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zenodo32/100

Subspecies and Distribution. C.m.mitisWolf,1822—WAngola. C.m.boutourliniiGiglioli,1887—SWEthiopia,fromLakeTanaSalongtheWsideoftheEthiopianRifttoNofLakeTurkana. C.m.elgonisLonnberg,1919—WKenya(MtElgon).IntermediatesbetweenthesubspecieselgonisandstuhlmanniiarefoundinKakamegaForestandontheeasternflanksoftheRuwenzoriMts. C.m.heymansiColyn&Verheyen,1987—EDRCongo(betweentheLomaniandLualabarivers,reachingtoc.2°S,andextendingslightlytotheWoftheLomaniRiver). C.m.opusthostictusSclater,1894—SEDRCongo(fromc.6°NontheWbankoftheLualabaRiverStoKatangaProvince,andWtotheLakeTanganyika),NZambia(WoftheLuangwaRiver),andEAngola. C.m.schoutedeniSchwarz,1928—EDRCongo,typicallyonIdjwiandShushuislandsinLakeKivu;onthemainland,specimensarefromtheWVirungaVolcanoesandasfarSWasBobandana,althoughthesestronglytendtowardthesubspeciesstuhlmanni. C. m. stuhlmanni Matschie, 1893 — S South Sudan (Didinga Hills and Imatong Mts), Uganda (N in Bunyoro, E in Tororo, and in the W), W Kenya (W of the Rift Valley, including Mt Elgon and Kakamega Forest), and NE DR Congo, from the region between the Uele and the Congo rivers, from the Itimbiri River E to the Ituri and Semliki Forests, and S to the LLualaba River c.6° S. in Cercopithecidae

Subspecies and Distribution. C.m.mitisWolf,1822—WAngola. C.m.boutourliniiGiglioli,1887—SWEthiopia,fromLakeTanaSalongtheWsideoftheEthiopianRifttoNofLakeTurkana. C.m.elgonisLonnberg,1919—WKenya(MtElgon).IntermediatesbetweenthesubspecieselgonisandstuhlmanniiarefoundinKakamegaForestandontheeasternflanksoftheRuwenzoriMts. C.m.heymansiColyn&Verheyen,1987—EDRCongo(betweentheLomaniandLualabarivers,reachingtoc.2°S,andextendingslightlytotheWoftheLomaniRiver). C.m.opusthostictusSclater,1894—SEDRCongo(fromc.6°NontheWbankoftheLualabaRiverStoKatangaProvince,andWtotheLakeTanganyika),NZambia(WoftheLuangwaRiver),andEAngola. C.m.schoutedeniSchwarz,1928—EDRCongo,typicallyonIdjwiandShushuislandsinLakeKivu;onthemainland,specimensarefromtheWVirungaVolcanoesandasfarSWasBobandana,althoughthesestronglytendtowardthesubspeciesstuhlmanni. C. m. stuhlmanni Matschie, 1893 — S South Sudan (Didinga Hills and Imatong Mts), Uganda (N in Bunyoro, E in Tororo, and in the W), W Kenya (W of the Rift Valley, including Mt Elgon and Kakamega Forest), and NE DR Congo, from the region between the Uele and the Congo rivers, from the Itimbiri River E to the Ituri and Semliki Forests, and S to the LLualaba River c.6° S.

opennotspecifiedMar 2013View details →
zenodo32/100

Distribution. NE Africa E of the White Nile, in Eritrea, Ethiopia (S to the Omo River and E as far as the Rift Valley), Djibouti, SE Sudan (from Khartoum in the N to Mongalla in the S), and E South Sudan; possibly in S Egypt. in Cercopithecidae

Distribution. NE Africa E of the White Nile, in Eritrea, Ethiopia (S to the Omo River and E as far as the Rift Valley), Djibouti, SE Sudan (from Khartoum in the N to Mongalla in the S), and E South Sudan; possibly in S Egypt.

