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FIGURE 1 in Continental fishes of Nicaragua: diversity, distribution and conservation status; with an annotated and illustrated checklist of species and an identification guide to families
FIGURE 1. Map of Nicaragua, Central America, showing the division into 19 major river drainage basins: Coco (Co), Ulang (Ul), Wawa-Kukulaya (WK), Prinzapolka (Pr), Grande de Matagalpa (GM), Kurinwas-Laguna las Perlas (KP), Escondido (Es), Blue Fields-Punta Gorda (BF), Indio Maíz (IM), Tortuguero (To), Sarapiquí (Sa), San Juan (SJ), Río Frío (RF) and Lago de Nicaragua (LN) (Atlantic); Choluteca (Ch), Negro (Ne), Estero Real (ER), Pacífico de Nicaragua and Nicoya (Ni). Pacific drainages are shown in light blue. Data from the continental basins were obtained from HydroSHEDS (Lehner et al. 2008).
FIGURE 4 in Continental fishes of Nicaragua: diversity, distribution and conservation status; with an annotated and illustrated checklist of species and an identification guide to families
FIGURE 4. Families of continental fishes of Nicaragua, part 3; Achiridae (A), Carangidae (B), Cichlidae (C), Pomacentridae (D), Atherinopsidae (E), Rivulidae (F), Poeciliidae (G), Anablepidae (H), Belonidae (I), Hemiramphidae (J), Mugilidae (K), Gobiesocidae (L), Dactyloscopidae (M) and Lutjanidae (N). Illustrations adapted (with permission) from Nelson et al. (2016) and Angulo et al. (2021).
Subspecies and Distribution. S. s. scrofa Linnaeus, 1758 — W Europe, from Denmark, Germany, Poland, and Czech Republic to N Italy and N Iberian Peninsula; possibly also Albania. The taxonomic status of animals in Austria, Switzerland, Slovenia, and Slovakia is unclear but presumably these populations are included in scrofa, as are the populations of Sweden, Finland, and the Baltic states. However, restocking of once depleted populations, for example in Italy, has likely involved the introduction and mixing of this subspecies with other subspecies, such as attila. S. s. affinis Gray, 1847 — S India and Sri Lanka. S. s. algirus Loche, 1867 — Tunisia, Algeria, and Morocco, on the coastal side of the mountains or in the low montane areas. S. s. attila Thomas, 1912 — Hungary, Ukraine, C & S Belarus, Romania, Moldova, and S Russia towards the N flank of the Caucasus, but not including the Transcaucasian countries of Georgia, Armenia, and Azerbaijan. The range possibly extends as far S as the Mesopotamian Delta in Iraq, in which case it would likely include W & SW Iran, and possibly E Turkey and Syria, where it borders with lybicus. Such a range could not be easily reconciled with a statement by Groves that "the difference between pigs from N and S of the Caucasus is quite striking; Transcaucasian boars are certainly not attila." This subspecies may also extend into C Asia and include Kazakhstan, Uzbekistan, and Turkmenistan, but no data exist to support this. S. s. baeticus Thomas, 1912 — originally described from Coto Donana, S Spain, and later merged with meridionalis; also S Portugal. Unless evidence is found that these Italian and Iberian populations are the relics of a much larger formerly contiguous range, this subspecies should be kept as distinct. S. s. coreanus Heude, 1897 — Korean Peninsula. S. s. eristatus Wagner, 1839 — Himalayas S to C India and E to Indochina (N of the Kra Isthmus). S. s. davidi Groves, 1981 — the arid zone from E Iran to Gujarat, including Pakistan and NW India, and perhaps N to Tajikistan. S. s. leucomystax Temminck, 1842 — main Is ofJapan (Honshu, Shikoku, Kyushu, Nakadori, Hiburijima, Tojima, Kushima, and other smaller Is). S. s. lybicus Gray, 1868 — Bulgaria, Greece, Turkey, Syria, Jordan, Israel, Palestine, in the past also in Lybia, and Egypt. The former Yugoslavia was included in its range, which would suggest that now Slovenia, Serbia, Croatia, Bosnia and Herzegovina, Montenegro, and Kosovo are within