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opencc-by-4.0Jul 2019View details →

Fig. 2 in Intraspecific Morphological Variation In Free- Living Stages Of Strongyloides Papillosus (Nematoda, Strongyloididae) Parasitizing Various Mammal Species

Fig. 2. Morphometric parameters of L1 of S. papillosus: а — body length; b — body width; c — length of esophagus; d — length of intestine; e — length of tail; on the ordinate axis — length in µm, on the abscissa axis — species of host (Ch — Capra hircus, Oc — Oryctolagus cuniculus, Cp — Cavia porcellus).

opencc-by-4.0Jul 2019View details →

Fig. 4 in Intraspecific Morphological Variation In Free- Living Stages Of Strongyloides Papillosus (Nematoda, Strongyloididae) Parasitizing Various Mammal Species

Fig. 4. Third-stage larva of S. papillosus: a — general view; b — anterior part (the pointer indicates the place where the esophagus joins the intestine); c — posterior part; scale bars 100 µm.

opencc-by-4.0Jul 2019View details →

Fig. 1 in Intraspecific Morphological Variation In Free- Living Stages Of Strongyloides Papillosus (Nematoda, Strongyloididae) Parasitizing Various Mammal Species

Fig. 1. Rhabditiform larvae of S. papillosus: a — L1 from C. hircus (arrowheads indicate the bulb-like dilatations on the esophagus and the tail); b — L1 from O. hircus (arrowheads indicate bulb-like dilatations on the esophagus and the tail); c — L2 from C. hircus (arrowheads indicate two bulb-like dilatations); scale bars 100 µm.

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Data and code for Winter conditions structure extratropical patterns of species richness of amphibians, birds, and mammals globally

<p>This repository contains the dataset analyzed in 'Winter conditions structure extratropical patterns of species richness of amphibians, birds, and mammals globally' - published in the journal Global Ecology and Biogeography - and the R code used to generate the correlations, generalized additive models, and related figures presented in the manuscript. Column descriptions for the data can be found in the associated README.txt file. Please refer to the manuscript for further detail on the variables and how they were derived.</p> <p>The Winter Indices (WIs) were derived using satellite remote sensing data from optical (MODIS, snow cover) and microwave (MEaSUREs freeze/thaw, frozen ground) sensors. The species richness maps were derived using IUCN range maps for individual species of amphibians, birds, and mammals (data requests can be made here: <a href="https://www.iucnredlist.org/resources/spatial-data-download">https://www.iucnredlist.org/resources/spatial-data-download</a>). Climatic varibales were derived from WorldClim v2.0 data, elevation from USGS GMTED2010 data, and primary productivity from the cumulative dynamic habitat index available here: <a href="http://silvis.forest.wisc.edu/maps-data/">http://silvis.forest.wisc.edu/maps-data/</a>.</p>

opencc-zeroApr 2022View details →

Text-fig. 6. Correlation of the Cheringoma and Mazamba formations on the basis of benthic foraminiferans and mammals respectively. Identifications of foraminiferans are from Newton (1924) and Abrard (1928), and the ranges of foraminiferans are from Sella-Kiel et al. (1998). The time scale is from Gradstein et al. (2020). The distribution of Nummulites atacicus is included, but it is not known whether it is reworked from older deposits. If the identification is valid, it would support the thesis that there was a period of Ypresian deposition in the vicinity during which remains of the species were fossilised. in Stratigraphy, Chronology And Palaeontology Of The Tertiary Rocks Of The Cheringoma Plateau, Mozambique

Text-fig. 6. Correlation of the Cheringoma and Mazamba formations on the basis of benthic foraminiferans and mammals respectively. Identifications of foraminiferans are from Newton (1924) and Abrard (1928), and the ranges of foraminiferans are from Sella-Kiel et al. (1998). The time scale is from Gradstein et al. (2020). The distribution of Nummulites atacicus is included, but it is not known whether it is reworked from older deposits. If the identification is valid, it would support the thesis that there was a period of Ypresian deposition in the vicinity during which remains of the species were fossilised.

FIGURE 10 in Palaeoecology and sea level changes: Decline of mammal species richness during late Quaternary island formation in the Montebello Islands, north-western Australia

FIGURE 10. Number of species identified from each spit in Morgan's Cave, illustrating the increasing loss of species from spits four to one.

