Find research datasets worth reusing
Search datasets from major research repositories and use ShareScore to quickly assess how well each record supports discovery, access, and reuse.
1,810
datasets available to search
ShareScore release 0.9.0
Dataset results
1,810 results for “species range”
Fig. 7. Dordrecht Mountain, where a in Neoclita pringlei (Scarabaeidae, Cetoniinae), a new relict genus and species from the Drakensberg Range of South Africa
Fig. 7. Dordrecht Mountain, where a second population of Neoclita pringlei gen. et sp. nov. was frst recorded in Dec. 2013 (photo: Lynette Clennell, Dordrecht, 31 Dec. 2015).
Fig. 1 in Neoclita pringlei (Scarabaeidae, Cetoniinae), a new relict genus and species from the Drakensberg Range of South Africa
Fig. 1. Neoclita pringlei gen. et sp. nov., holotype, ♂, total length = 16.3 mm. A. Habitus, dorsal view. B. Habitus, ventral view. (South Africa, Eastern Cape Province, Matatiele Nature Reserve, 6 Dec. 2008, R. Perissinotto and L. Clennell leg.)
Supplementary material 1 from: Hejda M (2013) Do species differ in their ability to coexist with the dominant alien Lupinus polyphyllus? A comparison between two distinct invaded ranges and a native range. NeoBiota 17: 39-55. https://doi.org/10.3897/neobiota.17.4317
Entry data for the univariate models with species richness as a response variable. (doi: 10.3897/neobiota.17.4317.app1) File format: Micrisoft Excell document (xls). :
FIGURE 4 in Taxon-specific variability of leaf traits in three long-ranging fossil-species of the Paleogene and Neogene: Responses to climate?
FIGURE 4. Site-specific data for lamina length and lamina width plotted for each taxon. 4A: Lamina length for Platanus neptuni. 4B: Lamina width for P. neptuni. 4C: Lamina length for Eotrigonobalanus furcinervis. 4D: Lamina width for E. furcinervis. 4E: Lamina length for Daphnogene cinnamomifolia. 4F: Lamina width for D. cinnamomifolia. The boxes span the 50% interquartile. The horizontal lines within the boxes indicate the median values. The "whiskers" mark the highest and lowest values. Outliers located at a distance of up to 1.5 times the quartile span outside the whiskers are drawn as asterisks, and extreme outliers are drawn as circles. Different minuscule letters indicate statistically significant differences among sites. Colors indicate deposit type. Colors indicate deposit type. Green: fluviatile. Red: volcanic. Blue: marine. Lines delimit age groups. LE: Late Eocene. EO: Early Oligocene. LO: Late Oligocene. EM: Early Miocene. For site numbers and dating see Table 1.
FIGURE 1 in Taxon-specific variability of leaf traits in three long-ranging fossil-species of the Paleogene and Neogene: Responses to climate?
FIGURE 1. Map showing the locations of the considered sites, which are numbered according to Table 1.
FIGURE 3 in Taxon-specific variability of leaf traits in three long-ranging fossil-species of the Paleogene and Neogene: Responses to climate?
FIGURE 3. Site-specific data for lamina area and lamina perimeter plotted for each taxon. 3A: Lamina area for Platanus neptuni. 3B: Lamina perimeter for P. neptuni. 3C: Lamina area for Eotrigonobalanus furcinervis. 3D: Lamina perimeter for E. furcinervis. 3E: Lamina area for Daphnogene cinnamomifolia. 3F: Lamina perimeter for D. cinnamomifolia. The boxes span the 50% interquartile. The horizontal lines within the boxes indicate the median values. The "whiskers" mark the highest and lowest values. Outliers located at a distance of up to 1.5 times the quartile span outside the whiskers are drawn as asterisks, and extreme outliers are drawn as circles. Different minuscule letters indicate statistically significant differences among sites. Colors indicate deposit type. Green: fluviatile. Red: volcanic. Blue: marine. Lines delimit age groups. LE: Late Eocene. EO: Early Oligocene. LO: Late Oligocene. EM: Early Miocene. For site numbers and dating see Table 1.
FIGURE 6 in Taxon-specific variability of leaf traits in three long-ranging fossil-species of the Paleogene and Neogene: Responses to climate?
