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IO Islamic 2548. Historical Miscellanies by Various Hands
<p>IO Islamic 2548. Historical Miscellanies by Various Hands</p>
IO Islamic 1543. Historical Miscellanies of Niżâms of Ḥaidarâbâd, The rulers of Bijâpûr, Ḥaidar 'Alî of Mysore, and the Marattah and Afghân invasions of India
<p>IO Islamic 1543. Historical Miscellanies of Niżâms of Ḥaidarâbâd, The rulers of Bijâpûr, Ḥaidar ‘Alî of Mysore, and the Marattah and Afghân invasions of India</p>
IO Islamic 3057. A Short Historical Account of Seringapatan
<p>IO Islamic 3057. A Short Historical Account of Seringapatan</p>
FIG. 11 in Climatic evolution in Western Europe during the Cenozoic: insights from historical collections using leaf physiognomy
FIG. 11. — Evolution of MAT in Europe in terrestrial, marine shallow-water and deep-sea records. Abbreviations: MEN, Menat; GEL, Gelinden; SEZ, Sézanne; CEL, Célas; ARM, Armissan; AIX, Aix-en-Provence; SB, Saint-Bauzile. Symbols: black circle, this study, CLAMP on leaves; light blue solid line, Bechtel et al. (2008), δ13C on coal; pink solid line, Héran et al. (2010), δ18O on rodents; orange solid line, Hren et al. (2013), δ47 freshwater gastropods; grey background, Mosbrugger et al. (2005), CA on leaves; blue square, Moiseeva et al. (2018), CLAMP on leaves; yellow circle, Domingo et al. (2007), multi-proxy; green stars, Inglis et al. (2017), lignites; black solid line, Huygue et al. (2017), marine mollusks δ18O. Deep-sea record is adapted from Zachos et al. (2008). Numerical values are from Table 3. For Gelinden, Sézanne and Armissan, the results from CLAMP analysis using Asia1 calibration are displayed. For all other localities, the results from CLAMP analysis using BR calibration are displayed.
FIG. 8 in Climatic evolution in Western Europe during the Cenozoic: insights from historical collections using leaf physiognomy
FIG. 8. — Saint-Bauzile paleoflora (Tortonian, Miocene): A, Castanea vesca Gaertner (MNHN.F.40273); B, Juglans regia L. (MNHN.F.40289); C, Populus tremula L. (MNHN.F.40244); D, Quercus cerris L. (MNHN.F.40225.2); E, Acer decipiens Braun (MNHN.F.40296); F, Acer campestre L. (MNHN.F.40318); G, Carpinus sp. (MNHN.F.40358); H, Quercus sp. – Ilex group (MNHN.F.40268); I, OTU 1 (MNHN.F.40393); J, Crataegus sp. (MNHN.F.40372); K, Vitis teutonica Braun (MNHN.F.40585.1); L, Vitis thunbergii Siebold & Zuccarini (MNHN.F.40228); M, Betula sp. (MNHN.F.40368); N, Ulmus sp. (MNHN.F.40366); O, Tilia sp. (MNHN.F.40323); P, OTU 2 (MNHN.F.40394); Q, OTU 4 (MNHN.F.40421); R, OTU 6 (MNHN.F.40345). Scale bars: A-F, H, I, K-R, 2 cm; G, J, 1 cm.
FIG. 9 in Climatic evolution in Western Europe during the Cenozoic: insights from historical collections using leaf physiognomy
FIG. 9. — Physiognomic spaces showing the location of the fossil sites within the extant sites of A, Global calibration, B, BR calibration (excluding cold sites), C, Asia1 and D, Asia2 (both including monsoonal localities: blue filled circles). Numbers: 1, Menat; 2, Gelinden; 3, Sézanne; 4, Célas; 5, Armissan; 6, Aix-en- Provence; 7, Saint-Bauzile; green: localities close to the monsoonal sites.
