austin. Bureau of Economic Geology
Year: 1952
Subjects: subject: Geology -- Texas -- Gillespie County -- Maps

description: To obtain a print version of this publication visit: https://store.beg.utexas.edu/ and search for: GQ0008. Accompanied by 1 fold-out map, with text : Geologic Map of the Palo Alto Creek Quadrangle, Gillespie County, Texas
description: Palo Alto Creek quadrangle is south of the Llano region and is in the marginal portion of the Edwards Plateau where much of the plateau surface has been destroyed by erosion. Along the northern edge of the quadrangle, a portion of a finger of the plateau trends eastward, and in the west-central part, another finger of the plateau frays out into a number of isolated outliers. The rest of the quadrangle is a portion of the gently undulating broad Pedernales River basin. The geology of the Palo Alto Creek quadrangle is shown on a planimetric map, and the only topographic map available is the reconnaissance 30-minute Fredericksburg quadrangle. Elevations ranging between 1,556 and 1,975 feet were determined during traversing for control, but neither the highest nor the lowest elevation was reached. However, it is estimated that the relief within the quadrangle is about 550 feet, ranging between about 1,525 and 2,075 feet in elevation. The quadrangle is entirely within the Pedernales River drainage basin and is mostly drained by Palo Alto Creek and its tributaries. Barons Creek drains the southwestern corner of the quadrangle, and Willow Creek and the tributaries of North Grape Creek drain a small area in the northeastern corner. The Palo Alto Creek quadrangle is high on the southern side of the Llano uplift, and rocks from pre-Cambrian to Ordovician in age outcrop as inliers surrounded by Cretaceous rocks. The faulting accompanying the Ouachita orogeny (Barnes, 1948) is not exposed, but dips in Paleozoic rocks up to 9 are present. The Cretaceous rocks are essentially horizontal, dipping eastward about 8 feet per mile. Broader discussions of the stratigraphic, structural, economic, and geophysical problems of the region cannot be given in the space available. References cited below deal with some of these problems. This publication on the Palo Alto Creek quadrangle is one of a series of similar publications, an index to which is shown on the opposite page. The reader is referred to this index map to locate other quadrangles mentioned in the present text.
Podocoryna apicata Kramp 1959
Creators: name: OLIVEIRA, OTTO M. P.
name: MIRANDA, THAÍS P.
name: ARAUJO, ENILMA M.
name: AYÓN, PATRICIA
name: CEDEÑO-POSSO, CRISTINA M.
name: CEPEDA-MERCADO, AMANCAY A.
name: CÓRDOVA, PABLO
name: CUNHA, AMANDA F.
name: GENZANO, GABRIEL N.
name: HADDAD, MARIA ANGÉLICA
name: MIANZAN, HERMES W.
name: MIGOTTO, ALVARO E.
name: MIRANDA, LUCÍLIA S.
name: MORANDINI, ANDRÉ C.
name: NAGATA, RENATO M.
name: NASCIMENTO, KARINE B.
name: JÚNIOR, MIODELI NOGUEIRA
name: PALMA, SERGIO
name: QUIÑONES, JAVIER
name: RODRIGUEZ, CAROLINA S.
name: SCARABINO, FABRIZIO
name: SCHIARITI, AGUSTÍN
name: STAMPAR, SÉRGIO N.
name: TRONOLONE, VALQUÍRIA B.
name: MARQUES, ANTONIO C.
Publisher: name: Zenodo
Year: 2016
Subjects: Biodiversity
Taxonomy
Animalia
Cnidaria
Hydrozoa
Anthoathecata
Hydractiniidae
Podocoryna
Podocoryna apicata

