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15 results for “Asian flora”
FIG. 2 in Contribution of French explorers to the study of Middle Asian flora: the herbarium collections by Guillaume Capus (1857-1931)
FIG. 2. — Travel route of Guillaume Capus and Gabriel Bonvalot in Middle Asia, 1880-1882 (Bonvalot 1884).
FIG. 1. — A in Contribution of French explorers to the study of Middle Asian flora: the herbarium collections by Guillaume Capus (1857-1931)
FIG. 1. — A, Guillaume Capus (Chevalier 1931), source Gallica (https://gallica.bnf.fr/ark:/12148/btv1b8450852x); B, Gabriel Bonvalot (Bibliothèque nationale de France, département Société de Géographie, SG PORTRAIT-10135).
FIG. 6. — Oxytropis tatarica Hook.f in Contribution of French explorers to the study of Middle Asian flora: the herbarium collections by Guillaume Capus (1857-1931)
FIG. 6. — Oxytropis tatarica Hook.f. & Thomson ex Bunge; collection by Guillaume Capus housed at the P Herbarium, G. Capus 365 (P[P02914846]).
FIG. 5 in Contribution of French explorers to the study of Middle Asian flora: the herbarium collections by Guillaume Capus (1857-1931)
FIG. 5. — Distribution of herbarium specimens collected by Capus in Middle Asia, following the current countries.
FIG. 4 in Contribution of French explorers to the study of Middle Asian flora: the herbarium collections by Guillaume Capus (1857-1931)
FIG. 4. — Collection density map based on Capus' herbarium specimens from the Middle Asia (1880-1882).
FIG. 3 in Contribution of French explorers to the study of Middle Asian flora: the herbarium collections by Guillaume Capus (1857-1931)
FIG. 3. — Species diversity map based on Capus' herbarium specimens from the Middle Asia (1880-1882).
Text-fig. 1. Modern vegetation proxies as delivered by the Drudge 1 and 2 tools for Parschlug. Left column results from KovarEder et al. (2021) based on the floristic spectrum published by Kovar-Eder et al. (2004). The other three columns result from three variants using the enlarged floristic spectrum herein. Differences between variants 1–3 from this study are caused by differences in assignment of some taxa and morphotypes (see Appendix 1). European vegetation formations: Formation C – Subarctic, boreal and nemoral-montane open woodlands as well as subalpine and oro-Mediterranean vegetation; Formation D – Mesophytic and hygromesophytic coniferous and mixed broad-leaved-coniferous forests; Formation F – Mesophytic broadleaved deciduous and mixed broadleaved/conifer forests; Formation G – Thermophilous mixed deciduous broadleaved forests; Formation J – Mediterranean sclerophyllous forests and scrub; Formation K – Xerophytic coniferous forests, coniferous woodland and scrub. East Asian vegetation types: MCF China, Japan – Montane Coniferous Forests China, Honshu, Yakushima; BLDF N and NE Provinces, China – Broad-leaved Deciduous Forests of the Northern and Northeastern Provinces (China); BLDF Upper Yangtze, Honshu – Broad-leaved Deciduous Forest, Upper Yangtze Provinces, Mt. Emei, and Honshu; MMF China – Mixed Mesophytic Forest, Lower Yangtze Provinces; BLEF China, Japan – Broad-leaved Evergreen Forests, China, Japan; Meili Snow Mt. high altitude SCL and BLF, China – Meili Snow Mt., Sclerophyllous and broad-leaved forest zone (2,580-3,650 m alt.). (Designations of European vegetation formations follow Bohn et al. (2004) and Asian ones follow Kovar-Eder et al. (2021). in Floristic, Vegetation And Climate Assessment Of The Early/Middle Miocene Parschlug Flora Indicates A Distinctly Seasonal Climate
Text-fig. 1. Modern vegetation proxies as delivered by the Drudge 1 and 2 tools for Parschlug. Left column results from KovarEder et al. (2021) based on the floristic spectrum published by Kovar-Eder et al. (2004). The other three columns result from three variants using the enlarged floristic spectrum herein. Differences between variants 1–3 from this study are caused by differences in assignment of some taxa and morphotypes (see Appendix 1). European vegetation formations: Formation C – Subarctic, boreal and nemoral-montane open woodlands as well as subalpine and oro-Mediterranean vegetation; Formation D – Mesophytic and hygromesophytic coniferous and mixed broad-leaved-coniferous forests; Formation F – Mesophytic broadleaved deciduous and mixed broadleaved/conifer forests; Formation G – Thermophilous mixed deciduous broadleaved forests; Formation J – Mediterranean sclerophyllous forests and scrub; Formation K – Xerophytic coniferous forests, coniferous woodland and scrub. East Asian vegetation types: MCF China, Japan – Montane Coniferous Forests China, Honshu, Yakushima; BLDF N and NE Provinces, China – Broad-leaved Deciduous Forests of the Northern and Northeastern Provinces (China); BLDF Upper Yangtze, Honshu – Broad-leaved Deciduous Forest, Upper Yangtze Provinces, Mt. Emei, and Honshu; MMF China – Mixed Mesophytic Forest, Lower Yangtze Provinces; BLEF China, Japan – Broad-leaved Evergreen Forests, China, Japan; Meili Snow Mt. high altitude SCL and BLF, China – Meili Snow Mt., Sclerophyllous and broad-leaved forest zone (2,580-3,650 m alt.). (Designations of European vegetation formations follow Bohn et al. (2004) and Asian ones follow Kovar-Eder et al. (2021).