FIGURE 6. Site-specific data for lamina centroid and leaf length-to-width ratio (LWR) plotted for each taxon. 6A: Lamina centroid for Platanus neptuni. 6B: LWR for P. neptuni. 6C: Lamina centroid for Eotrigonobalanus furcinervis. 6D: LWR for E. furcinervis. 6E: Lamina centroid for Daphnogene cinnamomifolia. 6F: LWR for D. cinnamomifolia. The boxes span the 50% interquartile. The horizontal lines within the boxes indicate the median values. The "whiskers" mark the highest and lowest values. Outliers located at a distance of up to 1.5 times the quartile span outside the whiskers are drawn as asterisks, and extreme outliers are drawn as circles. Different minuscule letters indicate statistically significant differences among sites. Colors indicate deposit type. Colors indicate deposit type. Green: fluviatile. Red: volcanic. Blue: marine. Lines delimit age groups. LE: Late Eocene. EO: Early Oligocene. LO: Late Oligocene. EM: Early Miocene. For site numbers and dating see Table 1.
FIGURE 2 in Taxon-specific variability of leaf traits in three long-ranging fossil-species of the Paleogene and Neogene: Responses to climate?
FIGURE 2. Plasticity index (PI) of various leaf traits, for the considered sites and taxa. 2A: PI for lamina area. 2B: PI for lamina length. 2C: PI for lamina perimeter. 2D: PI for lamina width. 2E: PI for lamina circularity. 2F: PI for lamina centroid. Squares: Platanus neptuni. Circles: Daphnogene cinnamomifolia. Triangles: Eotrigonobalanus furcinervis. Colors indicate deposit type. Green: fluviatile. Red: volcanic. Blue: marine. Lines delimit age groups. LE: Late Eocene. EO: Early Oligocene. LO: Late Oligocene. EM: Early Miocene. For site numbers and dating see Table 1.
FIGURE 5 in Taxon-specific variability of leaf traits in three long-ranging fossil-species of the Paleogene and Neogene: Responses to climate?
FIGURE 5. Site-specific data for lamina circularity and lamina roundness plotted for each taxon. 5A: Lamina circularity for Platanus neptuni. 5B: Lamina roundness for P. neptuni. 5C: Lamina circularity for Eotrigonobalanus furcinervis. 5D: Lamina roundness for E. furcinervis. 5E: Lamina circularity for Daphnogene cinnamomifolia. 5F: Lamina roundness for D. cinnamomifolia. The boxes span the 50% interquartile. The horizontal lines within the boxes indicate the median values. The "whiskers" mark the highest and lowest values. Outliers located at a distance of up to 1.5 times the quartile span outside the whiskers are drawn as asterisks, and extreme outliers are drawn as circles. Different minuscule letters indicate statistically significant differences among sites. Colors indicate deposit type. Colors indicate deposit type. Green: fluviatile. Red: volcanic. Blue: marine. Lines delimit age groups. LE: Late Eocene. EO: Early Oligocene. LO: Late Oligocene. EM: Early Miocene. For site numbers and dating see Table 1.
FIGURE 7. Age-specific discriminant analysis using all morphometric parameters for all sites. 7A in Taxon-specific variability of leaf traits in three long-ranging fossil-species of the Paleogene and Neogene: Responses to climate?
FIGURE 7. Age-specific discriminant analysis using all morphometric parameters for all sites. 7A: Eocene. 7B: Oligocene. Triangles: Platanus neptuni. Squares: Eotrigonobalanus furcinervis. Circles: Daphnogene cinnamomifolia.
FIGURE 8 in Taxon-specific variability of leaf traits in three long-ranging fossil-species of the Paleogene and Neogene: Responses to climate?
FIGURE 8. Circularity plotted against LWR. Blue circles: Platanus neptuni. Red squares: Eotrigonobalanus furcinervis. Yellow diamonds: Daphnogene cinnamomifolia. Black line: Relationship between circularity and length-towidth ratio of an ellipse. Please note that this relationship was calculated by using an approximate equation for the perimeter of an ellipse, which causes the slight deflection of the curve for high circularity values. As approximation, the following equation for the ellipse perimeter (EP) was used: EP = π* [2 * (a2 + b2)1/2].