opennotspecifiedMar 2013View details →
zenodo32/100

Nesokia is sister to Bandicota and are nested in Rattus phylogenetically, making Rat- tus paraphyletic. Tarsomys, Limnomys, and Diplothrix are also phylogenetically in Rat- tus, and the clade is in need of focused re- vision at the generic level. Nesokia bunnui was originally described as a separate ge-nus, Erythronesokia, because it is morphologically very distinctive from N. indica. Type specimen was destroyed during the Iraq War, and a neotype was recently designated to replace it. Monotypic. Distribution. Tigris and Euphrates river valleys, SE Iraq. Descriptive notes. Head—body 230-260 mm, tail 205-270 mm, ear 18-21 mm, hindfoot 49-58 mm; weight 519 g. The Long-tailed Bandicoot Rat is larger than the Short-tailed Bandicoot Rat (N. indica). Pelage is soft and woolly, interspersed with harsher coarse hair and long black hairs near mid-back. Dorsum is fawn to ocherous red, washed with purple or chestnuton darker individuals. Hairs are basally slate-gray and distally rufous, occasionally with whitish or black tips. Muzzle is drab. Sides arefawn, with gray edge toward venter. Venteris whitish, extending onto cheeks where the same pattern from gray to fawn to dorsal pelage occurs. Feet are large and robust, being light brown and well-furred dorsally. Claws are amber on forefeet and dull brown on hindfeet; pollux is extremely small. Ears are moderately long and brownish, with no hair internally. Tail is ¢.82-104% of head-body length and deep brownish drab, interspersed with visible white hair. Skull is large and robust, similarly to the Short-tailed Bandicoot Rat. Habitat. Marsh and swamp land. Food and Feeding. No information. Breeding. No information. Activity patterns. The Long-tailed Bandicoot Rat is terrestrial, although it isfound in swampy and marshy areas and is probably amphibious. Movements, Home range and Social organization. No information. Status and Conservation. Classified as Endangered on The IUCN Red List. The Longtailed Bandicoot Rat is apparently rare and is known from very few specimens. Marsh and swamp habitats in which it is found were completely destroyed during the Iraq War by draining, war damage, and agricultural expansion. In recent years, flooding from Tigris and Euphrates rivers and high snow fall and melt haveresulted in partial restoration ofits native habitat, although restoration is not a complete. Populations are now probably highly fragmented. Bibliography. Al-Ansari et al. (2012), Al-Robaae & Felten (1990), Khajuria (1981), Krystufek et al. (2017), Musser & Carleton (2005), Richardson & Hussain (2006), Stuart (2008). in Muridae

Nesokia is sister to Bandicota and are nested in Rattus phylogenetically, making Rat- tus paraphyletic. Tarsomys, Limnomys, and Diplothrix are also phylogenetically in Rat- tus, and the clade is in need of focused re- vision at the generic level. Nesokia bunnui was originally described as a separate ge-nus, Erythronesokia, because it is morphologically very distinctive from N. indica. Type specimen was destroyed during the Iraq War, and a neotype was recently designated to replace it. Monotypic. Distribution. Tigris and Euphrates river valleys, SE Iraq. Descriptive notes. Head—body 230-260 mm, tail 205-270 mm, ear 18-21 mm, hindfoot 49-58 mm; weight 519 g. The Long-tailed Bandicoot Rat is larger than the Short-tailed Bandicoot Rat (N. indica). Pelage is soft and woolly, interspersed with harsher coarse hair and long black hairs near mid-back. Dorsum is fawn to ocherous red, washed with purple or chestnuton darker individuals. Hairs are basally slate-gray and distally rufous, occasionally with whitish or black tips. Muzzle is drab. Sides arefawn, with gray edge toward venter. Venteris whitish, extending onto cheeks where the same pattern from gray to fawn to dorsal pelage occurs. Feet are large and robust, being light brown and well-furred dorsally. Claws are amber on forefeet and dull brown on hindfeet; pollux is extremely small. Ears are moderately long and brownish, with no hair internally. Tail is ¢.82-104% of head-body length and deep brownish drab, interspersed with visible white hair. Skull is large and robust, similarly to the Short-tailed Bandicoot Rat. Habitat. Marsh and swamp land. Food and Feeding. No information. Breeding. No information. Activity patterns. The Long-tailed Bandicoot Rat is terrestrial, although it isfound in swampy and marshy areas and is probably amphibious. Movements, Home range and Social organization. No information. Status and Conservation. Classified as Endangered on The IUCN Red List. The Longtailed Bandicoot Rat is apparently rare and is known from very few specimens. Marsh and swamp habitats in which it is found were completely destroyed during the Iraq War by draining, war damage, and agricultural expansion. In recent years, flooding from Tigris and Euphrates rivers and high snow fall and melt haveresulted in partial restoration ofits native habitat, although restoration is not a complete. Populations are now probably highly fragmented. Bibliography. Al-Ansari et al. (2012), Al-Robaae & Felten (1990), Khajuria (1981), Krystufek et al. (2017), Musser & Carleton (2005), Richardson & Hussain (2006), Stuart (2008).