description: Podocoryna apicata Kramp, 1959b
Synonyms in the area: Podocoryne apicata —Segura-Puertas 1984 [medusa]. Distribution in South America: medusa—Pacific Ocean, Ecuador, at northwest and southeast of Galápagos Archipelago (Segura-Puertas 1984).
Podocoryna areolata (Alder, 1862)
Synonyms in the area: Hydractinia areolata — Guerrero et al. 2013 [medusa]. Distribution in South America: medusa—Atlantic Ocean, Argentina, from 40°S to 42.25°S (Guerrero et al. 2013).
description: Published as part of OLIVEIRA, OTTO M. P., MIRANDA, THAÍS P., ARAUJO, ENILMA M., AYÓN, PATRICIA, CEDEÑO-POSSO, CRISTINA M., CEPEDA-MERCADO, AMANCAY A., CÓRDOVA, PABLO, CUNHA, AMANDA F., GENZANO, GABRIEL N., HADDAD, MARIA ANGÉLICA, MIANZAN, HERMES W., MIGOTTO, ALVARO E., MIRANDA, LUCÍLIA S., MORANDINI, ANDRÉ C., NAGATA, RENATO M., NASCIMENTO, KARINE B., JÚNIOR, MIODELI NOGUEIRA, PALMA, SERGIO, QUIÑONES, JAVIER, RODRIGUEZ, CAROLINA S., SCARABINO, FABRIZIO, SCHIARITI, AGUSTÍN, STAMPAR, SÉRGIO N., TRONOLONE, VALQUÍRIA B. & MARQUES, ANTONIO C., 2016, Census of Cnidaria (Medusozoa) and Ctenophora from South American marine waters, pp. 1-256 in Zootaxa 4194 (1) on page 63, DOI: 10.11646/zootaxa.4194.1.1, http://zenodo.org/record/10068449
Additional file 6: of Tranexamic acid in bleeding trauma patients: an exploration of benefits and harms
Creators: name: Roberts, Ian
name: Edwards, Phil
name: Prieto, David
name: Miland Joshi
name: Abda Mahmood
name: Ker, Katharine
name: Shakur, Haleema
Publisher: name: Figshare
Year: 2017
Subjects: subject: Biochemistry
subject: Medicine
subject: 69999 Biological Sciences not elsewhere classified
subject: FOS: Biological sciences
subject: Developmental Biology
subject: Marine Biology
subject: Cancer
subject: Science Policy
subject: 110309 Infectious Diseases
subject: FOS: Health sciences
subject: Computational Biology

description: List of ethics committees that approved the trial. List of ethics committees. (DOCX 21 kb)
title: Cuneiform Tablet HS 1072
Creators: name: NN
Publisher: name: heidICON, Heidelberg University Library
Year: 2025

description: Genre: Administrative
Dates referenced: Amar-Suen.07.12.00, Amar-Suen.08.03.00
Accounting period: Amar-Suen.07.12.00 to Amar-Suen.08.03.00
Additional file 6: of Tranexamic acid in bleeding trauma patients: an exploration of benefits and harms
Creators: name: Roberts, Ian
name: Edwards, Phil
name: Prieto, David
name: Miland Joshi
name: Abda Mahmood
name: Ker, Katharine
name: Shakur, Haleema
Publisher: name: Figshare
Year: 2017
Subjects: subject: Biochemistry
subject: Medicine
subject: 69999 Biological Sciences not elsewhere classified
subject: FOS: Biological sciences
subject: Developmental Biology
subject: Marine Biology
subject: Cancer
subject: Science Policy
subject: Infectious Diseases
subject: FOS: Health sciences
subject: Computational Biology

description: List of ethics committees that approved the trial. List of ethics committees. (DOCX 21 kb)
title: Geologic map of the Cain City Quadrangle, Gillespie and Kendall Counties, Texas
title: Geology of the Cain City Quadrangle, Gillespie and Kendall Counties, Texas
titleType: AlternativeTitle
title: Cain City Quadrangle, Gillespie and Kendall Counties, Texas
titleType: AlternativeTitle
Creators: name: Barnes, Virgil E. (Virgil Everett), 1903-1998
Publisher: name: University of Texas at Austin. Bureau of Economic Geology
Year: 1952
Subjects: subject: Geology -- Texas -- Gillespie County -- Maps
subject: Geology -- Texas -- Kendall County -- Maps