Figs 28–34 in Acrobasis khachella (Amsel, 1950): Little-known snout moth species and new data about its range and habitats (Lepidoptera, Pyralidae, Phycitinae)
Figs 28–34. Acrobasis khachella (Amsel, 1950),genitalia: 28–30 —male genitalia; 31–34 —female genitalia: 28 — Kazakhstan, Dzhungarsky Alatau Mts., Usek river valley; 29 — Kyrgyzstan, Moldo-Too Mts., near the Koro-Goo Pass; 30 — Tajikistan, Shakhdarinsky Mts., Vezdara river valley; 31 — Kazakhstan, Dzhungarsky Alatau Mts., Usek river valley; 32 — Kyrgyzstan, Fergansky Mts., southern shore of Toktogul reservoir near the settlement Imeni Chkalova; 33 — Kyrgyzstan, Moldo-Too Mts., near the Koro-Goo Pass; 34 — Tajikistan, Shakhdarinsky Mts., Vezdara river valley Рис. 28–34. Acrobasis khachella (Amsel, 1950), генитаΛии: 28–30 — генитаΛии самца; 31–34 — генитаΛии самки: 28 — Казахстан, хр. Δжунгарский АΛатау, ΑоΛина р. Усек; 29 — Киргизия, хр. МоΛΑо-Тоо, бΛиз пер. Коро-Гоо; 30 — ТаΑжикистан, ШахΑаринский хр., ΑоΛина р. ВезΑара; 31 — Казахстан, хр. Δжунгарский АΛатау, ΑоΛина р. Усек; 32 — Киргизия, Ферганский хр., южный берег ТоктогуΛьского вΑхр. бΛиз пос. имени ЧкаΛова; 33 — Киргизия, хр. МоΛΑо-Тоо, бΛиз пер. Коро-Гоо; 34 — ТаΑжикистан, ШахΑаринский хр., ΑоΛина р. ВезΑара
Figs 35–42 in Acrobasis khachella (Amsel, 1950): Little-known snout moth species and new data about its range and habitats (Lepidoptera, Pyralidae, Phycitinae)
Figs 35–42. Acrobasis khachella (Amsel, 1950), habitats: Kyrgyzstan: 35 — Talassky Mts., Kara-Buura river bank; 36 — Alai Mts., Kyzyl-Eshme valley; 37 — Moldo-Too Mts., Koro-Goo Pass environs; 38 — Dzhumgaltoo Mts., Sary-Kaiky gorge near Kojomkul; 39 — Kirghizsky Mts., Ala-Too settlement environs; 40 — Alai Mts., near Kara-Bulak; Kazakhstan: 41 — Dzhungarsky Alatau Mts., Usek river valley; Tajikistan: 42 — Shakhdarinsky Mts., Vezdara river valley (in the center: the author of this article with the local driver, Maziyo) Рис. 35–42. Acrobasis khachella (Amsel, 1950), биотопы: Киргизия: 35 — ТаΛасский хр., побережье р. Кара-Буура; 36 — АΛайский хр., ущ. КызыΛ-Эшме; 37 — хр. МоΛΑо-Тоо, окр. пер. Коро-Гоо; 38 — хр. ΔжумгаΛтоо, массив Сары-Кайкы бΛиз пос. КожомкуΛ; 39 — Киргизский хр., окр. пос. АΛа-Тоо; 40 — АΛайский хр., бΛиз пос. Кара-БуΛак; Казахстан: 41 — хр. Δжунгарский АΛатау, ΑоΛина р. Усек; ТаAжикистан: 42 — ШахΑаринский хр., ΑоΛина р. ВезΑара (в центре: автор настоящей работы и местный воΑитеΛь, Мазиё)
Figs 1–27 in Acrobasis khachella (Amsel, 1950): Little-known snout moth species and new data about its range and habitats (Lepidoptera, Pyralidae, Phycitinae)
Figs 1–27. Acrobasis khachella (Amsel, 1950), upper sides: 1 — Kyrgyzstan, Kirghizsky Mts., Ala-Too environs; 2 — Kazakhstan, Dzhungarsky Alatau Mts., Usek river valley; 3 — Tajikistan, Shakhdarinsky Mts., Vezdara river valley; 4 — Kyrgyzstan, Fergansky Mts., southern shore of Toktogul reservoir near Imeni Chkalova; 5 — Kyrgyzstan, Alai Mts., Kyzyl-Eshme valley; 6–8 — Kyrgyzstan, Alai Mts. near Kara-Bulak; 9–14 — Kyrgyzstan, Talassky Mts., Kara-Buura river valley; 15–18 — Kyrgyzstan, Fergansky Mts., Kara-Suu river valley; 19 — Kyrgyzstan, south shore of the Issyk Kul Lake near Kara-Talaa; 20–27 — Kyrgyzstan, Moldo-Too Mts., near the Koro-Goo Pass. 1, 9, 23, 24 — females, the remaining specimens — males. Scale bar: 1 cm Рис. 1–27. Acrobasis khachella (Amsel, 1950), виΑ сверху: 1 — Киргизия, Киргизский хр., окр. пос. АΛа-Тоо; 2 — Казахстан, хр. Δжунгарский АΛатау, ΑоΛина р. Усек; 3 — ТаΑжикистан, ШахΑаринский хр., ΑоΛина р. ВезΑара; 4 — Киргизия, Ферганский хр., южный берег ТоктогуΛьского вΑхр. бΛиз пос. имени ЧкаΛова; 5 — Киргизия, АΛайский хр., ущ. КызыΛ-Эшме; 6–8 — Киргизия, АΛайский хр. бΛиз пос. Кара-БуΛак; 9–14 — Киргизия, ТаΛасский хр., ΑоΛина р. Кара-Буура; 15–18 — Киргизия, Ферганский хр., ΑоΛина р. Кара-Суу; 19 — Киргизия, южный берег оз. Иссык-КуΛь бΛиз пос. Кара-ТаΛаа; 20–27 — Киргизия, хр. МоΛΑо-Тоо, бΛиз пер. Коро-Гоо; 1, 9, 23, 24 — самки, остаΛьные — самцы. Масштабная метка: 1 см