FIG. 6 in Climatic evolution in Western Europe during the Cenozoic: insights from historical collections using leaf physiognomy
FIG. 6. — Armissan paleoflora (Rupelian, Oligocene): A, Acer pseudocampestre Unger (MNHN.F.11137); B, Acer narbonense Saporta (MNHN.F.11139); C, Populus sclerophylla Saporta (MNHN.F.16043, MNHN.F.16089.B); D, Myrica banksiaefolia Unger (MNHN.F.12778); E, Quercus armata Saporta (MNHN.F.12782); F, Laurus resurgens Saporta (MNHN.F.16033); G, Laurus tournalii Saporta (MNHN.F.12773); H, Laurus conspicua Saporta (MNHN.F.12751); I, Celtis primigenia Saporta (MNHN.F.16099); J, Ilex acuminata Saporta (MNHN.F.16023); K, Ilex rigida Saporta (MNHN.F.16048); L, Engelhardtia oxyptera (MNHN.F.16091); M, Engelhardtia brongniartii (MNHN.F.12741.2M); N, Myrsine celastroides Ettingshausen (MNHN.F.11128.2, arrow);O, Ficus dryophylla Saporta (MNHN.F.16027, 16102); P, Zanthoxylon falcatum Saporta? (MNHN.F.16038); Q, Pinus divaricata Saporta (MNHN.F.11169); R, Pinus tenuis Saporta (MNHN.F.11072). Scale bars: A-L, P-R, 2 cm; M, O, 1 cm.
FIG. 7 in Climatic evolution in Western Europe during the Cenozoic: insights from historical collections using leaf physiognomy
FIG. 7. — Aix-en-Provence paleoflora (Chattian, Oligocene): A, Cinnamomum aquense Saporta (MNHN.F.16204); B, Cinnamomum polymorphum (Braun) Heer (MNHN.F.12809); C, Ficus venusta Saporta (MNHN.F.13969); D, Ficus pulcherrima Saporta (MNHN.F.13972); E, Myrsine recuperata Saporta (MNHN.F.14174); F, Diospyros varians Saporta (MNHN.F.14251); G, Diospyros multinervis Saporta (MNHN.F.14252); H, Diospyros discreta Saporta (MNHN.F.14248.1); I, Myrica dryomorpha Saporta (MNHN.F.28566); J, Myrica angustata Saporta (MNHN.F.11707); K, Myrsine miramba Saporta (MNHN.F.14180); L, Oreodaphne detecta Saporta (MNHN.F.16189); M, Rhus macilenta (MNHN.F.14153); N, Rhus rhomboidalis Saporta (MNHN.F.14158); O, Vaccinium obscurum Saporta (MNHN.F.14645); P, Quercus palaeophellos Saporta (MNHN.F.13958); Q, Quercus elaena Unger (MNHN.F.11680); R, Aralia tripartita Saporta (MNHN.F.14098); S, Podocarpus proxima Saporta (MNHN.F.16174); T, Pinus coquandii Saporta (MNHN.F.12818.1M). Scale bars: A-K, N, P-T, 2 cm; L, M, O, 1 cm.
