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Figure 17 in Redefinition of Nipponbathynella based on the four new species from East Asia (Crustacea: Bathynellacea: Parabathynellidae)
Figure 17. Nipponbathynella shigaensis sp. nov. (♂: holotype. ♀: allotype). (A) Thoracopod V ♂ (frontal); (B) thoracopod VI ♂ (frontal); (C) protopod of thoracopod VI ♀ (frontal); (D) thoracopod VII ♂ (frontal). Scale bar = 0.05 mm.
Figure 1 in Redefinition of Nipponbathynella based on the four new species from East Asia (Crustacea: Bathynellacea: Parabathynellidae)
Figure 1. Nipponbathynella leesookyungae sp. nov. (♂: holotype, ♀: allotype). (A) General habitus ♀; (B) antennule ♂ (dorsal); (C) antenna ♂ (dorsal); (D) labrum ♂ (ventral); (E) mandible ♂ (ventral); (F) maxillule ♂ (dorsal). Scale bars = 0.05 mm (unless otherwise specified).
Figure 4 in Two new free-living nematode species of Setosabatieria (Comesomatidea) from the East China Sea and the Chukchi Sea
Figure 4. Setosabatieria major sp. nov. (A) lateral view of male head end, showing cervical setae; (B) lateral view of female head end, showing female amphidial fovea; (C) lateral view of female vulva region, showing vulva and eggs; (D) lateral view of male tail region. Scale bars: A = 25 µm; B = 10 µm; C, D = 50 µm.
Figure 2 in Two new species of Lauratonema (Nematoda: Lauratonematidae) from the intertidal zone of the East China Sea
Figure 2. Lauratonema macrostoma sp. nov. (A) lateral view of male head end, showing amphids and bacteria; (B) lateral view of male body part, showing spicule; (C) lateral view of female body part, showing eggs; (D) lateral view of female head end, showing buccal cavity; (E) lateral view of female tail. Scale bar: A–D = 10 µm; E = 25 µm.
Figure 3 in Two new species of Lauratonema (Nematoda: Lauratonematidae) from the intertidal zone of the East China Sea
Figure 3. Lauratonema dongshanense sp. nov. (A) lateral view of male head end, showing amphid and cephalic setae; (B) lateral view of female head end, showing buccal cavity; (C) lateral view of female head end, showing amphid and bacteria; (D) lateral view of female body part, showing eggs; (E, F) lateral view of male body part, showing spicules; (G) lateral view of male tail. Scale bar: A–F = 10 µm; G = 25 µm.
Figure 1 in Two new species of Lauratonema (Nematoda: Lauratonematidae) from the intertidal zone of the East China Sea
Figure 1. Lauratonema macrostoma sp. nov. (A) lateral view of male anterior part; (B) lateral view of female tail; (C) lateral view of male tail; (D) lateral view of female posterior part, showing reproductive system; (E) lateral view of female anterior part. Scale bar: A, B, C, E = 20 µm; D = 50 µm.
Figure 3 in Harpacticoida (Copepoda) of the northern East Sea (the Sea of Japan) and the southern Sea of Okhotsk: diversity, taxocenes, and biogeographical aspects
Figure 3. Biogeographical structure of the faunas from the three main species complexes in the East Sea and the southern part of the Sea of Okhotsk. Relative species abundances with different distribution ranges are presented.
Figs 22-23 in Contribution to the knowledge of the genus Quedius S , 1829 of Siberia and Russian Far East (Coleoptera: Staphylinidae: Staphylinini: Quediina)
Figs 22-23: (22) Type locality of Quedius conviva nov.sp.; (23) Type locality of Quedius amurensis nov.sp.
Figure 5 in Further morphological and molecular studies of driftwood hoppers (Crustacea: Amphipoda: Talitridae) from Mediterraneanłnorth-east Atlantic coastlines
Figure 5. Hypothetical growth curves for: (♦) O. mediterranea from the Medway estuary diamonds (18 months); (A) unknown taxon from the Swale, UK (12 months); (★) M. roffensis from the Medway estuary, UK (12 months). (A) Linear fitting; (B) lognormal fitting.
Figure 4 in Further morphological and molecular studies of driftwood hoppers (Crustacea: Amphipoda: Talitridae) from Mediterraneanłnorth-east Atlantic coastlines
Figure 4. Bayesian estimate of the evolutionary relationships among the talitrid species included in the study based on the COI partition. Numbers at nodes are posterior probabilities; divergence time (myr) ± standard deviation (SD) is reported at each node. Taxa are labelled following the codes in Table 1. Species delimitations obtained with the ABGD method are shown next to the tree.
