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380 results for “Rifting”
Water Erosion Risk Assessment in the Eastern Rift Valley: The Case of Kenya Great Rift Valley Region
<p>RUSLE Supplementary Materials </p> <p> </p> <p>Water Erosion Risk Assessment in the Eastern Rift Valley: The Case of Kenya Great Rift Valley Region</p>
Gravity and magnetotelluric data in the Asal Rift, Republic of Djibouti
<p>Gravity data were obtained from a gravity survey carried out by BRGM between 1979 and 1980. Magnetotelluric data were produced in 2007 (Árnason et al, 2008, Khodayar, 2008) in collaboration with Iceland Geosurvey (ISOR), Reykjavik Energy Invest (REI) and the Centre d'Etude et de Recherche de Djibouti (CERD).</p>
TABLE 1 in A new species of the thorid shrimp genus Lebbeus White, 1847 (Decapoda: Caridea) from the Amami Rift hydrothermal vent field in the Ryukyu region, Japan
<p><b>TABLE 1.</b> GenBank accession numbers of the mitochondrial COI and 16S rRNA gene sequences from species of <i>Lebbeus</i> used for genetic analyses. *Registered as <i>Lebbeus carinatus</i> de Saint Laurent, 1984 in GenBank.</p><table><tbody><tr><th>Species</th><th>COI</th><th>16S</th></tr></tbody><tbody><tr><th><i>Lebbeus altus</i> Komai, Chang & Chan, 2021</th><td>MZ742156, MZ742157</td><td>-</td></tr><tr><th><i>Lebbeus antarcticus</i> Hale, 1941</th><td>KC494749–KC494752</td><td>-</td></tr><tr><th><i>Lebbeus brevicornis</i> Komai, 2011</th><td>LC831371</td><td>LC831221</td></tr><tr><th><i>Lebbeus compressus</i> (Yokoya, 1933)</th><td>MZ742158, MZ742159</td><td>LC699546</td></tr><tr><th><i>Lebbeus cultrirostris</i> Wang, Sha & Sun, 2023</th><td>OP580068</td><td>OP578210</td></tr><tr><th><i>Lebbeus formosus</i> Komai, Chang & Chan, 2010</th><td>MK409684</td><td>KF023087</td></tr><tr><th><i>Lebbeus fujimotoi</i> Matsuzaki, Hibino & Komai, 2016</th><td>LC699876, LC699877</td><td>LC699547</td></tr><tr><th><i>Lebbeus grandimanus</i> (Bražnikov, 1907)</th><td>MN138399</td><td>-</td></tr><tr><th><i>Lebbeus groenlandicus</i> (Fabricius, 1775)</th><td>DQ882082–DQ882884, FJ581737,</td><td>-</td></tr><tr><th>MG310744, MG312804, MG314359,</th></tr><tr><th>MG314559, MG315672, MG317214,</th></tr><tr><th>MG319295, MG319690, MG319934,</th></tr><tr><th>MG320381, MG320565, MG321028,</th></tr><tr><th></th><td>MG936123, MH242822</td><td></td></tr><tr><th><i>Lebbeus jaolongi</i> (Xu, Liu, Ding & Wang, 2016)</th><td>MH398092</td><td>MH398078</td></tr><tr><th><i>Lebbeus java</i> Komai, Chang & Chan, 2019</th><td>MK409683</td><td>-</td></tr><tr><th><i>Lebbeus kexuei</i> Wang, Sha & Sun, 2023</th><td>OP580069</td><td>OP578211</td></tr><tr><th><i>Lebbeus kiae</i> Schiaparelli, Ahyong & Bowden, 2015</th><td>KT187237–KT187243</td><td>-</td></tr><tr><th><i>Lebbeus laurentae</i> Wicksten, 2010 *</th><td>AF125421</td><td>-</td></tr><tr><th><i>Lebbeus longidactylus</i> (Kobjakova, 1936)</th><td>LC699878</td><td>LC699548</td></tr><tr><th><i>Lebbeus longipes</i> (Kobjakova, 1936)</th><td>LC699879</td><td>LC699549</td></tr><tr><th><i>Lebbeus parvirostris</i> <b>sp. nov.