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83 results for “Deccan”
Śaiva and Buddhist rhetoric in copperplate grants of the Eastern Deccan: textual analysis data
<p>This is a textual analysis dataset derived from copperplate grants of the Eastern Cālukyas, Viṣṇukuṇḍis and Śrīmūla.<br> The data accompany the following forthcoming publication (title and date of publication subject to change):<br> Balogh, Dániel. 2024. ‘Can We Discern a Śaiva and a Buddhist Rhetoric in Royal Eulogies?’ In Śaiva-Buddhist Encounters in Early Medieval East India, edited by Florinda De Simini. Studies on the History of Śaivism. Naples: UniorPress.<br> Details of the methodology are presented in other publications by Balogh to appear in 2024 (forthcoming or in preparation when this dataset is released).<br> The parent of this dataset is available at https://zenodo.org/record/7900312<br> The present dataset has been extended by adding analytical data from Viṣṇukuṇḍi and Śrīmūla charters, but simultaneously reduced by discarding all data not pertaining to the issuing sovereigns.<br> This dataset, the underlying research and the relevant publication are results of the project DHARMA ‘The Domestication of “Hindu” Asceticism and the Religious Making of South and Southeast Asia’. This project has received funding from the European Research Council (ERC) under the European Union’s Horizon 2020 research and innovation programme (grant agreement no 809994).</p>
Fig. 5 in The oldest birotule-bearing freshwater sponges from the Upper Cretaceous-lower Paleocene Deccan volcanic-associated sediments of India
Fig. 5. Spicular complement of skeleton and gemmules of palaeospongillid sponge Longibirotula antiqua gen. et sp. nov. from Upper Cretaceous–lower Paleocene of Naskal GSI Quarry (India) (slides PGNU/NSKQ/ST-1, 2). A, B. Acanthoxeas short with dense spines. C, D. Oxeas fusiform, long and with acute tips. E, F. Birotules with long shaft. Diagenetic processes affect all spicules to various degree. Scale bars 20 µm.
Fig. 3 in The oldest birotule-bearing freshwater sponges from the Upper Cretaceous-lower Paleocene Deccan volcanic-associated sediments of India
Fig. 3. Megascleres of palaeospongillid sponge Longibirotula antiqua gen. et sp. nov. from Upper Cretaceous–lower of Paleocene of Naskal GSI Quarry India). A–H. Acanthoxeas (slides PGNU/NSKQ/SL-1–13) with large spines. Diagenetic processes affect all spicules to various degree. Scale bars 20 µm.
Fig. 1 in The oldest birotule-bearing freshwater sponges from the Upper Cretaceous-lower Paleocene Deccan volcanic-associated sediments of India
Fig. 1. Map of India showing Deccan volcanic province (green area). A. Location of Naskal intertrappean, Naskal B (white star) and Naskal GSI Quarry sections (red star); map modified after Ahluwalia (1990) and Wilson Mantilla et al. (2022). B. Sponge spicule and diatom bearing horizon in Naskal GSI Quarry section. C. Palynomorph bearing Naskal B section (modified after Wilson Mantilla et al. 2022).
Fig. 4 in The oldest birotule-bearing freshwater sponges from the Upper Cretaceous-lower Paleocene Deccan volcanic-associated sediments of India
Fig. 4. Gemmuloscleres of palaeospongillid sponge Longibirotula antiqua gen. et sp. non. from Upper Cretaceous–lower Paleocene of Naskal GSI Quarry (India). A–O. Birotules (slides PGNU/NSKQ/SL-1–13) slender, spiny, with long shaft. Diagenetic processes affect all spicules to various degree. Scale bars 20 µm.
Fig. 2 in The oldest birotule-bearing freshwater sponges from the Upper Cretaceous-lower Paleocene Deccan volcanic-associated sediments of India
Fig. 2. Megascleres of palaeospongillid sponge Longibirotula antiqua gen. et sp. nov. from Upper Cretaceous–lower Paleocene of Naskal GSI Quarry (India). A–I. Oxeas (slides PGNU/NSKQ/SL-1–13) slim to stout with variably pointed tips. Diagenetic processes affect all spicules to various degree. Scale bars 20 µm. { fig. will be greyscale in printed version}
Fig. 2 in A new species of Lycodon (Serpentes: Colubridae) from the Deccan Plateau of India, with notes on the range of Lycodon travancoricus (Beddome, 1870) and a revised key to peninsular Indian forms
Fig. 2. Lycodon deccanensis sp. nov. in preservative: (a–b) entire and head closeup (inset) of Paratype ZSI 13271; (c) entire view of SACON/VR-93. Photos by K. Deuti and S.R.Ganesh.
Fig. 1 in A new species of Lycodon (Serpentes: Colubridae) from the Deccan Plateau of India, with notes on the range of Lycodon travancoricus (Beddome, 1870) and a revised key to peninsular Indian forms
Fig. 1. Lycodon deccanensis sp. nov. in life: (a) entire, dorsolateral view; (b–d) head profiles of a live uncollected specimen from Devarayana Durga; (e–f) live uncollected adult and juvenile from Melagiri, showing ontogenic color shift. Photos by K.G. Punith, M.V. Shreeram, and S.R.Ganesh.
Fig. 4 in A new species of Lycodon (Serpentes: Colubridae) from the Deccan Plateau of India, with notes on the range of Lycodon travancoricus (Beddome, 1870) and a revised key to peninsular Indian forms
Fig. 4. Extralimital records re-identified as (a–b) Lycodon anamallensis (BNHS 1602a and b) and (c–e) Lycodon cf. aulicus (BNHS 1603 and 1604). Photos by A. Omkar.