opennotspecifiedNov 2017View details →
zenodo32/100

Distribution. Endemic to Ethiopia, where it is known only from a few localities, most- ly in the Rift Valley. in Muridae

Distribution. Endemic to Ethiopia, where it is known only from a few localities, most- ly in the Rift Valley.

opennotspecifiedNov 2017View details →
zenodo32/100

Distribution. Mt Elgon, Cherangani Hills, and Mau Escarpment in Kenya, W of Rift Valley; presumably on Ugandan slopes of Mt Elgon. in Muridae

Distribution. Mt Elgon, Cherangani Hills, and Mau Escarpment in Kenya, W of Rift Valley; presumably on Ugandan slopes of Mt Elgon.

opennotspecifiedNov 2017View details →
zenodo32/100

Other common names: East African Grammomys, Rwenzori Grammomys, Rwenzori Thicket Rat Taxonomy. Thamnomys ibeanus Osgood, 1910, Molo, Kenya. Grammomys ibeanus was previously includ-ed in G. cometes, but molecular data show it to be closer to G. macmillani. Monotypic. Distribution. Occurs quite widely in E Africa associated with mountains of the Rift Valley system and the Eastern Arc, including S South Sudan, E Uganda, Kenya, Tanzania, Malawi, and Mozambique. in Muridae

Other common names: East African Grammomys, Rwenzori Grammomys, Rwenzori Thicket Rat Taxonomy. Thamnomys ibeanus Osgood, 1910, Molo, Kenya. Grammomys ibeanus was previously includ-ed in G. cometes, but molecular data show it to be closer to G. macmillani. Monotypic. Distribution. Occurs quite widely in E Africa associated with mountains of the Rift Valley system and the Eastern Arc, including S South Sudan, E Uganda, Kenya, Tanzania, Malawi, and Mozambique.

opennotspecifiedNov 2017View details →
zenodo32/100

Distribution. Widespread from Mauritania and Senegal E to Ethiopia, and S to Tanzania and SW Zambia; range extends N along Nile Valley to the Nile Delta in Egypt, with an isolated population in SW Arabia (Yemen). in Muridae

Distribution. Widespread from Mauritania and Senegal E to Ethiopia, and S to Tanzania and SW Zambia; range extends N along Nile Valley to the Nile Delta in Egypt, with an isolated population in SW Arabia (Yemen).

opennotspecifiedNov 2017View details →
zenodo32/100

Distribution. Three disjunct populations in SW & E South Africa, in the Paarl Valley and Cape Peninsula of Western Cape Province and E slopes of the Drakensberg in Mpumalanga and KwaZulu-Natal provinces. in Muridae

Distribution. Three disjunct populations in SW & E South Africa, in the Paarl Valley and Cape Peninsula of Western Cape Province and E slopes of the Drakensberg in Mpumalanga and KwaZulu-Natal provinces.