description: To obtain a print version of this publication visit: https://store.beg.utexas.edu/ and search for: GQ0013. 1 fold-out plate with text and map : Geologic Map of the Cain City Quadrangle, Gillespie and Kendall Counties, Texas
description: Cain City quadrangle is south of the Llano region and is in the marginal portion of the Edwards Plateau where much of the plateau surface has been destroyed by erosion. Northeastward-trending lobes and outliers of the Edwards Plateau are present in the southern part. The rest of the quadrangle is in the gently undulating broad Pedernales River basin. The geology of the Cain City quadrangle is shown on a planimetric map since the only topographic map available is the reconnaissance 30-minute Fredericksburg quadrangle. Elevations ranging between 1,512 and 1,932 feet were determined during traversing for control, but neither the highest nor the lowest elevation was reached. However, from the traverse it is estimated that the relief within the quadrangle is about 500 feet, ranging between about 1,500 and 2,000 feet in elevation. The quadrangle is entirely within the Pedernales River drainage basin and is mostly drained by South Grape Creek, Meusebach Creek, and numerous short branches of Pedernales River. Barons Creek and Palo Alto Creek empty into Pedernales River within the quadrangle. The Cain City quadrangle is on the southern side of the Llano uplift, and rocks of Ordovician age outcrop as inliers surrounded by Cretaceous rocks. The faulting accompanying the Ouachita orogeny (Barnes, 1948) is not exposed but southeastward dips up to 8 are present in the Paleozoic rocks. The Cretaceous rocks are essentially horizontal, dipping mostly southward about 8 feet per mile. A gentle nose with a southeastward trend is present, and one of the few faults in Cretaceous rocks noted in the vicinity of the Llano uplift is in the southern part of the quadrangle. Broader discussions of the stratigraphic, structural, economic, and geophysical problems of the region cannot be given in the space available. References cited below deal with some of these problems. This publication on the Cain City quadrangle is one of a series of similar publications, an index to which is shown on the opposite page. The reader is referred to this index map to locate other quadrangles mentioned in the present text.
Napaeozapus insignis
Creators: name: Wilson, Don E.
name: Reeder, DeeAnn
Publisher: name: The Johns Hopkins University Press
Year: 2005
Subjects: Biodiversity
Taxonomy
Animalia
Chordata
Mammalia
Rodentia
Dipodidae
Napaeozapus
Napaeozapus insignis

description: Napaeozapus insignis (Miller 1891)
[Zapus] insignis Miller 1891, Am. Nat., 25: 742.
Type Locality: Canada, New Brunswick, Restigouche River.
Vernacular Names: Woodland Jumping Mouse.
Synonyms: Napaeozapus abietorum (Preble 1899); Napaeozapus algonquinensis Prince 1941; Napaeozapus frutectanus Jackson 1919; Napaeozapus gaspensis Anderson 1942; Napaeozapus roanensis (Preble 1899); Napaeozapus saguenayensis Anderson 1942.
Distribution: Canada: SE Manitoba, SW and E Ontario, S and E Quebec north to S Labrador. USA: E Minnesota, N and C Wisconsin, upper peninsular and N lower peninsular Michigan, E Ohio, Pennsylvania; north and east to NW New Jersey, New York, Connecticut, Rhode Island, W Massachusetts (isolated population in Martha's Vinyard), Vermont, New Hampshire, and Maine; south to West Virginia, W Virginia, E Kentucky, E Tennessee, W North Carolina, NW South Carolina, and NE Georgia.
Conservation: IUCN – Lower Risk (lc).
Discussion: A specimen of Napaeozapus was collected in Park County, Indiana (Lyon, 1942), though subsequent trapping failed to yield further examples (Mumford, 1969). The identity of the specimen was verified by Klingener (1965:645) and Wrigley (1972:42). Systematic revision and biology provided by Wrigley (1972). Myology, in context of adaptive and phylogenetic significance, studied by Klingener (1964). Diagnosis, range map, and records provided by Hall (1981). Population in E Kentucky discussed by Meade (1992). Reviewed by Whitaker and Wrigley (1972, Mammalian Species, 14), Whitaker and Hamilton (1998), and Whitaker (1999 a). For synonyms see Hall (1981).
description: Published as part of Wilson, Don E. & Reeder, DeeAnn, 2005, Order Rodentia - Family Dipodidae, pp. 871-893 in Mammal Species of the World: a Taxonomic and Geographic Reference (3 rd Edition), Volume 2, Baltimore :The Johns Hopkins University Press on page 892, DOI: 10.5281/zenodo.7316535
title: Geologic map of the Stonewall Quadrangle, Gillespie and Kendall Counties, Texas
title: Stonewall Quadrangle, Gillespie and Kendall Counties, Texas
titleType: AlternativeTitle
Creators: name: Barnes, Virgil E. (Virgil Everett), 1903-1998
Publisher: name: University of Texas at Austin. Bureau of Economic Geology
Year: 1952
Subjects: subject: Geology -- Texas -- Gillespie County -- Maps
subject: Geology -- Texas -- Kendall County -- Maps