Figure 3 in Further morphological and molecular studies of driftwood hoppers (Crustacea: Amphipoda: Talitridae) from Mediterraneanłnorth-east Atlantic coastlines
Figure 3. Bayesian estimate of the evolutionary relationships among the talitrid species included in the study based on all genes combined together (COI, 18S and two 28S fragments). Numbers at nodes are posterior probabilities.
Figure 1 in Further morphological and molecular studies of driftwood hoppers (Crustacea: Amphipoda: Talitridae) from Mediterraneanłnorth-east Atlantic coastlines
Figure 1. Scatterplots and fitted linear regressions for: (A) Pl3 ExL on TBL in O. mediterranea from Ria Formosa, Faro, Portugal, for all life history stages (♦); and O. microphtalma from Cap Ferret, France (▀). (B) A2 FA on TBL in O. microphtalma from Cap Ferret, France (★) and M. remyi from Principina a Mare, Italy (♦).
Figure 2 in Further morphological and molecular studies of driftwood hoppers (Crustacea: Amphipoda: Talitridae) from Mediterraneanłnorth-east Atlantic coastlines
Figure 2. Scatterplots and fitted regression lines for: (A) A2 PL on TBL for the unknown taxon from the Swale, UK (★) and juvenile O. mediterranea from the Medway estuary, UK (A). (B) ED on TBL for the unknown taxon from the Swale, UK (★) and juvenile O. mediterranea from the Medway estuary, UK (A).
40Ar/39Ar dating of the East Tenda Shear Zone: Chemical composition of white mica and ages data
<p>In order to clarify the link between <sup>40</sup>Ar/<sup>39</sup>Ar record in white mica and deformation, we performed <em>in situ</em> and bulkwise <sup>40</sup>Ar/<sup>39</sup>Ar dating over the East Tenda Shear Zone (Tenda massif, alpine Corsica). White micas from 11 samples were selected and extensively analyzed using <em>in situ</em> techniques across nested scales of strain-intensity gradients developed at the expense of a Late-Variscan protolith. <sup>40</sup>Ar/<sup>39</sup>Ar systematics are unaffected by inherited Ar and directly linked to deformation with little or no Ar lattice (volume) diffusion. Extensive sampling allows constraining the end of deformation related to burial and exhumation respectively at ~34 and ~22 Ma, bracketing the duration of regional extensional shear to ~12 Myr. Results also highlight a regional strain localization toward the upper contact of the unit with smaller-scale localization in specific lithologies, notably meta-aplites.</p> <p> Second-order complications exist, such as local ill-defined correlations between ages and finite-strain microstructures. Thus, the use of a strain gradient as a proxy for strain localization in time is regionally valid but sometimes locally too complex to track or resolve strain partitioning/localization trends at the meter (outcrop) scale and below. Age mixing and incomplete isotopic homogenization by dissolution/precipitation are identified as the main causes of local discrepancies that complicate the link between age and microstructure and the derivation of strain localization rates. Tracking temporal trends in shear distribution across regional-scale deformation gradients in such settings is possible but requires a multi-scale approach as implemented here to reveal younging patterns associated to strain localization.</p>
Analyzing and predicting urban land use forms in East Africa using OpenStreetMap data, satellite imagery, and Convolutional Networks
<p>This multi-spectral satellite image data set is associated with our recent work on analyzing and predicting urban land use forms in East Africa using OpenStreetMap data, satellite imagery, and Convolutional Neural Networks.</p> <p>The images were extracted using an automated Python script from Google Maps Static API, based on sample locations in four East African capital cities namely Kampala, Nairobi, Dar es Salaam, and Kigali.</p> <p>Other data sets associated with this work, that is, ESRI shapefiles for administrative level 1 and OpenStreetMap data for the named cities may be downloaded directly from the respective URLs provided in the manuscript.</p>
East Coast Low Database Southeast Australia
