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496 results for “Tibetan Plateau”
In-situ lake level observations on the western Tibetan Plateau
<p>Lake level has been monitored at six lakes (Lumajiangdong Co, Memar Co, Jieze Caka, Longmu Co, Luotuo Lake, Aksaiqin Lake) on the western TP. HOBO water level loggers (U20-001-01) or Solist water level loggers were installed in the littoral zone of the lakes. To validate lake level changes, two HOBO water-level loggers were installed in different regions of Lumajiangdong Co (Fig. S1). Because water levels were recorded as changes in pressure (less than 0.5 cm water level equivalent), air pressure data were subtracted from the level loggers to obtain pressure changes related to water column variations. The loggers can still work efficiently at the beginning of ice cover. However, there is no data available when the lake ice was thick enough and loggers were frozen up. Daily lake-level changes were used in this study. At Lumajiangdong Co, lake level data are available between October 2016 and September 2021. At Memar Co, lake level data are only available between October 2017 and September 2019 and between October 2020 and September 2021. For Jieze Caka, Longmu Co and Luotuo Lake, there is only one year’s data available. Water depth of the loggers was measured during fieldwork to validate the logger data.</p>
Distribution. The Chiru is endemic to the Tibetan Plateau in the Chinese provinces of Xinjiang, Qinghai, and Xizang; it also occurs in very small numbers in the Ladakh district of NW India, mainly during summer. in Bovidae
Distribution. The Chiru is endemic to the Tibetan Plateau in the Chinese provinces of Xinjiang, Qinghai, and Xizang; it also occurs in very small numbers in the Ladakh district of NW India, mainly during summer.
Distribution. Fragmented distribution in the Tibetan Plateau in China (Xinjiang, Xizang & Qinghai); one population drifts from S Xinjiang into NW India (Ladakh) and another from Qinghai to Gansu, China. in Bovidae
Distribution. Fragmented distribution in the Tibetan Plateau in China (Xinjiang, Xizang & Qinghai); one population drifts from S Xinjiang into NW India (Ladakh) and another from Qinghai to Gansu, China.
Distribution. Patchily distributed in NE and E periphery of the Tibetan Plateau (Qilian, Burhan Budai, Amne Machin, and Bayan Har Mts) in Qinghai, Gansu, and NW Sichuan, China. in Ochotonidae
Distribution. Patchily distributed in NE and E periphery of the Tibetan Plateau (Qilian, Burhan Budai, Amne Machin, and Bayan Har Mts) in Qinghai, Gansu, and NW Sichuan, China.
Subspecies and Distribution. O.c.curzoniaeHodgson,1858—S&EpartsofTibetanPlateau(China)andadjoiningNIndia(Sikkim);probablyalsoinextremeNNepal. O. c. melanostoma Buchner, 1890 — N & W parts of Tibetan Plateau, E to Mts adjoining Qinghai Lake (China). in Ochotonidae
Subspecies and Distribution. O.c.curzoniaeHodgson,1858—S&EpartsofTibetanPlateau(China)andadjoiningNIndia(Sikkim);probablyalsoinextremeNNepal. O. c. melanostoma Buchner, 1890 — N & W parts of Tibetan Plateau, E to Mts adjoining Qinghai Lake (China).
Subspecies and Distribution. O.n.nubricaThomas,1922—LadakhandupperIndusValley(NIndia)andwaterdivideofupperGangesandBrahmaputrariversinNNepalandSTibetanPlateau. O. n. lhasaensis Feng Zuojian & Kao Yuehting, 1974 — E Tibetan Plateau, in the left bank of middle Brahmaputra River, E Xizang, China. in Ochotonidae
Subspecies and Distribution. O.n.nubricaThomas,1922—LadakhandupperIndusValley(NIndia)andwaterdivideofupperGangesandBrahmaputrariversinNNepalandSTibetanPlateau. O. n. lhasaensis Feng Zuojian & Kao Yuehting, 1974 — E Tibetan Plateau, in the left bank of middle Brahmaputra River, E Xizang, China.