description: To obtain a print version of this publication visit: https://store.beg.utexas.edu/ and search for: GQ0014. 1 fold-out plate with text and map : Geologic Map of the Stonewall Quadrangle, Gillespie and Kendall Counties, Texas
description: Stonewall quadrangle is south of the Llano region and is in the marginal portion of the Edwards Plateau where much of the plateau surface has been destroyed by erosion. Along the southern edge, lobes of the Edwards Plateau are present, which coalesce southward to form a continuous narrow east-west plateau belt part of which is just south of the Stonewall quadrangle. Most of the quadrangle is within the gently undulating, broad Pedernales River basin. The geology of the Stonewall quadrangle is shown on a planimetric map, and the only topographic map available is the reconnaissance 30-minute Fredericksburg quadrangle. Elevations ranging between 1,423 and 1,969 feet were determined during traversing for control, but neither the highest nor the lowest elevation was reached. However, it is estimated that the relief within the quadrangle is about 600 feet, ranging between about 1,400 and 2,000 feet in elevation. The quadrangle is largely within the Pedernales River drainage basin and is mostly drained by Three Mile Creek, South Grape Creek, and its tributary Dry Creek. Cave Creek enters the Pedernales River within the quadrangle, and other important branches drain a considerable area in the vicinity of the river. A small area in the southeastern corner of the quadrangle is drained by branches of the Blanco River. The Stonewall quadrangle is high on the southern side of the Llano uplift, and rocks of Cambrian and Ordovician age outcrop in the northern part as inliers surrounded by Cretaceous rocks. Faulting related to the Ouachita orogeny (Barnes, 1948) is present. The Cretaceous rocks are essentially horizontal, dipping eastward about 10 feet per mile. Broader discussions of the stratigraphic, structural, economic, and geophysical problems of the region cannot be given in the space available. References cited below deal with some of these problems. This publication on the Stonewall quadrangle is one of a series of similar publications, an index to which is shown on the opposite page. The reader is referred to this index map to locate other quadrangles mentioned in the present text.
Additional file 1. of Overweight and obesity in children aged 3–13 years in urban Cameroon: a cross-sectional study of prevalence and association with socio-economic status
Creators: name: Simeon-Pierre Choukem
name: Kamdeu-Chedeu, Josiane
name: Leary, Sam
name: Mboue-Djieka, Yannick
name: Nebongo, Daniel
name: Akazong, Christoph
name: Yacouba Mapoure
name: Hamilton-Shield, Julian
name: Jean-François Gautier
name: Mbanya, Jean
Publisher: name: Figshare
Year: 2017
Subjects: subject: Medicine
subject: Sociology
subject: FOS: Sociology
subject: Developmental Biology
subject: Science Policy
subject: Virology
subject: Computational Biology

description: Summary of all categorical variables; whole cohort and separately for HSES and LSES. HSES = High socioeconomic status; LSES = Low socioeconomic status; IQR = inter-quartile range; *p-value from chi-squared tests, HSES vs.LSES; †of those who receive pocket money, median (IQR) = 150 (100, 200) FCFA. (DOCX 16 kb)
title: Geologic map of the Wendel Quadrangle, Kimble, Kerr, and Gillespie Counties, Texas
title: Geology of the Wendel Quadrangle, Kimble, Gillespie, and Kerr Counties, Texas
titleType: AlternativeTitle
title: Wendel Quadrangle, Gillespie, Kerr, and Kimble Counties, Texas
titleType: AlternativeTitle
Creators: name: Barnes, Virgil E. (Virgil Everett), 1903-1998
Publisher: name: University of Texas at Austin. Bureau of Economic Geology
Year: 1954
Subjects: subject: Geology -- Texas -- Gillespie County -- Maps
subject: Geology -- Texas -- Kerr County -- Maps
subject: Geology -- Texas -- Kimble County -- Maps