FIGURE 9 in Palaeoecology and sea level changes: Decline of mammal species richness during late Quaternary island formation in the Montebello Islands, north-western Australia

FIGURE 9. Species-area plot for islands on the north-west continental shelf (filled circles) (data from Abbott and Burbidge, 1995), and spits one to seven in Morgan's Cave (open circles).

FIGURE 8 in Palaeoecology and sea level changes: Decline of mammal species richness during late Quaternary island formation in the Montebello Islands, north-western Australia

FIGURE 8. Log non-volant species vs log area plot for the north-west islands (filled circles) and the super-island at sea level 10 m below present (open circle).

FIGURE 6 in Palaeoecology and sea level changes: Decline of mammal species richness during late Quaternary island formation in the Montebello Islands, north-western Australia

FIGURE 6. Species accumulation curve for Morgan's Cave, showing increasing species with increased sampling effort (cumulative NISP). Further sampling effort could have yielded more species.

opencc-by-4.0Dec 2022View details →

Рис. 1. Δинамика чисΛенности меΛких мΛекопитающих в Цасучейском бору: 1 — суммарная чисΛенность (особей / 100 циΛинΑро-суток); Αоминирующие виΑы: 2 — забайкаΛьский хомячок, 3 — бурозубка тунΑряная, 4 — бурозубка крошечная, 5 — поΛёвка монгоΛьская, 6 — поΛёвка РаΑΑе, 7 — красная поΛёвка; A — остепнённый сосняк, B — первичная гарь, С — старая гарь, D — повторная гарь; стреΛка указывает время прохожΑения пожара. Ось X — гг., ось Y — чисΛенность Fig. 1. Population dynamics of small mammals in the Tsasucheysky Pine Forest: 1 — total abundance (individuals / 100 cylinder-days); dominant species: 2 — Cricetulus pseudogriseus, 3 — Sorex tundrensis, 4 — S. minutissimus, 5 — Alexandromys mongolicus, 6 — Lasiopodomys raddei, 7 — Myodes rutilus; A — steppe pine forest, B — primary burns site, С — old burns site; D — repeated burns site; the arrow indicates the time of the fire. The X-axis shows years; the Y-axis shows population density in Population dynamics of small mammals after spring fires in steppe pine forest

Рис. 1. Δинамика чисΛенности меΛких мΛекопитающих в Цасучейском бору: 1 — суммарная чисΛенность (особей / 100 циΛинΑро-суток); Αоминирующие виΑы: 2 — забайкаΛьский хомячок, 3 — бурозубка тунΑряная, 4 — бурозубка крошечная, 5 — поΛёвка монгоΛьская, 6 — поΛёвка РаΑΑе, 7 — красная поΛёвка; A — остепнённый сосняк, B — первичная гарь, С — старая гарь, D — повторная гарь; стреΛка указывает время прохожΑения пожара. Ось X — гг., ось Y — чисΛенность Fig. 1. Population dynamics of small mammals in the Tsasucheysky Pine Forest: 1 — total abundance (individuals / 100 cylinder-days); dominant species: 2 — Cricetulus pseudogriseus, 3 — Sorex tundrensis, 4 — S. minutissimus, 5 — Alexandromys mongolicus, 6 — Lasiopodomys raddei, 7 — Myodes rutilus; A — steppe pine forest, B — primary burns site, С — old burns site; D — repeated burns site; the arrow indicates the time of the fire. The X-axis shows years; the Y-axis shows population density

opencc-by-4.0Jul 2016View details →

Figure 3. A in Humpback whales interfering when mammal-eating killer whales attack other species: Mobbing behavior and interspecific altruism?

Figure 3. A mother humpback whale and newborn calf photographed off Baja California, Mexico, Oct 2009. When necessary, the mother will use her massive pectoral flippers to defend her small calf from attacking predators, especially killer whales. Photo: M. Lynn, NOAA, Southwest Fisheries Science Center.

opencc-by-4.0Jul 2016View details →

Figure 1 in Humpback whales interfering when mammal-eating killer whales attack other species: Mobbing behavior and interspecific altruism?

Figure 1. Locations and numbers of recorded interactions between humpback and killer whales described in Appendix S2 and summarized in Table 1; the number in each circle is the number of interactions from the general area.

Fig. 3. A in A new species of the plagiaulacoid multituberculate mammal Eobaatar from the Early Cretaceous of southern Britain

Fig. 3. A. Outline location map of Southern Britain. B. Outline geological map of the Isle of Wight.