Subspecies and Distribution. L.o.owostolusHodgson,1840—WTibetanPlateau(79°Eto92°E). L.o.hypsibiusBlanford,1875—JammuandKashmir(NWIndia),UpperSutlejValley(SWXizang,China). L.o.pallipesHodgson,1842—C&ETibetanPlateau,NNepal,Sikkim(NEIndia);possiblyalsoinNBhutan. L. o. przewalskii Satunin, 1907 — NE & E Tibetan Plateau to Qinghai, Gansu, Sichuan, and N Yunnan (China). in Leporidae
Subspecies and Distribution. L.o.owostolusHodgson,1840—WTibetanPlateau(79°Eto92°E). L.o.hypsibiusBlanford,1875—JammuandKashmir(NWIndia),UpperSutlejValley(SWXizang,China). L.o.pallipesHodgson,1842—C&ETibetanPlateau,NNepal,Sikkim(NEIndia);possiblyalsoinNBhutan. L. o. przewalskii Satunin, 1907 — NE & E Tibetan Plateau to Qinghai, Gansu, Sichuan, and N Yunnan (China).
A dataset of sulfur content and density of vegetation on the Tibetan Plateau
<p>As an important part of China's terrestrial ecosystem, the variation and distribution of sulfur in the vegetation of the Tibetan Plateau (TP) will have a profound impact on the national and even global sulfur cycle. We collected and sorted out the field survey and test data of the research group from 2019 to 2020. This dataset encompasses forest, grassland, shrubland, desert and other major ecosystem types, including the average sulfur content, density and storage data of different vegetation types and plant organs. The establishment of this data set provides important basic data for the assessment of regional vegetation biomass and sulfur reserves and the optimization of sulfur cycle model.</p>
Subspecies and Distribution. A. s. stoliczkanus Blanford, 1875 — N Pakistan and NW India. A. s. bhatnagari Biswas & Khajuria, 1955 — Himalaya in Nepal, NE India (Sikkim), and possibly N Buthan. A. s. lama Barrett-Hamilton, 1900 — the entire Tibetan Plateau. in Cricetidae
Subspecies and Distribution. A. s. stoliczkanus Blanford, 1875 — N Pakistan and NW India. A. s. bhatnagari Biswas & Khajuria, 1955 — Himalaya in Nepal, NE India (Sikkim), and possibly N Buthan. A. s. lama Barrett-Hamilton, 1900 — the entire Tibetan Plateau.
Distribution. Tibetan Plateau of W China (Xinjiang, Qinghai, and Xizang), NW India (Jammu and Kashmir and Himachal Pradesh), and N Nepal. in Cricetidae
Distribution. Tibetan Plateau of W China (Xinjiang, Qinghai, and Xizang), NW India (Jammu and Kashmir and Himachal Pradesh), and N Nepal.
Distribution. High mountains of C China in Qinghai, S Gansu, NE Tibetan Plateau, W Sichuan, and NW Yunnan. in Cricetidae
Distribution. High mountains of C China in Qinghai, S Gansu, NE Tibetan Plateau, W Sichuan, and NW Yunnan.
Distribution. Disjunct distribution in E Himalayas from C & E Nepal through Sikkim and extreme N West Bengal (NE India) to Bhutan and S Tibetan Plateau (S China). in Cricetidae
Distribution. Disjunct distribution in E Himalayas from C & E Nepal through Sikkim and extreme N West Bengal (NE India) to Bhutan and S Tibetan Plateau (S China).
Subspecies and Distribution. A.l.stoliczkanusBlanford,1875—NPakistanandNWIndia. A.l.bhatnagariBiswas&Khajuria,1955—HimalayainNepal,NEIndia(Sikkim),andpossiblyNButhan. A. l. lama Barrett-Hamilton, 1900 — the entire Tibetan Plateau. in Cricetidae
Subspecies and Distribution. A.l.stoliczkanusBlanford,1875—NPakistanandNWIndia. A.l.bhatnagariBiswas&Khajuria,1955—HimalayainNepal,NEIndia(Sikkim),andpossiblyNButhan. A. l. lama Barrett-Hamilton, 1900 — the entire Tibetan Plateau.