</b></th><td>LC831370</td><td>LC831220</td></tr><tr><th><i>Lebbeus polaris</i> (Sabine, 1824)</th><td>FJ581738, FJ581739, HM425371,</td><td>KP725539, KP772540</td></tr><tr><th>HQ966810, KP759419, KP759420,</th></tr><tr><th>MG310343, MG311624, MG311072,</th></tr><tr><th>MG312952, MG312957, MG313605,</th></tr><tr><th>MG314788, MG315175, MG315873,</th></tr><tr><th>MG316672, MG317268, MG317301,</th></tr><tr><th>MG317705, MG317885, MG318148,</th></tr><tr><th>MG318608, MG318898, MG319773,</th></tr><tr><th>MG319844, MG319853, MG319864,</th></tr><tr><th>MG320139, MG320699, MG321050,</th></tr><tr><th>MG935131, MG935282</th></tr><tr><th><i>Lebbeus rufomaculosus</i> Komai & Matsuzaki, 2022</th><td>LC699872</td><td>LC699542</td></tr><tr><th><i>Lebbeus shinkaiae</i> Komai, Tsuchida & Segonzac,</th><td>MH398097</td><td>MH398083</td></tr><tr><th>2012</th><td></td><td></td></tr><tr><th><i>Lebbeus sokhobio</i> Marin, 2020</th><td>MN590012–MN590015, MN608153–</td><td>-</td></tr><tr><th>MN608155</th></tr><tr><th><i>Lebbeus subtilis</i> Komai & Matsuzaki, 2022</th><td>LC699873</td><td>LC699543</td></tr><tr><th><i>Lebbeus tenuipes</i> Komai & Matsuzaki, 2022</th><td>LC699874, LC699875</td><td>LC699544, LC699545</td></tr><tr><th><i>Lebbeus unalaskensis</i> (Rathbun, 1902)</th><td>-</td><td>LC699550</td></tr><tr><th><i>Lebbeus virentova</i> Nye, Copley, Plouviez & Van</th><td>JQ837265, KJ566966</td><td>KM979548</td></tr><tr><th>Dover, 2012</th></tr></tbody></table>
Fig. 1 in Deepest known novel species of the genus Ophiuroglypha Hertz, 1927 (Echinodermata: Ophiuroidea) from the central rift zone, Philippine Sea
Fig. 1. Map of collecting station of the central rift zone, Philippine Sea, in this study.
Rift Valley Fever in Kenya
ClinicalTrials.gov study NCT00287014. IPD Sharing: Not stated. Countries: 1. Publications: 0.
Safety and Immunogenicity Study of Rift Valley Fever Vaccine, Inactivated
ClinicalTrials.gov study NCT00869713. IPD Sharing: Not stated. Countries: 1. Publications: 0.
Phase 2 Safety and Immunogenicity Study of Rift Valley Fever Vaccine
ClinicalTrials.gov study NCT03609398. IPD Sharing: NO. Countries: 1. Publications: 0.
Safety and Immunogenicity of a Candidate Rift Valley Fever Vaccine (RVF003)
ClinicalTrials.gov study NCT06799234. IPD Sharing: NO. Countries: 1. Publications: 0.
Comparison of MBT/Pas and BALB/cByJ MEFs response after infection with Rift Valley Fever virus
GEO Series GSE18064. Mus musculus. 12 samples. Type: Expression profiling by array.
Distribution. From Senegal and Gambia to N Ethiopia and Eritrea, and S to Zambia;; isolated populations exist in S Gabon, W Republic of the Congo, and Angola. The Rift Valley in C Kenya and C Tanzania forms the E distributionallimit; distribution to the S is restricted by the Muchinga escarpment in Zambia. in Bovidae
Distribution. From Senegal and Gambia to N Ethiopia and Eritrea, and S to Zambia;; isolated populations exist in S Gabon, W Republic of the Congo, and Angola. The Rift Valley in C Kenya and C Tanzania forms the E distributionallimit; distribution to the S is restricted by the Muchinga escarpment in Zambia.
