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Text-fig. 4. Graphical visualization of Phytogeographic Reference Regions Assessment (PRRA) of nearest living relative genera of fossil-taxa from late Early Miocene Wiesa assemblage in eastern Germany. Analysis yields only NLRs which have modern distribution area (partly) in E and SE Asia. For relationships of fossil-taxa to nearest living relatives or ecological equivalents, see Tab. 6; taxa used for analysis marked with asterisks. Three geographic resolutions conducted: a – grid with 1.5° latitude/longitude resolution, b – grid with 2°, c – grid with 3°; similarity column indicates cooccurrences of genera of nearest living relatives in single grid box. Maximum value in our analysis: grid box marked with arrow in map a, located in western Yunnan Province, P. R. China and southern Kachin Province, NE Myanmar (east of Myitkyina city), area with 97.371 7–98.874 2° longitude and 24.586 7–25.837 5° latitude, yields 23 co-occurring species of 13 genera (Tab. 7). in Assessment Of Phytogeographic Reference Regions For Cenozoic Vegetation: A Case Study On The Miocene Flora Of Wiesa (Germany)

Text-fig. 4. Graphical visualization of Phytogeographic Reference Regions Assessment (PRRA) of nearest living relative genera of fossil-taxa from late Early Miocene Wiesa assemblage in eastern Germany. Analysis yields only NLRs which have modern distribution area (partly) in E and SE Asia. For relationships of fossil-taxa to nearest living relatives or ecological equivalents, see Tab. 6; taxa used for analysis marked with asterisks. Three geographic resolutions conducted: a – grid with 1.5° latitude/longitude resolution, b – grid with 2°, c – grid with 3°; similarity column indicates cooccurrences of genera of nearest living relatives in single grid box. Maximum value in our analysis: grid box marked with arrow in map a, located in western Yunnan Province, P. R. China and southern Kachin Province, NE Myanmar (east of Myitkyina city), area with 97.371 7–98.874 2° longitude and 24.586 7–25.837 5° latitude, yields 23 co-occurring species of 13 genera (Tab. 7).

opencc-by-4.0Dec 2019View details →

Рис. 2. Распредение биомассы Mytilus trossulus septentrionalis на литорали дальневоcточных морей России. Здесь и далее на гистограммах по оси абцисс после географических пунктов в скобках укаЗана выборка (число иЗученных проб), по оси ординат – максимальные ЗначениЯ биомассы вида. Под Значением биомассы 0.1 г/м² подраЗумеваютсЯ качественные пробы. СокраЩениЯ (бмп) и (топ) оЗначают соответственно беринговоморское и тихоокеанское побережьЯ Восточной Камчатки. Побережье Зал. Петра Великого от устьЯ р. Туманной к северу до м. Поворотного условно отноcитсЯ к южному Приморью; побережье к северу от м. Поворотного (пос. Преображение, б. СоколовскаЯ) до б. Ольга, включительно, условно относитсЯ к среднему Приморью; побережье к северу от б. Ольга до м. Белкина и материковое побережье Татарского пролива относим к северному Приморью. Fig. 2. The distribution of biomass of Mytilus trossulus septentrionalis in the intertidal zone of the Far Eastern seas of Russia. Here and throughout on histograms, on the abcissa is the number of studied samples (numbers in parentheses following the names geographic localities), on the ordinate is the maximum biomass of species. The number 0.1 g wet wt m-2 means the qualitative samples. Abbreviations (bmp) and (top) mean the Bering Sea coast and the Pacific coast of eastern Kamchatka. The coast of Peter the Great Bay from the mouth of the Tumannaya River to Cape Povorotny is conditionally referred to as southern Primorye; the area north of Cape Povorotny (Preobrazhenie Settlement, Sokolovskaya Bay) to Olga Bay inclusive is conditionally referred to as middle Primorye; north of Olga Bay to Cape Belkin and the mainland coast of the Tatar Strait to as northern Primorye. in Bivalve mollusks of the intertidal zone of the Far Eastern seas of Russia