Fig.10. A. BMNH M 45658 in A new species of the plagiaulacoid multituberculate mammal Eobaatar from the Early Cretaceous of southern Britain

Fig.10. A. BMNH M 45658, an I2 tentatively referred to Loxaulax valdensis from the Early Cretaceous Hastings Beds Group, mainland Britain, in occlusal (A1) and distal (A2) views, line drawing (A3) to show features giving the erroneous impression that BMNH M 45658 may be a left I3. See text for a discussion. B. BMNH M 45483 a left I3 assigned to Eobaatar clemensi from the Early Cretaceous Wessex Formation, Isle of Wight, in occlusal (B1) and anterolabial (B2) views, line drawing (B3) as seen in B2. C. Normal light photograph of an indeterminate plagiaulacoid left I2 (part of SMNS 51981) from the Early Cretaceous Wessex Formation, Isle of Wight, in labial view (it was not possible to obtain scanning electron micrographs of the specimen which was glued to card by the original collector).

Fig. 7 in A new species of the plagiaulacoid multituberculate mammal Eobaatar from the Early Cretaceous of southern Britain

Fig. 7. Scanning electron micrographs of plagiaulacoid multituberculate Eobaatar clemensi sp. nov. from the Early Cretaceous Wessex Formation, Isle of Wight. A. BMNH M 45482, holotype left m1 in occlusal (A1, stereo pair) and oblique distolingual (A2) views. B. BMNH M 45557, paratype left m1 in occlusal view (stereo pair).

Fig. 9 in A new species of the plagiaulacoid multituberculate mammal Eobaatar from the Early Cretaceous of southern Britain

Fig. 9. Plagiaulacoid multituberculate Eobaatar clemensi sp. nov. from the Early Cretaceous Wessex Formation, Isle of Wight. Scanning electron micrographs of BMNH M 45483, a multituberculate left I3, in mesiolabial (A), lingual (B), and occlusal (C, stereo pair) views.

Fig. 2. A, B in A new species of the plagiaulacoid multituberculate mammal Eobaatar from the Early Cretaceous of southern Britain

Fig. 2. A, B. Multituberculate teeth from the Wessex Formation of the Isle of Wight tentatively referred by Butler and Ford (1975) to Loxaulax sp. A. Left m2 (part of SMNS 51981) in occlusal (A1), mesiolabial (A2), and distolabial (A3) views (hatched areas represent broken surfaces) (see also Fig. 8B). B. Left I2 (part of SMNS 51981) in labial (B1), mesial (B2), and occlusal (B3) views (see also Fig. 10C). C. For comparison, right I2 from Cliff End provisionally referred by Clemens (1963) to Loxaulax valdensis Simpson, 1928 in labial (C1) and lingual (C2) views.

Fig. 8 in A new species of the plagiaulacoid multituberculate mammal Eobaatar from the Early Cretaceous of southern Britain

Fig. 8. Plagiaulacoid multituberculate Eobaatar clemensi sp. nov. from the Early Cretaceous Wessex Formation, Isle of Wight. A. Scanning electron micrograph of BMHH M 45482 in occlusal view. B. Normal light photograph of the m2 part of SMNS 51981 in occlusal view, to show its possible relationship to m1(s) BMNH M 45482 and 45557 (it was not possible to obtain scanning electron micrographs of the specimen which was glued to card by the original collector).

Fig. 6 in A new species of the plagiaulacoid multituberculate mammal Eobaatar from the Early Cretaceous of southern Britain

Fig. 6. Outline drawing of the holotype specimen, BMNH M 45482, to show disposition of cusps and pits, and cusp abbreviations used in the text.

Fig. 5. A in A new species of the plagiaulacoid multituberculate mammal Eobaatar from the Early Cretaceous of southern Britain

Fig. 5. A phylogenetic tree for the Plagiaulacida. After Hahn and Hahn (2004) with amendments and additions. Geological time scale from Gradstein et al. 2004. Temporal distribution of taxa from Kielan−Jaworowska et al. 2004. Abbreviations for Jurassic and Cretaceous stages: Al, Albian; Ap, Aptian; Ba, Barremian; Be, Berriasian; Ce, Cenomanian; Ha, Hauterivian; J1–J2, Middle and Lower Jurassic; Ki, Kimmeridgian; Ox, Oxfordian; Ti, Tithonian; Va, Valanginian.