opennotspecifiedNov 2017View details →
zenodo32/100

Distribution. Known from three localities along the Central Range of New Guinea (Mt Trikora, Tifalmin Valley, and Star Mts), at elevations of 1800-2800 m. in Muridae

Distribution. Known from three localities along the Central Range of New Guinea (Mt Trikora, Tifalmin Valley, and Star Mts), at elevations of 1800-2800 m.

opennotspecifiedNov 2017View details →
zenodo32/100

Distribution. Known only from Bele River valley, vicinity of Lake Habbema, WC New Guinea; it may occur on Mt Minni, Star Mts, but capture of a living animal is needed to confirm species identity. in Muridae

Distribution. Known only from Bele River valley, vicinity of Lake Habbema, WC New Guinea; it may occur on Mt Minni, Star Mts, but capture of a living animal is needed to confirm species identity.

opennotspecifiedNov 2017View details →
zenodo32/100

Distribution. New Guinea, including the Papuan Peninsula (Owen Stanley, Astrolabe, and Maneau ranges) and an outlying record at Markham River Valley, Morobe Province, and D'Entrecasteaux Is (Goodenough, Fergusson, and Normanby). in Muridae

Distribution. New Guinea, including the Papuan Peninsula (Owen Stanley, Astrolabe, and Maneau ranges) and an outlying record at Markham River Valley, Morobe Province, and D'Entrecasteaux Is (Goodenough, Fergusson, and Normanby).

opennotspecifiedNov 2017View details →
zenodo32/100

Distribution. Recorded from five discrete areas of New Guinea, including the Swart Valley of the Snow (= Surdiman) Mts, SW slopes of Mt Sisa, E Central Cordillera, Cromwell Range on Huon Peninsula, and Astrolabe Range. in Muridae

Distribution. Recorded from five discrete areas of New Guinea, including the Swart Valley of the Snow (= Surdiman) Mts, SW slopes of Mt Sisa, E Central Cordillera, Cromwell Range on Huon Peninsula, and Astrolabe Range.

opennotspecifiedNov 2017View details →
zenodo32/100

Distribution. Both sides of Nile Delta Valley and Sinai, N Egypt, and Negev and coastal plains of S Israel and Palestine. in Muridae

Distribution. Both sides of Nile Delta Valley and Sinai, N Egypt, and Negev and coastal plains of S Israel and Palestine.

opennotspecifiedNov 2017View details →
zenodo32/100

Width area slope data, valley bottom polygons and width measurements

<p>This link contains:</p> <p>1. &quot;Sections_raw_data_resubmission.xlsx&quot; - An excel file with 13 sheets. 12 sheets refer&nbsp;to the valley sections analyzed in the study, and one refers to the&nbsp;channel width data&nbsp;explored in valley 12.&nbsp;</p> <p>2.&nbsp;&nbsp;kml shapefiles of the valley bottom polygons before and after manual editing</p> <p>3. &nbsp;kml shapefiles of the width measuraments</p>