Fig. 3 in A new species of Lycodon (Serpentes: Colubridae) from the Deccan Plateau of India, with notes on the range of Lycodon travancoricus (Beddome, 1870) and a revised key to peninsular Indian forms
Fig. 3. Map showing the type locality and distribution records of Lycodon deccanensis sp. nov. Type locality (Devarayana Durga) marked with a red dot.
Linked collectors and determiners for: Catalogue of species of the subgenus Afromorgus Scholtz, 1986 (Coleoptera: Trogidae: Omorginae) known from the Oriental and Palaearctic Regions, including a description of one new species from the Deccan Plateau in India.
Natural history specimen data linked to collectors and determiners held within, "Catalogue of species of the subgenus Afromorgus Scholtz, 1986 (Coleoptera: Trogidae: Omorginae) known from the Oriental and Palaearctic Regions, including a description of one new species from the Deccan Plateau in India". Claims or attributions were made on Bionomia by volunteer Scribes, <a href="https://bionomia.net/dataset/9cb09294-5d9e-4bf9-accf-0d7344395d3a">https://bionomia.net/dataset/9cb09294-5d9e-4bf9-accf-0d7344395d3a</a> using specimen data from the dataset aggregated by the Global Biodiversity Information Facility, <a href="https://gbif.org/dataset/9cb09294-5d9e-4bf9-accf-0d7344395d3a">https://gbif.org/dataset/9cb09294-5d9e-4bf9-accf-0d7344395d3a</a>. Formatted as a Frictionless Data package.
Cryptic Magma Chamber in the Deccan Traps imaged using receiver functions and Surface wave dispersion
<p>This is a Dataset for the article titled "Cryptic Magma Chamber in the Deccan Traps imaged using receiver functions and Surface wave dispersion" by Saha et. al. (2023). For more information about the data, contact <a href="mailto:kumarsahagokul123@gmail.com">kumarsahagokul123@gmail.com.</a></p>
Anisotropy of magnetic susceptibility (AMS) and rock magnetic data for Pachmarhi dyke swarm of Deccan
<p>The Pachmarhi dyke swarms, situated in the Eastern part of the Narmada-Satpura-Tapi (N-S-T) dykes of the Deccan Continental Flood Basalt (DCFB), are studied using the Anisotropy of Magnetic Susceptibility (AMS) technique. Here, we determine the direction and sense of magma flow within the dykes to gain insights into the depth, number, and location of magma chambers, as well as the geodynamics of their plumbing system. Petrography and rock magnetism analyses revealed high-titanium magnetite particles, predominantly of Pseudo-Single Domain (PSD) nature, with a smaller proportion of Multi-Domain (MD) grains. We identified four distinct magnetic fabric types (I-IV) within the Pachmarhi dykes. The imbrication of magnetic foliation (for oblate fabric) and magnetic lineation (for prolate fabric) has been employed to discern the direction of magma flow which revealed multiple trends of magma flow, ranging from vertical/sub-vertical to inclined, with one particular dyke exhibiting lateral flow. The intersection of imbrication within the dyke margins provided valuable information about the presence of multiple shallow sub-crustal magma chambers which are supported by independent geophysical evidence and are similar to those of the Nandurbar-Dhule dyke swarms in the western region of the N-S-T dykes. Consequently, it can be inferred that the emplacement of dykes in the Pachmarhi region of the NSL, which were possible feeders to the late-stage Deccan volcanism, was primarily facilitated by a "polycentric flow" mechanism, wherein magma was injected vertically through shallow crustal fissures, potentially feeding into the late-stage Deccan flow units like Ambenali or Mahabaleshwar formation.</p>
Figure 2 in Occurrence of Coelostoma (Lachnocoelostoma) horni (Régimbart, 1902) (Coleoptera: Hydrophilidae) from Deccan Peninsular, India
Figure 2. Coelostoma horni: A. Dorsal View B. Ventral View C. Elytra D. Male Aedeagus.
Figure 1 in Occurrence of Coelostoma (Lachnocoelostoma) horni (Régimbart, 1902) (Coleoptera: Hydrophilidae) from Deccan Peninsular, India
Figure 1. Map showing Coelostoma horni distribution from Deccan peninsular India.
Anisotropy of magnetic susceptibility (AMS) and rock magnetic data for Pachmarhi dyke swarm of Deccan
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FIGURE 2 in A new species of Sphaerotheca Günther, 1859 (Anura: Dicroglossidae) from the degraded urban ecosystems of Bengaluru, Deccan Plateau, India
FIGURE 2. Maximum Likelihood (ML) gene tree for species of Sphaerotheca based on 585 bp of mitochondrial 16S rRNA gene.
FIGURE 4 in A new species of Sphaerotheca Günther, 1859 (Anura: Dicroglossidae) from the degraded urban ecosystems of Bengaluru, Deccan Plateau, India
FIGURE 4. Sphaerotheca bengaluru sp. nov. holotype in preservative (A) Dorsal view (B) Ventral view.
FIGURE 5 in A new species of Sphaerotheca Günther, 1859 (Anura: Dicroglossidae) from the degraded urban ecosystems of Bengaluru, Deccan Plateau, India
FIGURE 5. Habitat of Sphaerotheca bengaluru sp. nov. from the type locality, a degraded ecosystem of Bengaluru.
FIGURES 69–70 in Catalogue of species of the subgenus Afromorgus Scholtz, 1986 (Coleoptera: Trogidae: Omorginae) known from the Oriental and Palaearctic Regions, including a description of one new species from the Deccan Plateau in India
FIGURES 69–70. Omorgus (Afromorgus) procerus (Harold, 1872), lectotype (MNHN). 69, habitus, dorsal view; 70, labels. Photos by Olivier Montreuil, copyright MNHN.
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