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36 results for “isolation basin”
Distribution. Widespread in Mediterranean Basin from Iberian Peninsula and associated Is E through S Europe to Balkans, Caucasus, and Middle East; in North Africa in Morocco, Algeria, Tunisia, Libya, and Egypt as far S as S Sinai; from Middle East, range continues patchily E into regions surrounding Black and Caspian seas, including Iran, Turkmenistan, Uzbekistan, SE Kazakhstan, Kyrgyzstan, Tajikistan, and Afghanistan, and then finally in two isolated populations in E Nepal and N Myanmar; also Canary Is. in Molossidae
Distribution. Widespread in Mediterranean Basin from Iberian Peninsula and associated Is E through S Europe to Balkans, Caucasus, and Middle East; in North Africa in Morocco, Algeria, Tunisia, Libya, and Egypt as far S as S Sinai; from Middle East, range continues patchily E into regions surrounding Black and Caspian seas, including Iran, Turkmenistan, Uzbekistan, SE Kazakhstan, Kyrgyzstan, Tajikistan, and Afghanistan, and then finally in two isolated populations in E Nepal and N Myanmar; also Canary Is.
Distribution. Widely distributed throughout much of sub-Saharan Africa, from Senegal in W to Ethiopia and Somalia in E, S to South Africa (but absent from most of Congo Basin), and N along Nile River through Sudan to Egypt and across to Israel and Jordan; there is an isolated population in Morocco and another one on W coast of Saudi Arabia along Red Sea S to Yemen. in Nycteridae
Distribution. Widely distributed throughout much of sub-Saharan Africa, from Senegal in W to Ethiopia and Somalia in E, S to South Africa (but absent from most of Congo Basin), and N along Nile River through Sudan to Egypt and across to Israel and Jordan; there is an isolated population in Morocco and another one on W coast of Saudi Arabia along Red Sea S to Yemen.
Subspecies and Distribution. pos sagitta Pallas, 1773 — S Russia (Altai Krai) and right bank of Irtysh River in Kazakhstan (Pavlodar and East Kazakhstan regions). D.s.aksuensisWangSung,1964—NWChina(NTarimBasininXinjiang). D.s.austrouralensisShenbrot,1991—NWKazakhstan(WestKazakhstan,Atyrau,andAktoberegionsbetweenUralandEmbarivers). D.s.bulganensisShenbrot,1991—EKazakhstan(ELakeZaysaninEastKazakhstanRegion),NWChina(DzungarianBasininXinjiang),andMongolia(SKhovdandSWGovi-Altai). D.s.deasyiBarret-Hamilton,1900—NWChina(STarimBasininXinjiangandS&WQaidamBasininQinghai). D. s. fuscocanus Wang Sung, 1964 — W China (S foothills of E Tian Shan in Xinjiang). D. s. halli Sowerby, 1920 — China (NE Inner Mongolia [= Nei Mongol], SW Heilongjiang, NWJilin, and N Liaoning) and SE Mongolia (Stikhbaatar). D. s. innae Ognev, 1930 — S Russia (Astrakhan Region E of Volga River) and NW Kazakhstan (West Kazakhstan and Atyrau regions W of Ural River). D. s. lagopus Lichtenstein, 1823 — WC Kazakhstan (E of Emba and N of Syrdarya rivers). D. s. megacranius Shenbrot, 1991 — SE Kazakhstan (Moinkum Sands in Jambyl Region). D. s. nogai Satunin, 1907 — S European Russia (Volgograd and Astrakhan regions E of Volga River, Kalmykia, and Dagestan). D. s. sowerbyi Thomas, 1908 — N China (NE Xinjiang, N Qaidam Basin in Qinghai, Gansu, SW Inner Mongolia, N Ningxia, and N Shaanxi) and Mongolia. D. s. turanicus Shenbrot, 1991 — SW Kazakhstan (S Kyzylorda S of Syrdarya River and Mangystau regions), Uzbekistan, and Turkmenistan; it probably occurs in adjacent W Afghanistan. D. s. ubsanensis Bannikov, 1947 — NW Mongolia (N Uvs) and adjacent Russia (extreme S Tuva). D. s. usuni Shenbrot, 1991 — SE Kazakhstan (Almaty Region); it probably occurs in adjacent China (sands of Ili Valley of W Xinjiang). D. s. zaissanensis Selevin, 1934 — E Kazakhstan (NW Lake Zaysan Basin on the left bank of Irtysh River). Isolated population in N Iran (Turan Desert in E Semnan Province) may belong to turanicus or correspond to a yet undescribed subspecies. in Dipodidae