description: To obtain a print version of this publication visit: https://store.beg.utexas.edu/ and search for: GQ0015. 1 fold-out plate with text and map : Geologic Map of the Wendel Quadrangle, Kimble, Kerr, and Gillespie Counties, Texas
description: Wendel quadrangle is entirely within the Edwards Plateau province and is situated southwest of the Llano region. The geology of the Wendel quadrangle is shown on a planimetric map, and the only topographic map available is the reconnaissance 30-minute Kerrville quadrangle. Elevations ranging between 2,041 and 2,284 feet were determined during traversing for control, but neither the highest nor the lowest elevation was reached. However, it is estimated that the relief within the quadrangle is about 270 feet, ranging between 2,020 and 2,290 feet. The quadrangle has diverse drainage patterns. About half the drainage flows westward and northward to Little Devils River, ultimately reaching the Llano River by way of James River. White Oak Creek, Fall Prong, and Burr Oak Draw are the chief tributaries of Little Devils River. The headwaters of the Pedernales River occupy about one-third of the quadrangle, centered in the southeastern part. A small area in the northwest corner drains into Threadgill Creek and then into Beaver Creek and Llano River. A small area in the southwestern part of the quadrangle is in the Guadalupe River drainage basin, reaching the river by way of Rough Hollow and Johnson Creek. The Wendel quadrangle is on the southwestern side of the Llano uplift, and Cretaceous rocks crop out throughout the quadrangle. Rocks of Ordovician and Carboniferous age are probably less than a thousand feet below the surface. The Cretaceous rocks are essentially horizontal. References cited below deal more broadly with some of the stratigraphic, structural, economic, and geophysical problems of the region. This publication on the Wendel quadrangle is one of a series of similar publications, an index to which is shown on the opposite page. The reader is referred to the index map to locate other quadrangles mentioned in the present text.
Podocoryna borealis Mayer 1900
Creators: name: OLIVEIRA, OTTO M. P.
name: MIRANDA, THAÍS P.
name: ARAUJO, ENILMA M.
name: AYÓN, PATRICIA
name: CEDEÑO-POSSO, CRISTINA M.
name: CEPEDA-MERCADO, AMANCAY A.
name: CÓRDOVA, PABLO
name: CUNHA, AMANDA F.
name: GENZANO, GABRIEL N.
name: HADDAD, MARIA ANGÉLICA
name: MIANZAN, HERMES W.
name: MIGOTTO, ALVARO E.
name: MIRANDA, LUCÍLIA S.
name: MORANDINI, ANDRÉ C.
name: NAGATA, RENATO M.
name: NASCIMENTO, KARINE B.
name: JÚNIOR, MIODELI NOGUEIRA
name: PALMA, SERGIO
name: QUIÑONES, JAVIER
name: RODRIGUEZ, CAROLINA S.
name: SCARABINO, FABRIZIO
name: SCHIARITI, AGUSTÍN
name: STAMPAR, SÉRGIO N.
name: TRONOLONE, VALQUÍRIA B.
name: MARQUES, ANTONIO C.
Publisher: name: Zenodo
Year: 2016
Subjects: Biodiversity
Taxonomy
Animalia
Cnidaria
Hydrozoa
Anthoathecata
Hydractiniidae
Podocoryna
Podocoryna borealis

