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9 results for “cave climate”
Data for: "Climatic drivers of (changes in) bat migration phenology at Bracken Cave (USA)"
<p>This dataset contains the spring and autumn migration phenology dataset used in Haest <em>et al.</em> (2020) to determine the drivers of migration phenology of Brazilian free-tailed bats at Bracken Cave (USA) over the period 1995-2017. The phenology dataset was derived from nightly colony population sizes estimated using weather radar data (Stepanian <em>et al.</em>, 2018). See the Materials and Methods section in Haest <em>et al.</em> (2020) for more details on the dataset. </p> <p>References:</p> <p>Haest, B., Stepanian, P. M., Wainwright, C. E., Liechti, F., & Bauer, S. (2021). Climatic drivers of (changes in) bat migration phenology at Bracken Cave (USA). <em>Global Change Biology</em>, 27(4), 768-780. <a href="https://doi.org/10.1111/gcb.15433">https://doi.org/10.1111/gcb.15433</a></p> <p>Stepanian, P. M., & Wainwright, C. E. (2018). Ongoing changes in migration phenology and winter residency at Bracken Bat Cave. <em>Global Change Biology</em>, <em>24</em>(7), 3266–3275. <a href="https://doi.org/10.1111/gcb.14051">https://doi.org/10.1111/gcb.14051</a></p> <p> </p>
Data from: Ancient climate changes and relaxed selection shape cave colonization in North American cavefishes
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Data from: Climate change may drive cave spiders to extinction
Subterranean ecosystems present ideal opportunities to study mechanisms underlying responses to changes in climate because species within them are often adapted to a largely constant temperature. We have characterized the thermal conditions of caves in the Western Alps, and related these hypogean climate data to the occurrence of Troglohyphantes spiders (Araneae, Linyphiidae). Our data indicated that present distributions reflect Pleistocene glaciation events and also pointed to specific responses as a consequence of changes in temperature. Constant temperatures recorded inside caves provide an approximation of the mean annual temperature outside, thus we extended the results to a regional scale. We used ecological niche modeling to predict habitat suitability both in the Pleistocene and under future global warming scenarios. These analyses pointed toward a future decline in habitat suitability for subterranean spiders and the potential extinction of the most restricted endemic species. When compared with other species that live in confined habitats such as islands and mountains, we expect cave species to be as much, if not more, vulnerable to climate change.
Fig. 4 in Climate Relicts: Asian Scorpion Family Pseudochactidae Survived Miocene Aridification in Caves of the Annamite Mountains
Fig. 4. Estimation of ancestral ranges for the relictual Asian scorpion family Pseudochactidae Gromov 1998 in four biogeographical regions: Tajik and north Pamir blocks (northern Afghanistan and southern China, Uzbekistan and Tajikistan) (A); western Cimmeria, including only the Farah, Helmand, south and central Pamirs (SP and CP, respectively), Karakorum (K) and Band-e Bayan (BB) blocks (present-day Afghanistan and northern Pakistan) (B); northwest Annamite Mountains (Khammouan Karst, Laos) (C); northeast Annamite Mountains (Phong Nha-Ke Montenat (2009), Collett et al. (2015), Robinson (2015), Siehl (2017), and Li et al. (2020).
Fig. 3 in Climate Relicts: Asian Scorpion Family Pseudochactidae Survived Miocene Aridification in Caves of the Annamite Mountains
Fig. 3. Estimation of divergence times (A) in evolution of the relictual Asian scorpion family Pseudochactidae Gromov 1998 with palaeogeographical reconstructions (B) indicating tectonic positions and past and present plate boundaries. Geological time periods on phylogeny include Devonian, Carboniferous, Permian,Triassic, Jurassic, Cretaceous, and Cenozoic. Divergence ages (in millions of years) plotted on phylogeny. Circled numbers denote three divergence events leading to Pseudochactidae and its three subfamilies.Timeline for origins, dispersal, and diversification of Pseudochactidae as follows: Carboniferous (340 Ma), Pseudochactidae originates near Tajik block (colored grey area), situated among chain of continental blocks and island arcs between Turkestan and Palaeo-Tethys Oceans. Jurassic–Triassic Boundary (202 Ma): Cimmerian continent collides with Eurasia and Indochina in the Jurassic, allowing ancestor of
Fig. 2 in Climate Relicts: Asian Scorpion Family Pseudochactidae Survived Miocene Aridification in Caves of the Annamite Mountains
Fig. 2. Preferred phylogeny (A) of the relictual Asian scorpion family Pseudochactidae Gromov 1998 based on simultaneous analysis of the morphological and molecular datasets using Maximum Likelihood with unambiguous morphological synapomorphies optimized. Black circles indicate uniquely derived apomorphic states, white circles, parallel deviations of apomorphic states. Numbers above circles indicate characters, numbers below indicate states (Supp Appendices 2 and 3 [online only]). Dorsal habitus (B–F) of five species of Pseudochactidae: Pseudochactas ovchinnikovi Gromov 1998, Babatag, Uzbekistan, ♀ (AMNH) (B), Troglokhammouanus steineri Lourenço 2007,Tham Xe Bang Fai, Laos, ♀ (AMNH) (C), Aemngvantom thamnongpaseuam Prendini et al. 2021,Tham Nong Pa Seuam, Laos, holotype ♀ (AMNH) (D), Aemngvantom lao (Lourenço 2012),Tham Nam Lot (Lod), Laos, ♀ (AMNH) (E) and Vietbocap canhi Lourenço and Pham 2010,Tiên Sơn, Vietnam,♀ (AMNH) (F). Scale bars = 10 mm.
Fig. 1 in Climate Relicts: Asian Scorpion Family Pseudochactidae Survived Miocene Aridification in Caves of the Annamite Mountains
Fig. 1. Distribution of subfamilies of the relictual Asian scorpion family Pseudochactidae Gromov 1998: Pseudochactinae Gromov 1998, Troglokhammouaninae Prendini et al. 2021, Vietbocapinae Lourenço 2007.
Fig. 5 in Climate Relicts: Asian Scorpion Family Pseudochactidae Survived Miocene Aridification in Caves of the Annamite Mountains
Fig. 5. Preferred ancestral state reconstruction (A) for the relictual Asian scorpion family Pseudochactidae Gromov 1998 using ARD model of troglomorphism index (scale = 1–10) ranging from epigean (score = 1) to hypogean, troglobitic (score = 10). Ecomorphotypes classified as epigean (1–5); hypogean, troglophilic (6–8); and hypogean, troglobitic (9–10). Carapace (B–D) of three pseudochactid species, representing each ecomorphotype: epigean: Pseudochactas ovchinnikovi Gromov 1998 (B); troglophilic: Troglokhammouanus steineri Lourenço 2007 (C); and troglobitic: Vietbocap canhi Lourenço 2010 (D).
Data from: Climate change may drive cave spiders to extinction
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Allen Brain Atlas
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DANDI Archive for NWB datasets
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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.