FIG. 5 in Climatic evolution in Western Europe during the Cenozoic: insights from historical collections using leaf physiognomy
FIG. 5. — Célas paleoflora (Priabonian, Eocene): A, Cocculus intermedius Laurent (MHN Marseille, 4991); B, Phyllites sp (MHN Marseille, 4955); C, Parkinsonia recta Laurent (MHN Marseille, 4966); D, Rhododendron celasensis Laurent (MHN Marseille, 4988); E, Ficus ovalis Laurent (MHN Marseille, 4998); F, Ficus marioni Laurent (MHN Marseille, 5009); G, OTU 8 (MHN Marseille, 16733.45); H, Indet. (MHN Marseille, 16773.94); I, Andromeda neglecta Saporta (MHN Marseille, 4987); J, Zizyphus paradisiaca Heer (MHN Marseille, 4976); K, OTU 10 (MHN Marseille, 16773.53); L, OTU 19 (MHN Marseille, 16773.98); M,?Myrica dryandroefolia Brongniart (MHN Marseille, 16773.39); N, OTU 2 (MHN Marseille, 16733.2); O, OTU 1 (MHN Marseille, 16773.1.2); P, OTU 11 (MHN Marseille, 16773.54). Doliostrobus Marion cones at different stages of disintegration. Q, MHN Marseille, 16773.20 (Marion 1888: pl. II.16A-B); R, MHN Marseille, 16773.18; S, MHN Marseille, 16773.16 (Marion 1888: pl. II.15); T, MHN Marseille, 16773.14; U, MHN Marseille, 16773.17 (Marion 1888: pl. II.13); V, MHN Marseille, 16773.12. Scale bars: A, D-P, 2 cm; B, C, Q-V 1 cm.
FIG. 4 in Climatic evolution in Western Europe during the Cenozoic: insights from historical collections using leaf physiognomy
FIG. 4. — Sézanne paleoflora (Thanetian, Paleocene): A, Protoficus sezannensis Saporta (MNHN.F.11873); B, Aralia hederacea Saporta (MNHN.F.11917); C, Sterculia variabilis Saporta (MNHN.F.11933); D, Ulmus antiquissima Saporta (MNHN.F.11870); E, Laurus assimilis Saporta (MNHN.F.11900); F, Zizyphus raincourtii Saporta (MNHN.F.11954); G, Daphnogene raincourtii Saporta (MNHN.F.11906); H, Sassafras primigenium Saporta (MNHN.F.11902); I, Cissus primaeva Saporta (MNHN.F.11926); J, Salix stupenda Saporta (MNHN.F.11880); K, Dryophyllum palaeocastanea Saporta (MNHN.F.11864); L, Aralia hederacea Saporta (MNHN.F.11964). Scale bars: A-E, I-L, 2 cm; F-H: 1 cm.
FIG. 3 in Climatic evolution in Western Europe during the Cenozoic: insights from historical collections using leaf physiognomy
FIG. 3. — Menat paleoflora (Selandian, Paleocene): A, Populus balsamoides Goeppert (MNHN.F.21144); B, Corylus Mac-Quarrii (Forbes) Heer (MNHN.F.20734); C, Fraxinus agassiziana Heer (MNHN.F.12657); D, Salix lamottei Saporta (MNHN.F.21346); E, Dryophyllum dewalquei Saporta & Marion (MNHN.F.12665); F, Myrica saportana Schimper (MNHN.F.20790); G, Dryophyllum curticellense Saporta & Marion (MNHN.F.21097); H, Quercus elaena Unger (MNHN.F.21182); I, Acer loetum eocenicum C. A. Mey (MNHN.F.21157); J, Platanus schimperi (Heer) Saporta & Marion (MNHN.F.20711); K, Cinnamomum martyi Fritel (MNHN.F.12646); L, Laurus praecellens Saporta (MNHN.F.21332); M, Actinodaphne germari Heer (MNHN.F.21314); N, Lindera stenoloba (Saporta) Laurent (MNHN.F.21205); O, Quercus lonchitis Unger (MNHN.F.21300); P, Luheopsis vernieri Marty (MNHN.F.21165); Q, Ficus tiliaefolia Heer (MNHN.F.21260); R, Myrica hakeifolia Saporta (MNHN.F.21323). Scale bars: A-C, E, I-R, 2 cm; D, F, G, H, 1 cm.
FIG. 1 in Climatic evolution in Western Europe during the Cenozoic: insights from historical collections using leaf physiognomy
FIG. 1. — Location and chronostratigraphical positions of the deposits: A, Paleocene; B, Eocene-Oligocene; C, Miocene; D, present; adapted from Mai (1995), Rögl (1999), Bruch et al. (2007) and Kvaček (2010). Information on the provinces and floras are taken from Mai (1995) and Kvaček (2010), in regular and italic fonts respectively.
