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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.
Fig. 2 in An extended range of the multituberculate Kryptobaatar and distribution of mammals in the Upper Cretaceous of the Gobi Desert
Fig. 2. Comparison of teeth in Kryptobaatar dashzevegi. A. PM 120/108, Hermiin Tsav I, Gobi Desert, Mongolia; upper incisors (A1), right P1−P3 (A2), left P2, P3 (A3), left M1, M2 (A4). B. Right M2, ZPALMgM−I/52, Djadokhta Formation, Bayan Zag. C. Right M1 and M2, ZPALMgM−I/8, Djadokhta Formation, Bayan Zag. All SEM micrographs in occlusal view. M1 in A4 appears narrower than it originally was because of break of the middle cusps in outer row and outer margin.
Figure 4 in Deforestation affects biogeographical regionalization: a case study contrasting potential and extant distributions of Mexican terrestrial mammals
Figure 4. Map of Mexican provinces based on models of species' distributions in t1: baj, Baja California Chiapas; ist, Isthmus of Tehuantepec; mgu, Mexican Gulf; mpa, Mexican Pacific Coast; mpl, Mexican Sierra Madre Occidental; sms, Sierra Madre del Sur; son, Sonora; tam, Tamaulipas; vol, Transmexican
Figure 2 in Deforestation affects biogeographical regionalization: a case study contrasting potential and extant distributions of Mexican terrestrial mammals
Figure 2. Simplified consensus cladograms of (a) t1 (natural vegetation), and (b) t2 (land use and vegetation map based on the 2000 Inventario Forestal Nacional (SEMARNAT 2001).
Figure 1 in Deforestation affects biogeographical regionalization: a case study contrasting potential and extant distributions of Mexican terrestrial mammals
Figure 1. Ecological niche modelling projected as potential (based on the natural vegetation, t1) and extant (based on land use and natural vegetation, t2) distribution of two terrestrial mammals. Black areas depict part of distributions of (a) Chaetodipus spinatus in the Baja California Peninsula, and (b) Cabassous centralis in Chiapas.
Fig. 2 in Opportunistic Observations On The Distribution Of Cetaceans In The Malaysian South China, Sulu And Sulawesi Seas And An Updated Checklist Of Marine Mammals In Malaysia
Fig. 2. Map showing the locations of live sightings and strandings of various cetacean species in Peninsular Malaysia as listed in the updated checklist in Table 3. Each species' code on the map is according to the two-letter abbreviations listed in Table 3.
Fig. 1 in Opportunistic Observations On The Distribution Of Cetaceans In The Malaysian South China, Sulu And Sulawesi Seas And An Updated Checklist Of Marine Mammals In Malaysia
Fig. 1. Map showing the transect lines on which cetacean observations were conducted as well as the sightings of cetaceans that were encountered during the 2009 Prime Scientific Sailing Expedition.
Text-fig. 4. Distribution of arsinoitheres in Africa. Reconstruction of Arsinoitherium is adapted from Pomerol (1973) (the body in the image is probably too similar to that of an elephant, but the reconstruction gives an idea of the dimensions and possible body plan of Arsinoitherium). in Arsinoitherium (Embrithopoda) And Other Large Mammals And Plants From The Oligocene Of Tunisia
Text-fig. 4. Distribution of arsinoitheres in Africa. Reconstruction of Arsinoitherium is adapted from Pomerol (1973) (the body in the image is probably too similar to that of an elephant, but the reconstruction gives an idea of the dimensions and possible body plan of Arsinoitherium).
Text-fig. 6. Distribution of Oligocene continental sediments of Africa, revealing the patchy and incomplete coverage of the occurrences. The Tunisian sedimentary outcrops represent an important resource for the north-western part of the continent. in Arsinoitherium (Embrithopoda) And Other Large Mammals And Plants From The Oligocene Of Tunisia
Text-fig. 6. Distribution of Oligocene continental sediments of Africa, revealing the patchy and incomplete coverage of the occurrences. The Tunisian sedimentary outcrops represent an important resource for the north-western part of the continent.
Text-fig. 7. Temporal distribution of the described taxa from the Plio-Pleistocene localities of Turkey. The described localities are marked in red. in Plio-Pleistocene Amphibians And Reptiles From Central Turkey: New Faunas And Faunal Records With Comments On Their Biochronological Position Based On Small Mammals
Text-fig. 7. Temporal distribution of the described taxa from the Plio-Pleistocene localities of Turkey. The described localities are marked in red.