the range of this subspecies, although the exact boundaries are unclear. Pigs from Albania have been assigned to S. s. scrofa. S. s. majori De Beaux & Festa, 1927 — C & S Italian Peninsula. S. s. menidionalis Forsyth Major, 1882 — Corsica and Sardinia, with the proviso that the two populations are very likely to be introduced or feral. S. s. moupinensis Milne-Edwards, 1871 — China, S to Vietnam and W to Sichuan. S. s. nigripes Blanford, 1875 — the flanks of the Tianshan mountains in Kyrgyzstan and NW China (Xinjiang). An animal photographed in NE Iran (Golestan) looked like this subspecies. S. s. nukiuanus Kuroda, 1924 — Iriomote, Ishigaki, Okinawa, Tokunoshima, Amamioshima, and Kakerome Is in the Ryukyu chain in extreme S Japan, though some of these populations have hybridized with introduced domesticates. S. s. sibiricus Staffe, 1922 — Mongolia and Transbaikal (S & E of Lake Baikal). S. s. tawvanus Swinhoe, 1863 — Taiwan. S. s. ussuricus Heude, 1888 — far E Russia and the Manchurian region (China). Korean populations were previously included in this subspecies, but based on new evidence, the Korean taxon seems more similar to moupinensis. S. s. vittatus Boie, 1828 — Malay Peninsula, S of the Isthmus of Kra, the offshore islands of Terutai and Langkawi, Sumatra, Riau Archipelago, Java, Bali, and a range of smaller islands around these, including Babi, Bakong, Batam, Bawean, Bengkalis, Bintan, Bulan, Bunguran, Cuyo, Deli, Durian, Enggano, Galang, Jambongan, Karimon (Riau Is), Kundur, Lagong, Laut, Lingga, Lingung, Mapor, Moro Kecil, North Pagai, Nias, Panaitan, Payong, Penang, Pinie, Rupat, Siantan, Siberut, Simeulue, Singkep, Sugi, Sugi Bawa, Telibon, Tinggi, Tuangku, and the Tambelan Is. This species was originally present from the British Is in the extreme W, through Eurasia from S Scandinavia to S Siberia, extending as far E as Korea and Japan, and SE into some of the Sunda Is and Taiwan. In the S the species ranged along the Nile Valley to Khartoum, and N of the Sahara in Africa, more orless following the continental coasts of S, E, and SE Asia. Within this range it was absent only from extremely dry deserts, e.g. the driest regions of Mongolia and in China W of Sichuan; and alpine zones, such as the high altitudes of Pamir and Tien Shan. In recent centuries, the range of S. scrofa has changed dramatically because of hunting and changes in available habitat. The species disappeared from the British Is in the 17" century, from Denmark in the 19" century, and was greatly reduced in range and numbers in the 20" century from areas as distant as Tunisia, Sudan, Germany, and Russia. Following these severe declines, there were some slight population recoveries in Russia, Italy, Spain, and Germany in the mid-20™ century, and natural and assisted range expansions in Denmark and Sweden. The species has also been inadvertently reintroduced in various locations in the Great Britain via escapees of mixed origin from commercial farming enterprises. Ex-S. scrofa stocks also occur as introduced feral populations in various other parts of the world, including Australia, New Zealand, the eastern Malay Archipelago, and in North, Central, and South America. In all of these areas they are now generally recognized as a major pest. in Suidae
Subspecies and Distribution. S. s. scrofa Linnaeus, 1758 — W Europe, from Denmark, Germany, Poland, and Czech Republic to N Italy and N Iberian Peninsula; possibly also Albania. The taxonomic status of animals in Austria, Switzerland, Slovenia, and Slovakia is unclear but presumably these populations are included in scrofa, as are the populations of Sweden, Finland, and the Baltic states. However, restocking of once depleted populations, for example in Italy, has likely involved the introduction and mixing of this subspecies with other subspecies, such as attila. S. s. affinis Gray, 1847 — S India and Sri