Variable species establishment in response to microhabitat indicates different likelihoods of climate-driven range shifts
<p>Climate change is causing geographic range shifts globally, and understanding the factors that influence species' range expansions is crucial for predicting future biodiversity changes. A common, yet untested, assumption in forecasting approaches is that species will shift beyond current range edges into new habitats as they become macroclimatically suitable, even though microhabitat variability could have overriding effects on local population dynamics. We aim to better understand the role of microhabitat in range shifts in plants through its impacts on establishment by Q1) examining microhabitat variability along large macroclimatic (i.e., elevational) gradients, Q2) testing which of these microhabitat variables explain plant recruitment and seedling survival, and Q3) predicting microhabitat suitability beyond species range limits. We transplanted seeds of 25 common tree, shrub, forb, and graminoid species across and beyond their current elevational ranges in the Washington Cascade Range, USA, along a large elevational gradient spanning a broad range of macroclimates. Over five years, we recorded recruitment, survival, and microhabitat (i.e., high resolution soil, air, and light) characteristics rarely measured in biogeographic studies. We asked whether microhabitat variables correlate with elevation, which variables drive species establishment, and whether microhabitat variables important for establishment are already suitable beyond leading range limits. We found that only 30% of microhabitat parameters covaried with elevation. We further observed extremely low recruitment and moderate seedling survival, and these were generally only weakly explained by microhabitat. Moreover, species and life stages responded in contrasting ways to soil biota, soil moisture, temperature, and snow duration. Microhabitat suitability predictions suggest that distribution shifts are likely to be species-specific, as different species have different suitability and availability of microhabitat beyond their present ranges, thus calling into question low-resolution macroclimatic projections that will miss such complexities. We encourage further research on species responses to microhabitat and including microhabitat in range shift forecasts.</p>
Рис. 1. Sicista betulina: 1 — Λесная мышовка, пойманная в окрестностях сеΛа КойÀа; 2 — карта распространения виÀа: зеΛеная заΛивка — ареаΛ виÀа по Burgin et al. 2020, синие звезÀочки — точки нахоÀок в национаΛьном парке «Онежское Поморье» и на СоΛовецком архипеΛаге (Черенкова 2014), красный круг — новая нахоÀка в районе Àеревни КойÀа; 3–4 — биотопы, в которых быΛ встречен виÀ в окрестностях сеΛа КойÀа Fig. 1. Sicista betulina: 1 — the northern birch mouse caught in the vicinity of Koida village; 2 — the species distribution map: the green fill — species range according to Burgin et al. 2020; the blue stars — points where the species was found in the Onezhskoye Pomorye National Park and on the Solovetsky Archipelago (Cherenkova 2014); the red circle — a new find in the area of Koida village; 3–4 — biotopes in which the species was encountered in the vicinity of Koida village in A new record of the northern birch mouse Sicista betulina (Pallas, 1779) in the north of the Arkhangelsk Region (Rodentia: Sminthidae)