Linked collectors and determiners for: Contribution of French explorers to the study of Middle Asian flora: the herbarium collections by Guillaume Capus (1857 - 1931).
Natural history specimen data linked to collectors and determiners held within, "Contribution of French explorers to the study of Middle Asian flora: the herbarium collections by Guillaume Capus (1857 - 1931)". Claims or attributions were made on Bionomia by volunteer Scribes, <a href="https://bionomia.net/dataset/bf81983a-101e-4e6b-af21-ef6a9359f7f0">https://bionomia.net/dataset/bf81983a-101e-4e6b-af21-ef6a9359f7f0</a> using specimen data from the dataset aggregated by the Global Biodiversity Information Facility, <a href="https://gbif.org/dataset/bf81983a-101e-4e6b-af21-ef6a9359f7f0">https://gbif.org/dataset/bf81983a-101e-4e6b-af21-ef6a9359f7f0</a>. Formatted as a Frictionless Data package.
Immigration dynamics of tropical and subtropical Southeast Asian limestone karst floras
<p><i>Ex situ </i>origins and dispersal of taxa have played important roles in the assembly of island-like biodiversity hotspots. Insular limestone karsts in Southeast Asia are hotspots of biodiversity and endemism, but the immigration processes of their unique floras are still poorly known. Here, we used Gesneriaceae as a proxy to investigate immigration dynamics of tropical and subtropical Southeast Asian karst floras. We show that immigration into subtropical Southeast Asian karst floras first occurred in the early Miocene, with two peaks in the early to middle Miocene and the Pliocene to early Pleistocene, whereas immigration into tropical Southeast Asian karsts initiated in the late Eocene, with two peaks in the late Oligocene and the late Miocene. The rich geological and ecological diversities of different regions, together with habitat isolation due to climatic changes, might be responsible for the different immigration patterns. We also discover that Southeast Asian karst biodiversity comprises a mix of immigrant pre-adapted lineages and descendants from local acid soil ancestors, although niche shift from acid soil to karst in tropical Southeast Asian islands was lacking. <span>These </span><span>findings</span> <span>provide insights into </span><span>how</span> <span>Southeast </span><span>Asian </span><span>k</span><span>arst</span><span>s</span><span> respond to ongoing climate change and are of particular importance for</span><span> their </span><span>conservation planning</span><span>.</span></p>
FIGURE 2 in New species and records in the fern genus Didymoglossum for the flora of Seychelles, with notes on the Southeast Asian D. motleyi complex (Hymenophyllaceae)
FIGURE 2. Illustration of Didymoglossum beaverianum (Fouzer Kati). A. Micro-habitat, rupicolous in wet ravines; B. Mat, showing the inclined position of leaves, not appressed on the substrate; C. Tortuous rhizome irregularly branching; D. Shape of fertile and sterile leaves; E. Developing sori in shallow apical notches; F. Developing sorus (early stage); G. Developing sorus (intermediate stage); H. Winged margins of the sorus; I. Rhizome showing unicellular hairs.
FIGURE 1 in New species and records in the fern genus Didymoglossum for the flora of Seychelles, with notes on the Southeast Asian D. motleyi complex (Hymenophyllaceae)
FIGURE 1. Bayesian phylogeny inferred from rbcL sequences showing relationships in the genus Didymoglossum. Support values on nodes are posterior probabilities. The species/populations studied and compared here are shown in coloured boxes. D = subgenus Didymoglossum, M = subgenus Microgonium.
FIGURE 3 in New species and records in the fern genus Didymoglossum for the flora of Seychelles, with notes on the Southeast Asian D. motleyi complex (Hymenophyllaceae)
FIGURE 3. Illustration of the range of within specimen variability in the lamina shape and petiole length and pubescence in fertile leaves of the Seychellois population of Didymoglossum beccarianum (A, B, C) and D. beaverianum (D, E, F).
FIGURE 5 in New species and records in the fern genus Didymoglossum for the flora of Seychelles, with notes on the Southeast Asian D. motleyi complex (Hymenophyllaceae)
FIGURE 5. Illustration of Didymoglossum beccarianum (Pti fouzer ron). A. Micro-habitat, corticolous at the base of endemic palm Phoenicophorium borsigianum; B. Mat, showing leaves slightly appressed to the substrate; C. Rhizome showing regular branching; D. Shape of fertile and sterile leaves; E. Developing sorus in deep apical notch; F. Un-winged margins of the sorus; G. Leaf base showing unicellular hairs below the false veins.
Immigration dynamics of tropical and subtropical Southeast Asian limestone karst floras
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FIGURE 4. Distribution map for Didymoglossum beccarianum and D in New species and records in the fern genus Didymoglossum for the flora of Seychelles, with notes on the Southeast Asian D. motleyi complex (Hymenophyllaceae)
FIGURE 4. Distribution map for Didymoglossum beccarianum and D. beaverianum in Seychelles.
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