Figure 7 from: Turcios-Casco MA, Ávila-Palma HD, LaVal RК, Stevens RD, Ordoñez-Trejo EJ, Soler-Orellana JA, Ordoñez-Mazier DI (2020) A systematic revision of the bats (Chiroptera) of Honduras: an updated checklist with corroboration of historical specimens and new records. Zoosystematics and Evolution 96(2): 411-429. https://doi.org/10.3897/zse.96.51059
Figure 7 Map with new records of D. youngii and N. lanatus for Honduras. None of the previous records (except D. youngii) have exact coordinates, however, we shaded the municipality on each department in which they were recorded. The blue shaded area indicates the localities of N. lanatus captured in the municipality of Zamorano (municipality of San Antonio de Oriente) in the department of Francisco Morazán in central Honduras, and in La Cueva del Viejo in the department of La Paz in western Honduras. The big yellow-shaded area refers to two localities in which L. yerbabuenae was recorded in the municipality of Nacaome in the department of Valle in southern Honduras by Lee and Bradley (1992) and R. D. Bradley in 1991 (GBIF.org 2019). The small brown-shaded areas in southern Honduras refer to the localities in which M. Sandiford reported one L. yerbabuenae from the municipality of Santa Ana de Yusguare in the department of Choluteca (GBIF.org 2019). Finally, the purple point refers to the exact location of D. youngii recorded in the department of Colón in northeastern Honduras. Abbreviations as follows: La Paz (LP), Nacaome (NC), San Antonio de Oriente (SAO), and Santa Ana de Yusguare (SAY). There is no specific area highlighted in La Paz because there are several caves known as Cueva del Viejo.
Figure 6 from: Turcios-Casco MA, Ávila-Palma HD, LaVal RК, Stevens RD, Ordoñez-Trejo EJ, Soler-Orellana JA, Ordoñez-Mazier DI (2020) A systematic revision of the bats (Chiroptera) of Honduras: an updated checklist with corroboration of historical specimens and new records. Zoosystematics and Evolution 96(2): 411-429. https://doi.org/10.3897/zse.96.51059
Figure 6 A – Roost of Thyroptera discifera in a (Musaceae) from the Caribbean lowlands of Costa Rica. B – View of the colony T. discifera inside the leaves of Musa × acuminata. Photos by Bernal Rodríguez.
Figure 3 from: Turcios-Casco MA, Ávila-Palma HD, LaVal RК, Stevens RD, Ordoñez-Trejo EJ, Soler-Orellana JA, Ordoñez-Mazier DI (2020) A systematic revision of the bats (Chiroptera) of Honduras: an updated checklist with corroboration of historical specimens and new records. Zoosystematics and Evolution 96(2): 411-429. https://doi.org/10.3897/zse.96.51059
Figure 3 Diaemus youngii. A – Frosted brownish venter; B – Whitish tip of the wings; C – One pad on the base of the thumb.
Figure 2 from: Turcios-Casco MA, Ávila-Palma HD, LaVal RК, Stevens RD, Ordoñez-Trejo EJ, Soler-Orellana JA, Ordoñez-Mazier DI (2020) A systematic revision of the bats (Chiroptera) of Honduras: an updated checklist with corroboration of historical specimens and new records. Zoosystematics and Evolution 96(2): 411-429. https://doi.org/10.3897/zse.96.51059
Figure 2 A ventral, B lateral and C dorsal views of the skull of C. mexicanus (TTU 104070) captured in the SAG, La Ceiba in the deparment of Atlántida in northern Honduras.