Lanka. S. s. algirus Loche, 1867 — Tunisia, Algeria, and Morocco, on the coastal side of the mountains or in the low montane areas. S. s. attila Thomas, 1912 — Hungary, Ukraine, C & S Belarus, Romania, Moldova, and S Russia towards the N flank of the Caucasus, but not including the Transcaucasian countries of Georgia, Armenia, and Azerbaijan. The range possibly extends as far S as the Mesopotamian Delta in Iraq, in which case it would likely include W & SW Iran, and possibly E Turkey and Syria, where it borders with lybicus. Such a range could not be easily reconciled with a statement by Groves that "the difference between pigs from N and S of the Caucasus is quite striking; Transcaucasian boars are certainly not attila." This subspecies may also extend into C Asia and include Kazakhstan, Uzbekistan, and Turkmenistan, but no data exist to support this. S. s. baeticus Thomas, 1912 — originally described from Coto Donana, S Spain, and later merged with meridionalis; also S Portugal. Unless evidence is found that these Italian and Iberian populations are the relics of a much larger formerly contiguous range, this subspecies should be kept as distinct. S. s. coreanus Heude, 1897 — Korean Peninsula. S. s. eristatus Wagner, 1839 — Himalayas S to C India and E to Indochina (N of the Kra Isthmus). S. s. davidi Groves, 1981 — the arid zone from E Iran to Gujarat, including Pakistan and NW India, and perhaps N to Tajikistan. S. s. leucomystax Temminck, 1842 — main Is ofJapan (Honshu, Shikoku, Kyushu, Nakadori, Hiburijima, Tojima, Kushima, and other smaller Is). S. s. lybicus Gray, 1868 — Bulgaria, Greece, Turkey, Syria, Jordan, Israel, Palestine, in the past also in Lybia, and Egypt. The former Yugoslavia was included in its range, which would suggest that now Slovenia, Serbia, Croatia, Bosnia and Herzegovina, Montenegro, and Kosovo are within the range of this subspecies, although the exact boundaries are unclear. Pigs from Albania have been assigned to S. s. scrofa. S. s. majori De Beaux & Festa, 1927 — C & S Italian Peninsula. S. s. menidionalis Forsyth Major, 1882 — Corsica and Sardinia, with the proviso that the two populations are very likely to be introduced or feral. S. s. moupinensis Milne-Edwards, 1871 — China, S to Vietnam and W to Sichuan. S. s. nigripes Blanford, 1875 — the flanks of the Tianshan mountains in Kyrgyzstan and NW China (Xinjiang). An animal photographed in NE Iran (Golestan) looked like this subspecies. S. s. nukiuanus Kuroda, 1924 — Iriomote, Ishigaki, Okinawa, Tokunoshima, Amamioshima, and Kakerome Is in the Ryukyu chain in extreme S Japan, though some of these populations have hybridized with introduced domesticates. S. s. sibiricus Staffe, 1922 — Mongolia and Transbaikal (S & E of Lake Baikal). S. s. tawvanus Swinhoe, 1863 — Taiwan. S. s. ussuricus Heude, 1888 — far E Russia and the Manchurian region (China). Korean populations were previously included in this subspecies, but based on new evidence, the Korean taxon seems more similar to moupinensis. S. s. vittatus Boie, 1828 — Malay Peninsula, S of the Isthmus of Kra, the offshore islands of Terutai and Langkawi, Sumatra, Riau Archipelago, Java, Bali, and a range of smaller islands around these, including Babi, Bakong, Batam, Bawean, Bengkalis, Bintan, Bulan, Bunguran, Cuyo, Deli, Durian, Enggano, Galang, Jambongan, Karimon (Riau Is), Kundur, Lagong, Laut, Lingga, Lingung, Mapor, Moro Kecil, North Pagai, Nias, Panaitan, Payong, Penang, Pinie, Rupat, Siantan, Siberut, Simeulue, Singkep, Sugi, Sugi Bawa, Telibon, Tinggi, Tuangku, and the Tambelan Is. This species was originally present from the British Is in the extreme W, through Eurasia from S Scandinavia to S Siberia, extending as far E as Korea and Japan, and SE into some of the Sunda Is and Taiwan. In the S the species ranged along the Nile Valley to Khartoum, and N of the Sahara in Africa, more orless following the