<p>This east coast low (ECL) database 1970-2019 adjacent to the south east coast of Australia updates the database from 1970-2006 (Speer et al. 2009). This new database is restricted to April-September and records the initial date that a ECL forms in the area, its latitude/longitude position, central pressure on initial development and lowest pressure (strongest intensity), as shown on the Australian Bureau of Meteorology archived MSLP charts. In addition, if the ECL experiences a 24 h pressure drop greater than or equal to 10 hPa at 00 UTC, the date immediately at the end of the pressure drop is recorded. The data were grouped in 7 synoptic categories, as in Speer et al. (2009), followed by a division of those 7 that formed either in an easterly or westerly wind regime.</p> <p>Speer, MS., Wiles, P., Pepler, A. 2009. <em>Low pressure systems off the New South Wales coast and associated hazardous weather: establishment of a database.</em> <strong>Aust. Met. Mag., 58</strong>, 29-39.</p> <p>Speer, M.S., Leslie, L.M., Hartigan, J., MacNamara, S. <em>Trends in east coast low pressure systems affecting the southeast of Australia. </em><strong>J. South. Hemisphere Earth Sys. Sci. </strong><em>(in review)</em></p>
Holocene regional population dynamics and climatic trends in the Near East: a first comparison using archaeo-demographic proxies (dataset and R scripts)
<p>The present digital archive is the outcome of the paper: <strong>Palmisano, A., Lawrence, D., de Gruchy, M.W., Bevan, A., and Shennan, S., 2021. <a href="https://doi.org/10.1016/j.quascirev.2020.106739">Holocene regional population dynamics and climatic trends in the Near East: a first comparison using archaeo-demographic proxies</a>. <em>Quaternary Science Reviews</em>, <em>252</em></strong>.</p> <p>The dataset included here provides a collection of <strong>10,606</strong> radiocarbon dates, <strong>1884</strong> sites from archaeological surveys (1336 from Central Anatolia and 478 from Upper Mesopotamia) and <strong>16</strong> palaeoclimatic records for a period spanning between 14,000 and 2500 BP. In addition, the digital archive related to this paper provides reproducible analyses in the form of four scripts written in R statistical computing language.</p> <p>List of versions:</p> <ul> <li><strong>2.0.</strong> 15 December 2020 — Includes a few minor error corrections (the files 'References.txt' within the folder csv and the script 'radiocarbon.R').</li> <li><strong>1.0</strong> 28 November 2020 — First public release of the dataset on Zenodo.</li> </ul>
A Bloody Difficult Woman: Mayalee Dancing Girl Vs. the East India Company
<p>The images that accompany this podcast may be found here: <a href="https://gate.sc?url=https%3A%2F%2Fblogs.bl.uk%2Fasian-and-african%2F2019%2F03%2Fmusicians-and-dancers-in-the-india-office-records.html&token=2f0bcb-1-1609324650767">blogs.bl.uk/asian-and-african/2…office-records.html</a></p> <p>In 1818, the East India Company signed a treaty with the autonomous Rajput states of Jaipur and Jodhpur, offering British political and military protection in exchange for heavy cash tribute. By the early 1830s, these states were swimming in debt and increasingly resisting the Company's influence. So in 1835 the Company took direct control over the revenue of the salt lake at Sambhar, still one of India’s largest sources of that most precious of commodities, salt. Sambhar Lake was returned to Jaipur's and Jodhpur’s control in 1842 when, having been brought to the brink of ruin by the Company’s protection racket, their arrears were written off by the Government in Calcutta. Short-lived and little-studied, the Sambhar Lake affair left behind a set of financial accounts in the East India Company records that are alive with details of musicians and dancers, the cycle of Sambhar's festival year, and the economics of such cultural production.</p> <p>One musician in particular stands forth from Jaipur's accounts as exceptional, Mayalee “dancing girl”. As well as being paid a monthly cash stipend, she received 25 maunds of salt annually, and was clearly one of Sambhar’s chief courtesans. Little exculpatory notes in the margins of successive Company accounts reveal that Mayalee successfully resisted the Company’s attempt to force her to give up her salt stipend in exchange for cash. Was she merely protecting a nice little sideline selling salt? Or did the more lofty ideal of “faithfulness to the salt” (namak-halali) underpin her resistance? In this podcast I consider why Indian musicians and especially courtesans appear at all in the official records of the East India Company, and what this tells us about relations between the British colonial state and the Indian peoples whose worlds it was increasingly encroaching upon during the 1830s and 40s.</p> <p>This podcast is part of the series <a href="https://soundcloud.com/user-513302522">Histories of the Ephemeral: Writing on Music in Late Mughal India</a>, sponsored by the British Academy in association with the British Library; additional research was funded by the European Research Council.