Less-well-developed crustal flow in the central Tibetan Plateau revealed by receiver function and surface wave joint inversion
<p>A crustal flow model has been previously used to explain the crustal extension of the Tibetan Plateau. However, the existence of massive crustal flow in the central plateau is still controversial. We conducted a joint inversion of receiver functions and surface wave dispersions from the 2-D broadband seismic array SANDWICH deployed in the central plateau. The crustal S-wave velocity structure with high vertical resolution shows a low-velocity layer (LVL) in the middle-lower crust beneath most stations. The S-wave velocity of this LVL is mostly within 3.0-3.4 km/s, reflecting a melt volume percentage (MVP) ≤ 7%, except at two stations. Our study suggests that there is not a high enough melt volume in central Tibet to develop crustal flow, which requires an MVP ≥ 7% to decrease rock strength. The formation of extensional structures in the central plateau may contribute to ductile deformation in the middle-lower crust but not crustal flow.</p>
CH4 and CO2 dataset for the Qinghai-Tibetan Plateau rivers
<p>该数据集整理了青藏高原河流CH4和CO2浓度和通量的直接现场测量值,以及28个采样点的位置、水文、物理和化学条件信息。这些数据对于平衡区域和全球C预算将非常有价值。</p>
Magnesium isotope constraints on the Holocene hydromagnesite formation in alkaline Lake Dujiali, central Qinghai-Tibetan Plateau
<p>This dataset contains the following nice Tables:</p> <p>1. Table S-1 Mineralogical compositions of hydromagnesite and lake sediments.</p> <p>2. Table S-2 Mg isotope and Sr data of Dujiali Lake.</p> <p>3. Table S-3 Chemical compositions of waters in Dujiali lake. </p> <p>4. Table S-4 The compilation of small rivers draining only ultramafic rocks.</p> <p>5. Table S-5 The compilation of Mg/Ca ratios (mol/mol) of alkaline lakes in the world.</p> <p>6. Table S-6 The compilation of δ 26Mg in river waters, groundwater, soil water and hydromagnesite.</p> <p>7. Table S-7 The major elements compositions of lake sediments and hydromagensite.</p> <p>8. Table S-8 Model input parameters.</p> <p>9. Table S-9: Model parameters.</p>
FIGURE 4. Helvella lacunosa. a, b in Helvella cystidiata sp. nov. (Helvellaceae, Ascomycota) from Tibetan Plateau, China
FIGURE 4. Helvella lacunosa. a, b Mature specimens (a HKAS 87877; b HKAS 87878); c, d Receptacle surface of pileus; e, f Stipitipellis; g, h Asci and paraphyses; i–k Asci; l Ascospores. Scale bars: a, b = 1 cm; c–l = 50 μm.
FIGURE 3 in Helvella cystidiata sp. nov. (Helvellaceae, Ascomycota) from Tibetan Plateau, China
FIGURE 3. Helvella cystidiata (HKAS 78941, holotype). a–c Mature specimens (a, b HKAS 78941, c HKAS 74316); d Receptacle surface of pileus; e, f Stipitipellis; g, h Asci, and paraphyses; i–k Asci; l Ascospores. Scale bars: a–c = 1 cm; d–h = 50 μm.
FIGURE 1 in Helvella cystidiata sp. nov. (Helvellaceae, Ascomycota) from Tibetan Plateau, China
FIGURE 1. The phylogenetic tree obtained by RAxML analysis of ITS sequence data. The node shows the bootstrap support value with Maximum likelihood ML greater than or equal to 75% and the BI posterior probability greater than or equal to 0.95 BYPP. The new isolates of this study are in red bold. Helvella zhongtiaoensis (HKAS 74335) is selected as the outgroup (Zhao et al. 2016).
FIGURE 2 in Helvella cystidiata sp. nov. (Helvellaceae, Ascomycota) from Tibetan Plateau, China
FIGURE 2. The phylogenetic tree obtained by RAxML analysis of ITS, LSU sequence combination data. The node shows the bootstrap support value with Maximum likelihood ML greater than or equal to 75% and the BI posterior probability greater than or equal to 0.95 BYPP. The new isolates of this study are in red bold.
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