Figure 5 from: Turcios-Casco MA, Ávila-Palma HD, LaVal RК, Stevens RD, Ordoñez-Trejo EJ, Soler-Orellana JA, Ordoñez-Mazier DI (2020) A systematic revision of the bats (Chiroptera) of Honduras: an updated checklist with corroboration of historical specimens and new records. Zoosystematics and Evolution 96(2): 411-429. https://doi.org/10.3897/zse.96.51059
Figure 5 A – Ungual tufts of N. lanatus (TCWC 10992) and B – Naked feet of N. mexicanus (TCWC 19698).
Figure 1 from: Turcios-Casco MA, Ávila-Palma HD, LaVal RК, Stevens RD, Ordoñez-Trejo EJ, Soler-Orellana JA, Ordoñez-Mazier DI (2020) A systematic revision of the bats (Chiroptera) of Honduras: an updated checklist with corroboration of historical specimens and new records. Zoosystematics and Evolution 96(2): 411-429. https://doi.org/10.3897/zse.96.51059
Figure 1 Artibeus inopinatus. A – Adult male captured in Carboneras, Sabanagrande in the department of Francisco Morazán (center of Honduras). B – Adult female captured in Nagarejo, Nacaome in the department of Valle (southern Honduras).
Figure 4 from: Turcios-Casco MA, Ávila-Palma HD, LaVal RК, Stevens RD, Ordoñez-Trejo EJ, Soler-Orellana JA, Ordoñez-Mazier DI (2020) A systematic revision of the bats (Chiroptera) of Honduras: an updated checklist with corroboration of historical specimens and new records. Zoosystematics and Evolution 96(2): 411-429. https://doi.org/10.3897/zse.96.51059
Figure 4 A Lateral and B ventral views of the skull of Natalus lanatus (TCWC 10992) captured in Zamorano in department of Francisco Morazán, August 1963. C Bicolor ventral pelage of N. lanatus of the same specimen.
A combined approach of mitochondrial DNA and anchored nuclear phylogenomics sheds light on unrecognized diversity, phylogeny, and historical biogeography of the cascade frogs, genus Amolops (Anura: Ranidae)
<p><i>Amolops</i> is one of the most species-rich genera in Ranidae, with 59 recognized species. This genus currently includes six species groups diagnosed mainly by morphology. Several recent molecular studies indicated that the classification of species groups within <i>Amolops</i> remains controversial, and key nodes in the phylogeny have been inadequately resolved. In addition, the diversity of cascade frogs remains poorly understood, especially for those from incompletely sampled regions. Herein, we investigate the species-level diversity within genus <i>Amolops</i> throughout southern China and Southeast Asia, and infer evolutionary relationships among the species using mtDNA data (16S, <i>COI</i>, and <i>ND2</i>). Molecular analyses indicate nine new unnamed species, mostly distributed in the Himalayas. We then utilized anchored hybrid enrichment to generate a dataset representing major mitochondrial lineages to resolve phylogenetic relationships, biogeography, and pattern of species diversification. Our resulting phylogeny strongly supports the monophyly of three previously identified species groups (the <i>A. ricketti</i>, <i>A. daiyunensis</i>,<i> </i>and <i>A. hainanensis</i> groups), the paraphyly of the <i>A. mantzorum</i> and <i>A. marmoratus</i> groups, as previously defined, and monophyly of the <i>A. monticola</i> group. We erect one new species group, the <i>A. viridimaculatus</i> group, and recognize Dubois (1992) 'subgenus' <i>Amo</i> as the <i>A. larutensis</i> species group. Biogeographic analysis suggests that <i>Amolops</i> originated on the Indo-Burma/Tai-Malay Peninsula at the Eocene/Oligocene boundary, and dispersed outward, exemplifying a common pattern observed for the origin of Asia's biodiversity. The early divergence within <i>Amolops</i> coincides with the Himalayas uplift, and the lateral extrusion of Indochina at the Oligocene/Miocene boundary. Our results show that paleoclimatic and geomorphological events have profoundly influenced the pattern of lineage diversification within <i>Amolops</i>.</p>
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Allen Brain Atlas
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