description: Podocoryna borealis (Mayer, 1900)
Synonyms in the area: Podocoryne borealis —Pagès & Orejas 1999 [medusa];? Hydractinia sp.—Galea 2007 p. 23 [polyp]; Hydractinia borealis –Palma et al. 2007a p. 70, 73, 2007b p. 73, 74, 78, 80, 2011; Villenas et al. 2009; Bravo et al. 2011 [medusa].
Remarks: the geographic distribution of Podocoryna borealis (Mayer, 1900) is restricted to the North Atlantic and North Sea (Schuchert 2008).
Distribution in South America: polyp—Pacific Ocean, Chile, at 42.38°S 72.43°W (Galea 2007 p. 23); medusa—Pacific Ocean, Chile, from 41.50°S to 54.903°S in the Patagonian interior waters (Pagès & Orejas 1999; Galea 2007 p. 23; Palma et al. 2007a p. 70, 73, 2007b p. 73, 74, 78, 80, 2011; Villenas et al. 2009; Bravo et al. 2011).
Habitat: species with bipolar distribution (Pagès & Orejas 1999). medusa—from 0-50m depth (Galea 2007 p. 23).
description: Published as part of OLIVEIRA, OTTO M. P., MIRANDA, THAÍS P., ARAUJO, ENILMA M., AYÓN, PATRICIA, CEDEÑO-POSSO, CRISTINA M., CEPEDA-MERCADO, AMANCAY A., CÓRDOVA, PABLO, CUNHA, AMANDA F., GENZANO, GABRIEL N., HADDAD, MARIA ANGÉLICA, MIANZAN, HERMES W., MIGOTTO, ALVARO E., MIRANDA, LUCÍLIA S., MORANDINI, ANDRÉ C., NAGATA, RENATO M., NASCIMENTO, KARINE B., JÚNIOR, MIODELI NOGUEIRA, PALMA, SERGIO, QUIÑONES, JAVIER, RODRIGUEZ, CAROLINA S., SCARABINO, FABRIZIO, SCHIARITI, AGUSTÍN, STAMPAR, SÉRGIO N., TRONOLONE, VALQUÍRIA B. & MARQUES, ANTONIO C., 2016, Census of Cnidaria (Medusozoa) and Ctenophora from South American marine waters, pp. 1-256 in Zootaxa 4194 (1) on page 64, DOI: 10.11646/zootaxa.4194.1.1, http://zenodo.org/record/10068449
title: Geologic map of the Harper Quadrangle, Gillespie County, Texas
title: Harper Quadrangle, Gillespie County, Texas
titleType: AlternativeTitle
Creators: name: Barnes, Virgil E. (Virgil Everett), 1903-1998
Publisher: name: University of Texas at Austin. Bureau of Economic Geology
Year: 1954
Subjects: subject: Geology -- Texas -- Gillespie County -- Maps

description: To obtain a print version of this publication visit: https://store.beg.utexas.edu/ and search for: GQ0016. 1 fold-out plate with text and map : Geologic Map of the Harper Quadrangle, Gillespie County, Texas, 1954
description: Harper quadrangle is in the Edwards Plateau province south of the Llano region. The plateau surface within the quadrangle is dissected by the Pedernales River and its tributaries in the southern part, and by Threadgill and Edwards Creeks in the northern part. The geology of the Harper quadrangle is shown on a planimetric map, and the only topographic map available is the reconnaissance 30-minute Kerrville quadrangle. Elevations ranging between 1,891 and 2,226 feet were determined during traversing for control, but only the highest point was reached. The lowest point is somewhere in the southeastern part of the quadrangle and is estimated to be at an elevation of about 1,800 feet, giving about 425 feet of relief for the quadrangle. About two-thirds of the quadrangle is directly drained by Pedernales River and its branches. The northern third of the quadrangle is in the Llano River drainage basin and is drained by Edwards Creek, Maverick Spring Branch, and the headwaters of Threadgill Creek, which reach Llano River by way of Threadgill Creek and Beaver Creek. The Harper quadrangle is on the south side of the Llano uplift, and Cretaceous rocks crop out in all of the quadrangle. Rocks of Cambrian and Ordovician age are not far beneath the more deeply incised streams. The Cretaceous rocks are essentially horizontal and may dip 2 or 3 feet per mile to the northwest. Broader discussions of the stratigraphic, structural, economic, and geophysical problems of the region are given in references cited below. This publication on the Harper quadrangle is one of a series of similar publications, an index to which is shown on the opposite page. The reader is referred to the index map to locate other quadrangles mentioned in the present text.
Faronus AUBE 1844
Creators: name: Assing, Volker
name: Brachat, Volker
name: Meybohm, Heinrich
Publisher: name: Zenodo
Year: 2019
Subjects: Biodiversity
Taxonomy
Animalia
Arthropoda
Insecta
Coleoptera
Staphylinidae
Faronus