FIG. 1. — A in Mammal bearing late Miocene tuffs of the Akkaşdağı region; distribution, age, petrographical and geochemical characteristics
FIG. 1. — A, location map and major structural features of Turkey with location of Oligocene to Quarternary volcanism; B, map of the area SW of Çankırı-Çorum Basin (modified from Bilgin et al. 1986). Abbreviations: CAVP, Central Anatolian Volcanic Province; WAVP, West Anatolian Volcanic Province; EAVP, East Anatolian Volcanic Province; GVC, Galatia Volcanic Complex; NAFZ, North Anatolian Fault Zone; EAFZ, East Anatolian Fault Zone; BSZ, Bitlis Suture Zone; EFZ, Ecemis Fault Zone; KEF, Kırıkkale Erbaa Fault.
FIG. 3 in Mammal bearing late Miocene tuffs of the Akkaşdağı region; distribution, age, petrographical and geochemical characteristics
FIG. 3. — Representative photomicrographs of the studied tuffs; A, B, vitric tuff of upper level (cross-plane polarized light); C, D, vitric tuff of lower level (cross-plane polarized light); E, F, vitric tuffs consisting of an abundant glassy material, feldspar (Fl) and hornblend (Hb) (cross-plane polarized light); G, pumice clast (Pm) and oxyhornblend (Hn) (plane polarized light); H, rhyolitic lavas found at two levels in tuffs are completely calcified (cross polarized light). Abbreviations: Bi, biotite; Lt, lithic clast. Scales bars: A-D, G, H, 0.7 mm; E, F, 0.4 mm.
FIG. 5. — Integrated 39 in Mammal bearing late Miocene tuffs of the Akkaşdağı region; distribution, age, petrographical and geochemical characteristics
FIG. 5. — Integrated 39Ar/40Ar ages for two samples from the Akkaşdağı tuffs; A, sample AKK-1 from the main tuff horizon, three meters below the bone pocket AK-5; B, sample AKK-2 from the reworked tuffs filling the bone pocket AK-5.
FIG. 4. — A in Mammal bearing late Miocene tuffs of the Akkaşdağı region; distribution, age, petrographical and geochemical characteristics
FIG. 4. — A, total alkali vs. SiO2 diagram for the studied tuffs and Nevşehir Plateau ignimbrite. Classification scheme is from Le Bas et al. (1986), with the alkaline-subalkaline line by Miyashiro (1978); B, AFM diagram is from Irwine & Baragar (1971); C, Hacker variation diagrams for the studied tuffs and Nevşehir Plateau ignimbrite.
Text-fig. 21. Palaeogene fossil mammal localities of Africa and the Arabian Peninsula, highlighting the distribution of Omanitherium and other numidotheres and barytheres. in Large Mammals From The Rupelian Of Oman - Recent Finds
Text-fig. 21. Palaeogene fossil mammal localities of Africa and the Arabian Peninsula, highlighting the distribution of Omanitherium and other numidotheres and barytheres.
The role of climate and species interactions in determining the distribution of two elevationally segregated species of small mammals through time
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The distribution of plant consumption traits across habitat types and the patterns of fruit availability suggest a mechanism of coexistence of two sympatric frugivorous mammals
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Data from Uerpmann 1987, The Ancient Distribution of Ungulate Mammals in the Middle East, TAVO A27
<p>Data from Uerpmann’s (1987), <em><a href="https://reichert-verlag.de/en/author/u/uerpmann_hans_peter/9783882263954_the_ancient_distribution_of_ungulate_mammals_in_the_middle_east-detail">The Ancient Distribution of Ungulate Mammals in the Middle East</a></em>, volume 27 of the Tübinger Atlas des Vorderen Orients (TAVO), Series A.</p> <p>Uerpmann catalogued the occurrence of ungulate taxa in animal bone assemblages from 196 sites across the Middle East, from the Lower Palaeolithic to the historic period. Though no longer up-to-date, it remains one of the most comprehensive resources on quaternary biogeography in Southwest Asia. Here, the catalogue included in the volume has been transcribed into a structured format suitable for modern computerised data analysis.</p> <p>See README.md for further information and usage notes.</p>
Figure 3 in Deforestation affects biogeographical regionalization: a case study contrasting potential and extant distributions of Mexican terrestrial mammals
Figure 3. Mexican regionalization based on consensus cladogram of t1.
Data from: Distribution and protection of ecological specialists in Chinese terrestrial mammals
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OpenNeuro
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