Рис. 2. Распредение биомассы Mytilus trossulus septentrionalis на литорали дальневоcточных морей России. Здесь и далее на гистограммах по оси абцисс после географических пунктов в скобках укаЗана выборка (число иЗученных проб), по оси ординат – максимальные ЗначениЯ биомассы вида. Под Значением биомассы 0.1 г/м² подраЗумеваютсЯ качественные пробы. СокраЩениЯ (бмп) и (топ) оЗначают соответственно беринговоморское и тихоокеанское побережьЯ Восточной Камчатки. Побережье Зал. Петра Великого от устьЯ р. Туманной к северу до м. Поворотного условно отноcитсЯ к южному Приморью; побережье к северу от м. Поворотного (пос. Преображение, б. СоколовскаЯ) до б. Ольга, включительно, условно относитсЯ к среднему Приморью; побережье к северу от б. Ольга до м. Белкина и материковое побережье Татарского пролива относим к северному Приморью. Fig. 2. The distribution of biomass of Mytilus trossulus septentrionalis in the intertidal zone of the Far Eastern seas of Russia. Here and throughout on histograms, on the abcissa is the number of studied samples (numbers in parentheses following the names geographic localities), on the ordinate is the maximum biomass of species. The number 0.1 g wet wt m-2 means the qualitative samples. Abbreviations (bmp) and (top) mean the Bering Sea coast and the Pacific coast of eastern Kamchatka. The coast of Peter the Great Bay from the mouth of the Tumannaya River to Cape Povorotny is conditionally referred to as southern Primorye; the area north of Cape Povorotny (Preobrazhenie Settlement, Sokolovskaya Bay) to Olga Bay inclusive is conditionally referred to as middle Primorye; north of Olga Bay to Cape Belkin and the mainland coast of the Tatar Strait to as northern Primorye.

opencc-by-4.0Aug 2016View details →

Geographical distribution of the Mediterranean mussel Mytilus galloprovincialis Lamarck, 1819 in the Sea of Japan. in The extension of the distributional range of an invasive mussel, Mytilus galloprovincialis (Bivalvia: Mytilidae) in the Sea of Japan

Geographical distribution of the Mediterranean mussel Mytilus galloprovincialis Lamarck, 1819 in the Sea of Japan.

Fig. 10 in Morphological variations and geographic distribution of the rare Middle Jurassic ammonite Oecoptychius refractus

Fig. 10. Comparative dimensional proportions of various species of Oecoptychius Neumayr, 1878. Shaded areas display the range of variation in dimensional proportions.

Fig. 8 in Morphological variations and geographic distribution of the rare Middle Jurassic ammonite Oecoptychius refractus

Fig. 8. Strigoceratid ammonoid Oecoptychius refractus (Reinecke, 1818) m], SMNS 63457/1, from Ornatenton Formation, Kosmoceras jason Zone, Neidlingen, SW Germany, middle Callovian, Middle Jurassic. Note the strigations, a character noted only in well-preserved specimens and reminiscent of species attributed to Phlycticeras polygonium (Zieten, 1831) var. waageni [M] and considered herein to represent macroconch of O. refractus Reinecke, 1818).

Fig. 6 in Morphological variations and geographic distribution of the rare Middle Jurassic ammonite Oecoptychius refractus

Fig. 6. Strigoceratid ammonoid Oecoptychius refractus (Reinecke, 1818) [m] from Ogrodzieniec quarry, Quenstedtoceras lamberti Zone, upper Callovian. A. GIUS 8-3657/12 in lateral (A1), dorsal (A2), and dorsal (A3, note the ribbing pattern) views. B. GIUS 8-3657/5 in lateral (B1) and ventral (B2, B3, note the ribbing pattern) views. C. GIUS 8-3657/3 11 in lateral (C1), opposite lateral (C2), and ventral (C3) views. D. GIUS 8-3657/4 in lateral (D1), opposite lateral (D2), and ventral (D3, D4, note the ribbing pattern) views.

Fig. 5 in Morphological variations and geographic distribution of the rare Middle Jurassic ammonite Oecoptychius refractus

Fig. 5. Strigoceratid ammonoid Oecoptychius refractus (Reinecke, 1818) [m] from Ogrodzieniec quarry, Quenstedtoceras lamberti Zone, upper Callovian. A. GIUS 8-3657/9 in lateral (A1), dorsal (A2), ventral (A3), and dorsal (A4, note the ribbing pattern) views. B. GIUS 8-3657/10 in ventral view. C. GIUS 8-3657/11 in lateral (C1), opposite lateral (C2), ventral (C3), and dorsal (C4) views. D. GIUS 8-3657/2 in lateral (D1), opposite lateral (D2), ventral (D3), and dorsal (D4) views.

Fig. 4 in Morphological variations and geographic distribution of the rare Middle Jurassic ammonite Oecoptychius refractus

Fig. 4. Strigoceratid ammonoid Oecoptychius refractus (Reinecke, 1818) [m] from Ogrodzieniec quarry, Quenstedtoceras lamberti Zone, upper Callovian. A. GIUS 8-3657/1 in lateral (A1), opposite lateral (A2), ventral (A3), and dorsal (A4) views. B. GIUS 8-3657/6 in lateral (B1) and ventral (B2) views. C. GIUS 8-3657/7 in lateral view (C1), detail showing the smooth umbilical region (C2), opposite lateral (C3) and dorsal (C4) views. D. GIUS 8-3657/8 in lateral (D1), opposite lateral (D2), ventral (D3), and dorsal (D4) views.