</p> <p>Mayalee Dancing Girl vs the East india Company was written by me, Katherine Butler Schofield (King's College London), and is based on my original research. It was produced by Chris Elcombe. Additional voices were Michael Bywater, Chris Elcombe, and Kanav Gupta. It is published under a Creative Commons Attribution Non-Commercial No Derivatives (CC–BY-NC–ND) license.</p> <p>The recording of Rag Jaunpuri by Jaipur gharana doyenne Kesarbai Kerkar is courtesy of the Archive of Indian Music and Vikram Sampath. <a href="https://soundcloud.com/archive-of-indian-music/kesarbai-kerkar">Archive-of-indian-music – Kesarbai-kerkar</a></p> <p>The sarangi recording of Rag Bhairavi is by Nicolas Magriel and reproduced with thanks.</p> <p>Information on the Jaipur gunijan-khana is taken from the work of Joan Erdman, and material on Amber/Jaipur’s political life from the work of Giles Tillotson and Monika Horstmann.</p> <p>With thanks to: the British Academy, the British Library, the National Archives of India, the European Research Council, Norbert Peabody, Paul Schofield, and Mrinalini Venkateswaran.</p> <p>Flute and Drum, Rishikesh by Samuel Corwin CC BY 4.0</p> <p>Prayer Temple Jaipur by Xserra CC BY 4.0</p> <p>20160922_summers.end.marshes by dobroide CC BY 4.0</p> <p>Waves on the Lake by Vlatko Blazek CC BY 4.0</p> <p>Kirtana_in_Hindi by psubhashish CC BY 4.0</p> <p>Water Music From the Handel Show by The United States Army Old Guard Fife and Drum Corps Public Domain Mark 1.0 Licence</p> <p>Ganga Aarti Ceremony V, Haridwar by Samuel Corwin CC BY 4.0</p> <p>Shiva Worship Ceremony, Varanasi by Samuel Corwin CC BY 4.0</p> <p>A Man Approaches with Bowed Sitar, Rishikesh by Samuel Corwin CC BY 4.0</p> <p>Track 1 by Deep Singh and Ikhlaq Hussain Khan<br> Originally broadcast live on Rob Weisberg's show, Transpacific Sound Paradise on WFMU. CC BY NC SA 3.0</p>
FIG. 3 in New molecular and morphological evidences favor a combination of Blechnum bakeri C.Chr. in Cranfillia Gasper & V.A.O.Dittrich (Blechnaceae, Polypodiopsida), thus extending the distribution of Cranfillia to Madagascar and East Africa
FIG. 3. — Spores of Cranfillia and Austroblechnum as observed with SEM: A, B, C. bakeri Vázquez Ferreira & S.Molino, comb. nov. (MA389177); C, D, C. mucronata (MA655870 & UC1615719, respectively); E, F, A. lherminieri (Bory ex Kunze) Gasper & V.A.O.Dittrich (BA57587). Thick and straight muri are visible in Cranfillia, as well as the spongy-trabecular middle layer of the perine (B and D). Smooth and micro-granulated perine ornamentation is observed in A. lherminieri. Scale bar: A, 17 µm; B, 9 µm; C, 7 µm; D, 1 µm; E, 8 µm; F, 2 µm.
FIG. 2 in New molecular and morphological evidences favor a combination of Blechnum bakeri C.Chr. in Cranfillia Gasper & V.A.O.Dittrich (Blechnaceae, Polypodiopsida), thus extending the distribution of Cranfillia to Madagascar and East Africa
FIG. 2. — Morphology of sterile pinnae in Cranfillia species: A, Sterile frond of C. fullagari (K001092750); B-E, Basal pinnae morphology; B, C. opaca (US1431859); C, C. bakeri Vázquez Ferreira & S.Molino, comb. nov. (P00483198); D, C. mucronata (P01389538); E, C. nigra (K001092713). Scale bar: A, 28 mm; B, 6 mm; C, 10 mm; D, 17 mm; E, 7 mm.
ScienceDex guides
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These curated guides explain access requirements, typical timelines, costs, and reuse considerations for widely used research datasets.
Allen Brain Atlas
Allen Brain Atlas is an Allen Institute collection of brain map atlases, datasets, APIs, and analysis tools covering mouse, human, and non-human primate brain resources.
Annotated Behaviour and Observability Dataset (ABODe)
ABODe is a University of Edinburgh DataShare dataset for behavior classification in group-housed mice using home-cage video, identities, bounding boxes, ground-plate positions, and annotator labels.
DANDI Archive for NWB datasets
DANDI is a BRAIN Initiative archive for publishing and sharing neurophysiology data, including electrophysiology, optophysiology, and behavioral data packaged as NWB and related standards.
International Brain Laboratory public data
The International Brain Laboratory public data releases expose standardized mouse decision-making experiments, including Neuropixels recordings, widefield calcium imaging, behavior, and session metadata accessed through the ONE API.
OpenNeuro
OpenNeuro is a free, open platform for sharing neuroimaging datasets, with public search, dataset pages, and download paths for web, S3, DataLad, and the OpenNeuro CLI.