Distribution. From Lake Chad to E Sudan and possibly just into Ethiopia, SE to the borders of the East African Rift Valley, S to the Uasin Gishu Plateau in Kenya and to Ankole in Uganda. in Bovidae
Distribution. From Lake Chad to E Sudan and possibly just into Ethiopia, SE to the borders of the East African Rift Valley, S to the Uasin Gishu Plateau in Kenya and to Ankole in Uganda.
Subspecies and Distribution. C.h.hamlyniPocock,1907—EDRCongo,fromthelowlandsoftheRiverLualabaEtoIturiForestandtheAlbertineRiftinWRwanda(NyungweForestNationalPark),andextendingNtotheLindi-Nepokosystem,andStothelimitoftherainforest(poorlydefined);possiblyfoundinSUgandaandNBurundi. C. h. kahuziensis Colyn & Rahm, 1987 — E DR Congo, Mt. Kahuzi in the Albertine Rift Mts. in Cercopithecidae
Subspecies and Distribution. C.h.hamlyniPocock,1907—EDRCongo,fromthelowlandsoftheRiverLualabaEtoIturiForestandtheAlbertineRiftinWRwanda(NyungweForestNationalPark),andextendingNtotheLindi-Nepokosystem,andStothelimitoftherainforest(poorlydefined);possiblyfoundinSUgandaandNBurundi. C. h. kahuziensis Colyn & Rahm, 1987 — E DR Congo, Mt. Kahuzi in the Albertine Rift Mts.
FIGURE 10 in Systematics of the Central African Spiny Reed Frog Afrixalus laevis (Anura Hyperoliidae), with the description of two new species from the Albertine Rift
FIGURE 10. Total call length (diamonds; five-note advertisement calls only) and energy maximum of dominant frequency (triangles) of the advertisement call of Afrixalus phantasma sp. nov. at varying ambient temperatures.
FIGURE 4. A in Systematics of the Central African Spiny Reed Frog Afrixalus laevis (Anura Hyperoliidae), with the description of two new species from the Albertine Rift
FIGURE 4. A species-level divergence dating analysis of the hyperoliid genus Afrixalus generated with BEAST, based on the concatenated 16S and RAG1 genes. Each of the four samples of Afrixalus laevis shown in boldface were supported as distinct species in Bayesian species-delimitation (BPP) analyses.
FIGURE 12 in Taxonomy of the Rhampholeon boulengeri Complex (Sauria: Chamaeleonidae): Five New Species from Central Africa's Albertine Rift
FIGURE 12. Photographs of various individuals of Rhampholeon bombayi sp. nov. in life. (A)—Adult female holotype (UTEP 21701) from Kalundu, DRC; (B)—Adult female (UTEP 21705) from the vicinity of Irangi, DRC; (C)—Adult male (UTEP 21706) from the vicinity of Tumungu, DRC; (D)—Adult female (UTEP 22690) from Nyungwe Forest National Park, Rwanda; (E, F)—Adult male (UTEP 22691) from Nyungwe Forest National Park, Rwanda; (G)—Habitat view of the forest at the type locality; (H)—Habitat view of the forest at Tumungu, DRC.
FIGURE 1 in A new species of the palaearctic genus Dasypoda Latreille 1802 (Hymenoptera: Dasypodaidae) from the Great Rift Valley in Ethiopia
FIGURE 1. Distribution of Dasypodaidae and locus typicus (07°59'47"N 38°38'46"E) of Dasypoda riftensis sp. nov. (Dasypodaini: Samba and Dasypoda; Hesperapini: Capicola, Eremaphanta and Hesperapis).