opencc-by-4.0Aug 2022View details →
zenodo32/100

Finite-Source Model of the M6.0 July 8, 2021 Antelope Valley, CA Earthquake

<p>This zip file contains the InSAR line-of-sight (LOS) displacements derived from Sentinel-1 data collected along four satellite tracks (T42,T64, T137, T144) covering the 2021 M6 Antelope Valley earthquake in Eastern California. For each track, all possible interferograms of roughly 1-month long in time spanning the earthquake without sharing a common scene are stacked to obtain the average coseismic LOS displacement. See text for details.</p> <p>&nbsp;</p> <p># data format: NetCDF grid file</p> <p>&quot;dlos_stack_coseismic.grd&quot;&nbsp; ---- average coseismic LOS displacement (unit: meters); positive value corresponds to surface deformation toward the satellite.</p> <p>look_e/n/u.grd --- East, North, Vertical (Up) components of the line-of-sight direction, so that</p> <p>&nbsp;</p> <p>&nbsp; &nbsp; &nbsp; dlos_displacement = dUe*look_e + dUn*look_n + dUup*look_u</p> <p>&nbsp;</p> <p>where dUe, dUn, and dUup represent the Eastward, Northward, and Upward surface motion.</p> <p>&nbsp;</p> <p>We also provide the ascii-format downsampled LOS displacement of each track that went into the coseismic slip modeling (&quot;dlos_stack_coseismic_samp.txt&quot;). The file contains 6 columns:</p> <p>#longitude&nbsp; latitude&nbsp; dLOS(cm) vE&nbsp; &nbsp; vN&nbsp; vUp</p> <p>Questions: Kang Wang (kangwang@berkeley.edu)</p> <p>&nbsp;</p>

opencc-by-4.0Aug 2022View details →
zenodo32/100

Dog Valley Fault Traces

<p>This is a shapefile containing linework of the Dog Valley Fault in Northern California.&nbsp;</p>

opencc-by-4.0Aug 2022View details →
zenodo32/100

Dog Valley Trench Orthoimages

<p>These are orthoimages of the DV1 trench site in Hoke Valley on the Dog Valley fault in Northern California.&nbsp;</p>

opencc-by-4.0Aug 2022View details →
zenodo32/100

FIGURE. Petalidium mannheimerae, morphology of flowers from different localities in the Richtersveld, Northern Cape, South Africa (A–D), and leaf morphology (E). A. Flower in lateral view (Sun Valley). B. Flower in front view (Sun Valley). C. Flower in front view (Kosies). D. Flowers (Umdaus). E. Branchlet showing leaves being semi-succulent, the blade subconduplicate to conduplicate, recurved towards apex, the margins with isolated, robust, stalked glandular trichomes. Scale bar = 5 mm. Photographs by M. Koekemoer (A–C), N. Jürgens (D), & W. Swanepoel (E). in Petalidium mannheimerae (Acanthaceae), a new species from Namibia and South Africa, with notes on the taxonomic identity of P. parvifolium

FIGURE. Petalidium mannheimerae, morphology of flowers from different localities in the Richtersveld, Northern Cape, South Africa (A–D), and leaf morphology (E). A. Flower in lateral view (Sun Valley). B. Flower in front view (Sun Valley). C. Flower in front view (Kosies). D. Flowers (Umdaus). E. Branchlet showing leaves being semi-succulent, the blade subconduplicate to conduplicate, recurved towards apex, the margins with isolated, robust, stalked glandular trichomes. Scale bar = 5 mm. Photographs by M. Koekemoer (A–C), N. Jürgens (D), &amp; W. Swanepoel (E).

opennotspecifiedSep 2022View details →
zenodo32/100

Figure files for Coherent spin-valley oscillations in silicon

<p>This repository contains .fig (matlab) files corresponding to the figures in&nbsp;Coherent spin-valley oscillations in silicon.</p>

opencc-by-4.0Oct 2022View details →
zenodo32/100

Tulul adh-Dhahab, Zarqa Valley - MapBox imagery

Landscape around the lower Zarqa river valley, from the foothills of the West Bank to the Jordan Highlands, including the Jordan Valley, the Ghor al-Urdun. In the center of the map the Tulul adh-Dhahab (https://en.wikipedia.org/wiki/Tulul_adh-Dhahab). * Generator: [DEM Net Elevation API](https://elevationapi.com) * Digital Elevation Model: [SRTM_GL1 OpenTopography](https://opentopography.org/) * Imagery: [MapBox Satellite](https://www.mapbox.com) Source: Objaverse 1.0 / Sketchfab

opencc-by-nc-sa-2.0Jul 2020View details →

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allen-brain-atlas
neuroscienceopenDocumentation, web resources, and API references are available online.
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dandi-nwb
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Last verified 2026-04-30Open record

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Last verified 2026-04-29Open record

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