continental coasts of S, E, and SE Asia. Within this range it was absent only from extremely dry deserts, e.g. the driest regions of Mongolia and in China W of Sichuan; and alpine zones, such as the high altitudes of Pamir and Tien Shan. In recent centuries, the range of S. scrofa has changed dramatically because of hunting and changes in available habitat. The species disappeared from the British Is in the 17" century, from Denmark in the 19" century, and was greatly reduced in range and numbers in the 20" century from areas as distant as Tunisia, Sudan, Germany, and Russia. Following these severe declines, there were some slight population recoveries in Russia, Italy, Spain, and Germany in the mid-20™ century, and natural and assisted range expansions in Denmark and Sweden. The species has also been inadvertently reintroduced in various locations in the Great Britain via escapees of mixed origin from commercial farming enterprises. Ex-S. scrofa stocks also occur as introduced feral populations in various other parts of the world, including Australia, New Zealand, the eastern Malay Archipelago, and in North, Central, and South America. In all of these areas they are now generally recognized as a major pest.
Subspecies and Distribution. P.m. marmorata Martin, 1837 — Continental SE Asia, from SW China to Malaysia, and islands of Sumatra and Borneo. P.m. charltoni Gray, 1846 — Sub-Himalayan region, from Nepal to Mynamar. in Felidae
Subspecies and Distribution. P.m. marmorata Martin, 1837 — Continental SE Asia, from SW China to Malaysia, and islands of Sumatra and Borneo. P.m. charltoni Gray, 1846 — Sub-Himalayan region, from Nepal to Mynamar.
Distribution. Coastal areas and large inland rivers of West Africa from the Senegal River at the Mauritania—Senegal border S to the Longa River in Angola. They occur as far as 2000 km from the ocean in the Inner Niger Delta of Mali, up to 75 km off the continental shore in the shallows and mangrove creeks of the Bijagos Archipelago of Guinea-Bissau, and as far E as Lake Tréné in Chad; formerly in Lake Chad itself. in Trichechidae
Distribution. Coastal areas and large inland rivers of West Africa from the Senegal River at the Mauritania—Senegal border S to the Longa River in Angola. They occur as far as 2000 km from the ocean in the Inner Niger Delta of Mali, up to 75 km off the continental shore in the shallows and mangrove creeks of the Bijagos Archipelago of Guinea-Bissau, and as far E as Lake Tréné in Chad; formerly in Lake Chad itself.
Subspecies and Distribution. L.t.townsenditBachman,1839—WoftheContinentalDivideinSWCanada(SBritishColumbia)andWUSA(fromNCWashingtontoWWyoming,NWColorado,Utah,NENevada,andECCalifornia). L. t. campanius Hollister, 1915 — E of the Continental Divide in SC Canada (from S Alberta to extreme SW Ontario) and NC USA (from W Montana to E Wisconsin and S to NC New Mexico, N Nebraska, and NW Missouri). in Leporidae
Subspecies and Distribution. L.t.townsenditBachman,1839—WoftheContinentalDivideinSWCanada(SBritishColumbia)andWUSA(fromNCWashingtontoWWyoming,NWColorado,Utah,NENevada,andECCalifornia). L. t. campanius Hollister, 1915 — E of the Continental Divide in SC Canada (from S Alberta to extreme SW Ontario) and NC USA (from W Montana to E Wisconsin and S to NC New Mexico, N Nebraska, and NW Missouri).
Distribution. Panama (W to Chiriqui, and including Isla del Rey and Isla Saboga in the Gulf of Panama), N & W Colombia, N Venezuela (N of the Orinoco River), and on several islands on the continental shelf of South America and the Caribbean (Margarita, Trinidad, Tobago, and Grenada). in Didelphidae
Distribution. Panama (W to Chiriqui, and including Isla del Rey and Isla Saboga in the Gulf of Panama), N & W Colombia, N Venezuela (N of the Orinoco River), and on several islands on the continental shelf of South America and the Caribbean (Margarita, Trinidad, Tobago, and Grenada).