Рис. 1. Sicista betulina: 1 — Λесная мышовка, пойманная в окрестностях сеΛа КойÀа; 2 — карта распространения виÀа: зеΛеная заΛивка — ареаΛ виÀа по Burgin et al. 2020, синие звезÀочки — точки нахоÀок в национаΛьном парке «Онежское Поморье» и на СоΛовецком архипеΛаге (Черенкова 2014), красный круг — новая нахоÀка в районе Àеревни КойÀа; 3–4 — биотопы, в которых быΛ встречен виÀ в окрестностях сеΛа КойÀа Fig. 1. Sicista betulina: 1 — the northern birch mouse caught in the vicinity of Koida village; 2 — the species distribution map: the green fill — species range according to Burgin et al. 2020; the blue stars — points where the species was found in the Onezhskoye Pomorye National Park and on the Solovetsky Archipelago (Cherenkova 2014); the red circle — a new find in the area of Koida village; 3–4 — biotopes in which the species was encountered in the vicinity of Koida village
Figure 1 in Why may the same species have different elevational ranges at different sites in New Guinea?
Figure 1. Example of the Massenerhebung effect: variation in the elevational ceiling and floor of the Island Leaf Warbler Seicercus poliocephalus on New Guinea mountains. Note that the warbler's ceiling (upper graph) and floor (lower graph) are higher on Central Range peaks than on outlier peaks; that they tend to be higher on higher peaks (summit elevation, abscissa); that they tend to be higher on inland-facing or interior-facing outlier transects than on coast-facing outlier transects; and that they tend to be higher on outlier transects further from the coast than on outlier transects nearer the coast. Data from Table 4.
Figure 2 in Why may the same species have different elevational ranges at different sites in New Guinea?
Figure 2. Google Earth view of the environment of Diamond's 1979 Foja coastal transect. Visible are the narrow north-flowing stream on which Diamond's camp was sited; the western and eastern ridges flanking the valley in which the stream lies; at the bottom of the field of view, the ridges south of Diamond's camp, rising towards the Foja summits; the near-vertical east / west barrier ridge constituting the northern flank of the basin, and pierced by the stream; and, at the top, New Guinea's lowland coastal plain beyond the east / west ridge, and in which the stream flows in a braided gravel bed. A line traces the crest of the western, eastern and northern ridges, with numbers denoting elevation readings in metres. Diamond's camp in the basin, labelled 610 m, was at 02°45'S, 138°63'E.
Figure 3 in Why may the same species have different elevational ranges at different sites in New Guinea?
Figure 3. Google Earth close-up view, from the south, of the east / west ridge closing to the north the basin viewed in Fig. 2. The ridge has near-vertical southern and northern faces, and is pierced by the basin's stream via a cleft only c.20 m wide.
Phylogeography and paleoclimatic range dynamics explain variable outcomes to contact across a species' range
<p>Files required to run analyses related to the journal article:" Phylogeography and paleoclimatic range dynamics explain variable outcomes to contact across a species’ range."<br><br>Code which utilizes these data are found at: https://github.com/k-lamb/Campanula-range-history</p> <p>DOI code link: https://doi.org/10.5281/zenodo.12097775</p>
ScienceDex guides
Understand access before you commit
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.