Subspecies and Distribution. pos sagitta Pallas, 1773 — S Russia (Altai Krai) and right bank of Irtysh River in Kazakhstan (Pavlodar and East Kazakhstan regions). D.s.aksuensisWangSung,1964—NWChina(NTarimBasininXinjiang). D.s.austrouralensisShenbrot,1991—NWKazakhstan(WestKazakhstan,Atyrau,andAktoberegionsbetweenUralandEmbarivers). D.s.bulganensisShenbrot,1991—EKazakhstan(ELakeZaysaninEastKazakhstanRegion),NWChina(DzungarianBasininXinjiang),andMongolia(SKhovdandSWGovi-Altai). D.s.deasyiBarret-Hamilton,1900—NWChina(STarimBasininXinjiangandS&WQaidamBasininQinghai). D. s. fuscocanus Wang Sung, 1964 — W China (S foothills of E Tian Shan in Xinjiang). D. s. halli Sowerby, 1920 — China (NE Inner Mongolia [= Nei Mongol], SW Heilongjiang, NWJilin, and N Liaoning) and SE Mongolia (Stikhbaatar). D. s. innae Ognev, 1930 — S Russia (Astrakhan Region E of Volga River) and NW Kazakhstan (West Kazakhstan and Atyrau regions W of Ural River). D. s. lagopus Lichtenstein, 1823 — WC Kazakhstan (E of Emba and N of Syrdarya rivers). D. s. megacranius Shenbrot, 1991 — SE Kazakhstan (Moinkum Sands in Jambyl Region). D. s. nogai Satunin, 1907 — S European Russia (Volgograd and Astrakhan regions E of Volga River, Kalmykia, and Dagestan). D. s. sowerbyi Thomas, 1908 — N China (NE Xinjiang, N Qaidam Basin in Qinghai, Gansu, SW Inner Mongolia, N Ningxia, and N Shaanxi) and Mongolia. D. s. turanicus Shenbrot, 1991 — SW Kazakhstan (S Kyzylorda S of Syrdarya River and Mangystau regions), Uzbekistan, and Turkmenistan; it probably occurs in adjacent W Afghanistan. D. s. ubsanensis Bannikov, 1947 — NW Mongolia (N Uvs) and adjacent Russia (extreme S Tuva). D. s. usuni Shenbrot, 1991 — SE Kazakhstan (Almaty Region); it probably occurs in adjacent China (sands of Ili Valley of W Xinjiang). D. s. zaissanensis Selevin, 1934 — E Kazakhstan (NW Lake Zaysan Basin on the left bank of Irtysh River). Isolated population in N Iran (Turan Desert in E Semnan Province) may belong to turanicus or correspond to a yet undescribed subspecies.
Distribution. Most of the Great Basin and some of the adjacent intermountain areas of W USA,from SE Oregon and NE California through most of C & N Nevada to S Idaho, extreme SW Montana, extreme W Wyoming, and W Utah. An isolated reintroduced population exists in WC Washington. in Leporidae
Distribution. Most of the Great Basin and some of the adjacent intermountain areas of W USA,from SE Oregon and NE California through most of C & N Nevada to S Idaho, extreme SW Montana, extreme W Wyoming, and W Utah. An isolated reintroduced population exists in WC Washington.
Distribution. Upper Amazon Basin in E Colombia (N as far as the Rio Arauca on the Venezuelan border; an isolated population in the upper Rio Magdalena in the Huila Department), E Ecuador, E Peru, W Brazil, and C & N Bolivia (S at least to the upper Rio Beni); the exact limits of its distribution have not been delineated, and particularly where they meet those of the Guianan Brown Capuchin (S. apella) in the Rio Madeira Basin, in the N along the Orinoco, and in the interfluvium of the Rio Solimoes and upper Rio Negro. in Cebidae
Distribution. Upper Amazon Basin in E Colombia (N as far as the Rio Arauca on the Venezuelan border; an isolated population in the upper Rio Magdalena in the Huila Department), E Ecuador, E Peru, W Brazil, and C & N Bolivia (S at least to the upper Rio Beni); the exact limits of its distribution have not been delineated, and particularly where they meet those of the Guianan Brown Capuchin (S. apella) in the Rio Madeira Basin, in the N along the Orinoco, and in the interfluvium of the Rio Solimoes and upper Rio Negro.
Distribution. Restricted to three small isolated areas in the lower Amur River Basin of Russian Far East (Upper Bureya River Depression, Chukchagyr-Evoron lakes Depression, adjacent parts of Amgun River Valley, and Upper Zeya River Depression). in Cricetidae
Distribution. Restricted to three small isolated areas in the lower Amur River Basin of Russian Far East (Upper Bureya River Depression, Chukchagyr-Evoron lakes Depression, adjacent parts of Amgun River Valley, and Upper Zeya River Depression).
Distribution. Great Basin in EC California and SW Nevada as well as an isolated record from WC Utah (SW USA). in Soricidae
Distribution. Great Basin in EC California and SW Nevada as well as an isolated record from WC Utah (SW USA).
Distribution. Widely distributed in Congo Basin and Albertine Rift from the Niger River in W to shores of Lake Victoria in E; an isolated population occurs in NW Zambia and neighboring DR Congo. in Muridae
Distribution. Widely distributed in Congo Basin and Albertine Rift from the Niger River in W to shores of Lake Victoria in E; an isolated population occurs in NW Zambia and neighboring DR Congo.