Distribution. Islands off peninsular Thailand (Koh Samui) and Peninsular Malaysia (Tioman, and Mapur); one old specimen from Mt Tahan, Pahang State, Malaysia, might also belong to this species, but no recent confirmation of this taxon on the Malay Peninsula cast doubts about the existence of such a continental population of Peninsular White-toothed Shrew. in Soricidae
Distribution. Islands off peninsular Thailand (Koh Samui) and Peninsular Malaysia (Tioman, and Mapur); one old specimen from Mt Tahan, Pahang State, Malaysia, might also belong to this species, but no recent confirmation of this taxon on the Malay Peninsula cast doubts about the existence of such a continental population of Peninsular White-toothed Shrew.
Fig. 13 in Distribution and diversity of the Opheliidae (Annelida, Polychaeta) on the continental shelf and slope of Iceland, with a review of the genus Ophelina in northeast Atlantic waters and description of two new species
Fig. 13 Ophelina bowitzi sp. nov. (IMNH 24324, BIOICE sample 2863). a Anterior end, lateral view. b Detail of nuchal organ. c Chaetiger 11. d Chaetiger 18. e Chaetiger 25; arrows mark positions of two ciliary bands. (f) Chaetiger 28; arrow marks position of lateral organ. Scale bars: (a) 1 mm; (b) 90 μm; (c, d, f) 100 μm; (e) 900 μm
Fig. 10 in Distribution and diversity of the Opheliidae (Annelida, Polychaeta) on the continental shelf and slope of Iceland, with a review of the genus Ophelina in northeast Atlantic waters and description of two new species
Fig. 10 Posterior body region in three North Atlantic-Arctic species of Ophelina not found in BIOICE samples. a O. groenlandica Støp-Bowitz, 1948 (holotype, SMNH T-7831). b O. norvegica Støp-Bowitz, 1945 (SMNH 11137). c O. nybelini Eliason, 1951 (syntype, GNHM Polych. 10999). Scale bars: (a) 0.5 mm; (b, c) 1 mm
Fig. 11 in Distribution and diversity of the Opheliidae (Annelida, Polychaeta) on the continental shelf and slope of Iceland, with a review of the genus Ophelina in northeast Atlantic waters and description of two new species
Fig. 11 Ophelina helgolandica Augener (IMNH 24329, BIO- ICE sample 2579). a Anterior end, lateral view. b Detail of nuchal organ. c First chaetiger. d Chaetigers 2–3. e Last branchiate chaetiger; arrow marks position of lateral organ. f Posterior body region, lateral view; arrow marks position of last branchiate chaetiger followed by three abranchiate chaetigers. Scale bars: (a, f) 1 mm; (b, c, e), 100 μm; (d) 200 μm
Fig. 9 in Distribution and diversity of the Opheliidae (Annelida, Polychaeta) on the continental shelf and slope of Iceland, with a review of the genus Ophelina in northeast Atlantic waters and description of two new species
Fig. 9 Posterior body region in some Atlantic Ophelina species (redrawn from originals). a O. abranchiata (from Støp-Bowitz 1948). b O. bowitzi sp. nov. (from Fauvel 1914, as A. arctica). c O. delapidans longicephala (from HartmannSchröder 1977). d O. groenlandica (from Støp-Bowitz 1948). e O. helgolandica (from Augener 1912). f O. norvegica (from Støp-Bowitz 1945). g O. nybelini (from Eliason 1951)
Fig. 8 in Distribution and diversity of the Opheliidae (Annelida, Polychaeta) on the continental shelf and slope of Iceland, with a review of the genus Ophelina in northeast Atlantic waters and description of two new species
Fig. 8 Ophelina basicirra sp. nov. (Paratypes, IMNH 24318, BIOICE sample 2303). a, b Posterior end with anal tube, lateral views. c, d Cirri of anal tube. e Anal tube, ventral view. f Detail of anal cirrus of anal tube. Scale bars: (a, b) 300 μm; (c) 90 μm; (d) 50 μm; (e) 200 μm; (f) 60 μm
Fig. 1 in Distribution and diversity of the Opheliidae (Annelida, Polychaeta) on the continental shelf and slope of Iceland, with a review of the genus Ophelina in northeast Atlantic waters and description of two new species
Fig. 1 Maps of the study area and collecting sites of samples including specimens of Opheliidae. a All samples combined. b Ammotrypanella cf. arctica McIntosh. c Ophelina basicirra sp. nov. d Ophelina bowitzi sp. nov
Figure 3 in Craniid brachiopods: aspects of clade structure and distribution reflect continental drift (Brachiopoda: Craniiformea)
Figure 3. Craniid phylogeny. PAUP* maximum likelihood tree constructed from nuclear LSU rDNA sequences using the best-fitting evolutionary model and showing jackknife clade support (%). In this tree (contrast with Figure 2) the NE Pacific clade is allied to the Tethyan and Northern clades.