Switzerland 2022 Field Campaign - 360 degree Alpine Tethys rifted margin outcrops
<p>360 degree photospheres acquired during the summer data acquisition campaign targeting the pristine remnant outcrops of the Alpine Tethys rifted margins that are exposed in the Swiss Alps</p>
Supplementary Movies for Pérez-Gussinyé et al. (2023) Synrift and postrift thermal evolution of rifted margins: a re-evaluation of classic models of extension Accepted in GSL Special Publications
<p>Movie S1. Evolution of deformation for the three models shown in Figures 2 and 3. Full extension rate is 10 mm/yr. Sedimentation rate is given in Figures 2 and 3 and Methods (see also Table 1). Red shading shows brittle strain rate, blue shading shows ductile strain rate. The sediments are color coded with age since the start of rifting. The color circles are trackers. The color conventions for the phases are the same as in Figures 1 and 2.</p><p> </p><p>Movie S2. Top: Thermal evolution of the 10 mm/yr full rifting velocity model without sedimentation along with markers (model shown in Figures 2a-e and 3a-c). Grey shading indicates strain rate. Note the development of small scale convection cells. Middle: Evolution of the basement heat flow of markers shown in top panel. Bottom: Evolution of the basement temperature at markers shown in top panel. Note that the horizontal and vertical scale change in the postrift to better show the small scale convection in the top panel.</p><p> </p><p>Movie S3. Top: Thermal evolution of the10 mm/yr full rifting velocity model with average sedimentation along with markers (model shown in Figures 2f-j and 3d-g). Grey shading indicates strain rate. Note the development of small scale convection cells. Middle: Evolution of the basement heat flow of markers shown in top panel. Bottom: Evolution of the basement temperature at markers shown in top panel. Note that the horizontal and vertical scale change in the postrift to better show the small scale convection in the top panel.</p><p> </p><p>Movie S4. Top: Thermal evolution of the 10 mm/yr full rifting velocity model </p><p>with largest sedimentation along with markers (model shown in Figures 2k-o and 3h-k). Grey shading indicates strain rate. Note the development of small scale convection cells. Middle: Evolution of the basement heat flow of markers shown in top panel. bottom: Evolution of the basement temperature at markers shown in top panel. Note that the horizontal and vertical scale change in the postrift to better show the small scale convection in the top panel.</p><p> </p><p> </p><p>Movie S5. Evolution of temperature field for the 10 mm/yr full rifting velocity without sedimentation, (model shown in Figures 2a-e and 3a-c). b) and c) show the geotherms of trackers shown in a) computed from the dynamic model (solid colored lines), and from the ´1-D temperature´ solution (dashed colored lines). The black curve shows the initial geotherm used for the dynamic temperature and for the ´1-D temperature´ calculations. Grey shading indicates strain rate. Note that the horizontal scale is changing to show the rifted margins as the model evolves.</p><p> </p><p>Movie S6. Evolution of temperature field for the 100 mm/yr full rifting model without sedimentation, (model shown in Figures 2a-e and 3a-c). b) and c) show the geotherms of trackers shown in a) computed from the dynamic model (solid colored lines), and from the ´1-D temperature´ solution (dashed colored lines). The black curve shows the initial geotherm used for the dynamic temperature and for the ´1-D temperature´ calculations. Grey shading indicates strain rate. Note that the horizontal scale is changing to show the rifted margins as the model evolves.</p>
Supplementary Datasets for: Chapter 6: Timescales of dyke intrusion events in the Main Ethiopian Rift through olivine Fe-Mg diffusion chronometry
<p>Supplementary datasets for Chapter 6: Timescales of dyke intrusion events in the Main Ethiopian Rift through olivine Fe-Mg diffusion chronometry.</p> <p>Dataset S1: Standards, secondary standards, geochemical data and timescale data of olivine Fe-Mg diffusion profiles and carrier glasses.<br> Dataset S2: Combined and sorted dataset of greyscale images.</p>
Analogue modelling of plate rotation effects in transform margins and rift-transform intersections.
<p>Raw data for the manuscript titled "Analogue modelling of plate rotation effects in transform margins and rift-transform intersections." to the AGU journal Tectonics.</p>
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