FIGURE 1 in Discovery of isolated leaves of Marskea (Taxaceae) in the Middle Jurassic sediments of Irkutsk Basin (East Siberia, Russia)
FIGURE 1. Map of the Marskea cuspidata leafs location on the right side of the Irkutsk reservoir ().
FIGURE 3. Marskea cuspidata leaf structure. A, E, F in Discovery of isolated leaves of Marskea (Taxaceae) in the Middle Jurassic sediments of Irkutsk Basin (East Siberia, Russia)
FIGURE 3. Marskea cuspidata leaf structure. A, E, F. Cells of the stomatal bands. Flat papillae on periclinal walls are shown by arrows. A. Specimen no. 19-11/8-3. E. External view on SEM, specimen no. 19-11/7 holotype. F. Specimen no. 19-11/7 holotype. B. Lower surface of the epidermis, external view on SEM, specimen no. 19-11/7 holotype. C. Cells of the marginal non-stomatal zone (left) and the stomatal band (right), internal view on SEM, specimen no. 19-11/9-1. D. Cells of the marginal non-stomatal zone, external view on SEM, specimen no. 19-11/7 holotype. G, J, M. Stomatal complexes with proximal papillae. G. Specimen no. 19-11/7 holotype. J. External view on SEM, specimen no. 19-11/7 holotype. M. Specimen no. 19-11/8. H, I, K. Stomatal complexes with cuticular ring around stomatal pit. H. Specimen no. 19-11/8. I. Specimen no. 19-11/6. K. External view on SEM, specimen no. 19-11/7 holotype. L. Adjacent stomatal complexes, specimen no. 19-11/6. N, O. Stomatal complexes, internal view on SEM, specimen no. 19-11/7 holotype.
FIGURE 2. Marskea cuspidata leaf structure. A. Leafs and fragments thereof. A in Discovery of isolated leaves of Marskea (Taxaceae) in the Middle Jurassic sediments of Irkutsk Basin (East Siberia, Russia)
FIGURE 2. Marskea cuspidata leaf structure. A. Leafs and fragments thereof. A*. Specimen no. 19-11/7 holotype. B. Upper surface of the epidermis, specimen no. 19-11/7 holotype. C. Cells of the upper epidermis, specimen no. 19-11/4. D. Cells of the upper epidermis, internal view on SEM, specimen no. 19-11/7 holotype. E. Cells of the upper epidermis, specimen no. 19-11/9-1. Flat papillae on periclinal walls are shown by arrows. F, G. Lower surface of the epidermis with two stomatal bands, specimen no. 19-11/7 holotype. H. Cells of lower surface between stomatal band and leaf edge, specimen no. 19-11/7 holotype. I. Fragment of lower surface with stomatal band and central non-stomatal zone. A horizontal row of adjacent stomatal complexes is shown by arrow, specimen no. 19-11/7 holotype.
Data from: Examination of a historic collection of isolated cranial and appendicular hadrosaurid material from the lower Kirtland Formation of the San Juan Basin, New Mexico
Open the record for dataset details and reuse information.
FIGURE 2 in Genetic differentiation through dispersal and isolation in two freshwater fish species from coastal basins of Northeastern Brazil
FIGURE 2 | Distribution and haplotype structure of Schizodon dissimilis. A. Paleodrainage reconstruction of coastal basins from northeastern Brazil and geographic distribution of groups defined by SAMOVA. B. Estimate of the probable groups of populations produced by the BAPS. C. Haplotypes network of cytochrome oxidase I (coI). All analysis recovered a total of three groups in this area. The colors used to highlight areas in the network correspond to populations in map.
FIGURE 1 in Genetic differentiation through dispersal and isolation in two freshwater fish species from coastal basins of Northeastern Brazil
FIGURE 1 | Species used in this study, Schizodon dissimilis (above) and Prochilodus lacustris (below).
Fig. 1 in A report of 22 unrecorded bacterial species in Korea, isolated from the North Han River basin in 2017
Fig. 1. Neighbor-joining phylogenetic tree based on 16S rRNA gene sequences showing the relationship between the strains isolated in this study and their closest relatives. Bootstrap values (expressed as percentages of 1000 replications) over 70% are shown at nodes for neighbor-joining, maximum parsimony, and maximum likelihood methods, respectively. Filled circles indicate that the corresponding nodes were also recovered in the trees generated with the maximum-likelihood and maximum-parsimony algorithms, while open circles indicate that the corresponding nodes were also recovered in the tree generated with one of these algorithms. Bar, 0.05 substitutions per nucleotide position.
Lofoten-Vesterålen Isolation basin sediment geochemical data (B
<p>Sediment geochemical data from isolation basin records from the Lofoten-Vesterålen archipelagos, northern Norway</p>
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