Figure 4 in Craniid brachiopods: aspects of clade structure and distribution reflect continental drift (Brachiopoda: Craniiformea)
Figure 4. Craniid phylogeny. Relative age, Bayesian log-likelihood, relaxed-clock time-tree from BEAST, root age defined as 1.0, with inferred relative time-depths of other nodes as shown, or as noted in the Discussion. Confidence intervals (95% highest posterior density) are shown as bars across nodes. Based on SSU+LSU sequences of craniid ingroup and brachiopod and phoronid outgroups.
Rainfall continentality, via the winter GAMS angle, provides a new dimension to biogeographical distributions in the Western United States
<p><b>Aim:</b> Drought stress, and its effects on the biogeography of vegetation, has focused primarily on water availability during the growing season, thus focusing primarly on summer. However, variation in rainfall continentality (i.e., the continental interior being insulated from oceanic influences) can produce striking vegetation differences. We aim to disentangle summer water balance from the influence of rainfall continentality on winter rainfall, to better understand how climate regulated the distributions of woody plants in the Western USA.</p> <p><b>Location: </b>Western USA.</p> <p><b>Time period:</b> Actual.</p> <p><b>Major taxa studied: </b>Angiosperms and Conifers.</p> <p><b>Method: </b>We used Redundancy Analysis (RDA) to investigate correlations between rainfall continentality, summer water balance, minimum winter temperature and length of growing season on the distributions of 130 tree and shrub species in 467 plots. Rainfall continentality was calculated using the Gams (1932) index, modified for winter precipitation, and summer water balance with the ratio of summer precipitation to temperature. We estimated Actual EvapoTranspiration (AET), Deficit (DEF), mean annual temperature and rainfall from global gridded datasets and correlated them with RDA axes.</p> <p><b>Results: </b>Rainfall continentality measured with the Gams index and minimum temperatures best explained the contrast between oceanic vegetation in the Pacific Coast Ranges and continental vegetation in the Intermountain Region and Rocky Mountains. Growing Season Length (GSL) was the second strongest factor correlated with vegetation distributions. Summer water balance, despite being the most widely used climatic factor to assess drought stress in biogeography, was the third strongest factor correlating with vegetation classes of the western US. AET was equally correlated with RDA axes 1 and 3, and, thus, could not discriminate between the contrasts in the RDA.</p> <p><b>Main conclusions:</b> Rainfall continentality measured with the winter Gams index provides a more precise metric than summer water balance for understanding how the biogeography of woody plants in the western USA is regulated by climate. Broadly integrating the Gams index of continentality into plant distributions may improve our understanding of biogeographical distributions, the evolution of subspecies in species that span coastal to interior regions, and predictions of responses to climate change.</p>
Data from: Disentangling the genetic effects of refugial isolation and range expansion in a trans-continentally distributed species
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Rainfall continentality, via the winter GAMS angle, provides a new dimension to biogeographical distributions in the Western United States
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Data from: From ratites to rats: the size of fleshy fruits shapes species' distributions and continental rainforest assembly
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Allen Brain Atlas
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