description: Genus Faronus AUBÉ, 1844
Previously, only one species of this Mediterranean genus had been recorded from Crete, F. lafertei AUBÉ, 1844 (BLATTNÝ & BLATTNÝ 1916). Since the distribution of A. lafertei is confined to the West Mediterranean, this record undoubedly refers to F. parallelus BESUCHET, 1958, a widespread East Mediterranean species. Three additional species, all of them endemic to the Lefka Ori, West Crete, are described below.
Many Faronus species are subject to remarkable intraspecific variation, particularly of the number and position of impressions on the pronotum and the elytra, the length of the hind wings, and even of the shape of the aedeagus. The latter is often inverted (mirrored).
description: Published as part of Assing, Volker, Brachat, Volker & Meybohm, Heinrich, 2019, Monograph of the Staphylinidae of Crete (Greece). Part II. Descriptions of new species (Insecta: Coleoptera), pp. 239-289 in Beiträge Zur Entomologie = Contributions to Entomology 69 (2) on page 285, DOI: 10.21248/contrib.entomol.69.2.239-289, http://zenodo.org/record/4755240
Zapus Coues 1875
Creators: name: Wilson, Don E.
name: Reeder, DeeAnn
Publisher: name: The Johns Hopkins University Press
Year: 2005
Subjects: Biodiversity
Taxonomy
Animalia
Chordata
Mammalia
Rodentia
Dipodidae
Zapus

description: Zapus Coues 1875
Zapus Coues 1875, Bull. U. S. Geol. Geogr. Surv. Terr., ser. 2, 5 (3): 253.
Type Species: Dipus hudsonius Zimmermann 1780
Species and subspecies: 3 species:
Species Zapus hudsonius (Zimmermann 1780)
Species Zapus princeps Allen 1893
Species Zapus trinotatus Rhoads 1894
Discussion: Revised by Preble (1899) and Krutzsch (1954). Myology, in context of adaptive and phylogenetic significance, studied by Klingener (1964). Dental evolution investigated by Klingener (1963). For verification of the absence of cheek pouches in Zapus see Klingener (1971). Phallic morphology described by Shenbrot (1992). Evolutionary history extends back to late Pliocene in North America (Klingener, 1963; R. A. Martin, 1994).
description: Published as part of Wilson, Don E. & Reeder, DeeAnn, 2005, Order Rodentia - Family Dipodidae, pp. 871-893 in Mammal Species of the World: a Taxonomic and Geographic Reference (3 rd Edition), Volume 2, Baltimore :The Johns Hopkins University Press on page 892, DOI: 10.5281/zenodo.7316535
Ellesmerellidae Vachard
Creators: name: Vachard, Daniel
name: Le Coze, Francois
Publisher: name: Zenodo
Year: 2024
Subjects: Biodiversity
Taxonomy
Chromista
Foraminifera
Tubothalamea
Miliolida
Ellesmerellidae

description: Family ELLESMERELLIDAE Vachard in Krainer, Vachard & Schaffhauser, 2019
Description. See Fig. 8.
Composition: Ellesmerella Mamet & Roux in Mamet et al., 1987; Paraellesmerella Vachard in Krainer, Vachard & Schaffhauser, 2019.
description: Published as part of Vachard, Daniel & Le Coze, Francois, 2024, Paleozoic Foraminifera: Current State Of The Classification And Perspectives, pp. 97-130 in Acta Palaeontologica Romaniae 20 (2) on page 121, DOI: 10.35463/j.apr.2024.02.07, http://zenodo.org/record/14656136
Additional file 16: Table S7. of Evaluation of logistic regression models and effect of covariates for case–control study in RNA-Seq analysis
Creators: name: Choi, Seung
name: Labadorf, Adam
name: Myers, Richard
name: Lunetta, Kathryn
name: Dupuis, Josée
name: DeStefano, Anita
Publisher: name: Figshare
Year: 2017
Subjects: subject: Genetics
subject: FOS: Biological sciences
subject: Sociology
subject: FOS: Sociology
subject: 69999 Biological Sciences not elsewhere classified
subject: Cancer
subject: Inorganic Chemistry
subject: FOS: Chemical sciences

description: Bias with covariate models from the balanced design of N D=1  = 10 and μ D=0  = 1000. Disp: Dispersion, CovOR: Odds ratios between covariates and case–control status, Ncov: The number of covariates in a model, NB_TD: Negative binomial regression with the dispersion is used for the sampling, FL: Firth’s logistic regression. (DOCX 47 kb)
Podocoryna carnea M. Sars 1846
Creators: name: OLIVEIRA, OTTO M. P.
name: MIRANDA, THAÍS P.
name: ARAUJO, ENILMA M.
name: AYÓN, PATRICIA
name: CEDEÑO-POSSO, CRISTINA M.
name: CEPEDA-MERCADO, AMANCAY A.
name: CÓRDOVA, PABLO
name: CUNHA, AMANDA F.
name: GENZANO, GABRIEL N.
name: HADDAD, MARIA ANGÉLICA
name: MIANZAN, HERMES W.
name: MIGOTTO, ALVARO E.
name: MIRANDA, LUCÍLIA S.
name: MORANDINI, ANDRÉ C.
name: NAGATA, RENATO M.
name: NASCIMENTO, KARINE B.
name: JÚNIOR, MIODELI NOGUEIRA
name: PALMA, SERGIO
name: QUIÑONES, JAVIER
name: RODRIGUEZ, CAROLINA S.
name: SCARABINO, FABRIZIO
name: SCHIARITI, AGUSTÍN
name: STAMPAR, SÉRGIO N.
name: TRONOLONE, VALQUÍRIA B.
name: MARQUES, ANTONIO C.
Publisher: name: Zenodo
Year: 2016
Subjects: Biodiversity
Taxonomy
Animalia
Cnidaria
Hydrozoa
Anthoathecata
Hydractiniidae
Podocoryna
Podocoryna carnea

description: Podocoryna carnea (M. Sars, 1846)
Synonyms in the area:? Podocoryne carnea var. chilensis —Kramp 1952 [polyp and medusa]; Podocoryne carnea —Segura-Puertas 1984 [medusa].
Distribution in South America: polyp—Pacific Ocean, Chile, at Puerto Montt (Kramp 1952). medusa—Pacific Ocean, Peru to Chile, from 15°S to 56°S (Kramp 1952; Segura-Puertas 1984);
Habitat: medusa—eurythermic and euryhaline species (Segura-Puertas 1984).
description: Published as part of OLIVEIRA, OTTO M. P., MIRANDA, THAÍS P., ARAUJO, ENILMA M., AYÓN, PATRICIA, CEDEÑO-POSSO, CRISTINA M., CEPEDA-MERCADO, AMANCAY A., CÓRDOVA, PABLO, CUNHA, AMANDA F., GENZANO, GABRIEL N., HADDAD, MARIA ANGÉLICA, MIANZAN, HERMES W., MIGOTTO, ALVARO E., MIRANDA, LUCÍLIA S., MORANDINI, ANDRÉ C., NAGATA, RENATO M., NASCIMENTO, KARINE B., JÚNIOR, MIODELI NOGUEIRA, PALMA, SERGIO, QUIÑONES, JAVIER, RODRIGUEZ, CAROLINA S., SCARABINO, FABRIZIO, SCHIARITI, AGUSTÍN, STAMPAR, SÉRGIO N., TRONOLONE, VALQUÍRIA B. & MARQUES, ANTONIO C., 2016, Census of Cnidaria (Medusozoa) and Ctenophora from South American marine waters, pp. 1-256 in Zootaxa 4194 (1) on page 64, DOI: 10.11646/zootaxa.4194.1.1, http://zenodo.org/record/10068449
THE DESCRIPTION OF THE TOPONYMY OF UZBEKISTAN IN THE WORK "HUDUD UL-OLAM"
Creators: name: Usmonaliev, Isroiljon
Publisher: name: Zenodo
Year: 2025

description: This article provides an analysis of the work "Hudud ul-olam" and its sections, the scientific foundations of this work in the works of scientists, and a detailed description of the geographical, ethnographic, economic and toponomic names of the territory of Uzbekistan in the work.