Fig. 2 in Morphological variations and geographic distribution of the rare Middle Jurassic ammonite Oecoptychius refractus

Fig. 2. Lithostratigraphy and biostratigraphy at the Ogrodzieniec quarry (modified after Dembicz et al. 2006). Arrow shows the occurrence of Oecoptychius refractus (Reinecke, 1818) within the general stratigraphy of the Ogrodzieniec quarry. Bed numbers (1, 1a, 2, 3, 18, and 37) after Dembicz et al. (2006).

Fig. 9 in Morphological variations and geographic distribution of the rare Middle Jurassic ammonite Oecoptychius refractus

Fig. 9. Dimensional proportions of Oecoptychius refractus (Reinecke, 1818) [m]. The French and Polish specimens are compared with a reference point of the lectotype. A. Whorl height vs. shell diameter. B. Whorl thickness vs. shell diameter. C. Umbilicus vs. shell diameter. D. Whorl thickness vs. coiling ratio. For all given dimensional proportions, the French and Polish specimens form different groups.

Fig. 1. Geological map and the abandoned Ogrodzieniec quarry. A in Morphological variations and geographic distribution of the rare Middle Jurassic ammonite Oecoptychius refractus

Fig. 1. Geological map and the abandoned Ogrodzieniec quarry. A. Map showing the studied localities in Poland, western France, and Kachchh (western India). B. Map of France showing the position of St.-Laon and Montreuil-Bellay. C. Map of India showing the position of Kachchh. D. Map of Poland showing the the position of Ogrodzieniec. E. Detailed location of Ogrodzieniec quarry (modified after Jain and Mazur 2021). F. Geological map of the Polish Jura Chain showing the location of the studied Ogrodzieniec quarry. G. Aerial view of the Ogrodzieniec quarry; arrow marks the location of the studied section. H. Exposure of the studied section.

Fig. 3 in Morphological variations and geographic distribution of the rare Middle Jurassic ammonite Oecoptychius refractus

Fig. 3. Biostratigraphy of the studied section. A. Geological column, correlation of studied beds with these of Głowniak (2012) and the occurrence of specimens noted in the present study (modified after Jain and Salamon 2023). B. Field photo of the condensed bed where the studied specimens of Oecoptychius refractus (Reinecke, 1818) [m] were recorded. C. Close-up of the block with Quenstedtoceras lamberti (Q) and Hibolithes hastatus (H).

opencc-by-4.0Dec 2003View details →

Figure 1 in Geographic and depth distributional patterns of western Atlantic Porcellanidae (Crustacea: Decapoda: Anomura), with an updated list of species

Figure 1. Comparison of the tropical porcellanid faunas from different regions of the western Atlantic. Large, simple circles indicate total number of species in Florida and Brazil regions; small, simple circles indicate species shared by regions; double circle indicates species in Caribbean-West Indian region; rectangle indicates species in southern Caribbean; oval indicates species in the Antilles.

Figs 91–94 in Geographic Distribution Of Lispocephala Pokorny (Diptera: Muscidae), With Descriptions Of New Species From China

Figs 91–94. Lispocephala setilobata sp. n.: 91 = cerci, posterior view (scale bar: 0.2 mm); 92 = sternite 5, profile view (scale bar: 0.2 mm); 93 = phallosome (scale bar: 0.2 mm); 94 = terminalia,

Figs 87–90 in Geographic Distribution Of Lispocephala Pokorny (Diptera: Muscidae), With Descriptions Of New Species From China

Figs 87–90. Lispocephala setilobata sp. n.: 87 = male abdomen, dorsal view (scale bar: 1 mm); 88 = male abdomen, profile view (scale bar: 1 mm); 89 = sternite 5 (scale bar: 0.2 mm); 90 = paramere

Figs 83–86 in Geographic Distribution Of Lispocephala Pokorny (Diptera: Muscidae), With Descriptions Of New Species From China

Figs 83–86. Lispocephala leschenaulti sp. n. terminalia in profile (after HENNIG 1961): 83 = distiphallus, posterior view (scale bar: 0.2 mm), 84 = distiphallus, ventral view (scale bar: 0.2 mm), 85 = terminalia, profile view (scale bar: 0.2 mm). 86 = L. spuria (ZETTERSTEDT, 1838) terminalia in pro-

Figs 78–82 in Geographic Distribution Of Lispocephala Pokorny (Diptera: Muscidae), With Descriptions Of New Species From China

Figs 78–82. Lispocephala leschenaulti sp. n.: 78 = male abdomen, dorsal view (scale bar: 1 mm); 79 = cerci, posterior view (scale bar: 0.2 mm); 80 = sternite 5 (scale bar: 0.2 mm); 81 = paramere (scale bar:

Figs 71–75 in Geographic Distribution Of Lispocephala Pokorny (Diptera: Muscidae), With Descriptions Of New Species From China

Figs 71–75. Lispocephala nigriala sp. n.: 71 = male abdomen, dorsal view (scale bar: 0.5 mm); 72 = paramere (scale bar: 0.1 mm); 73 = cerci, posterior view (scale bar: 0.2 mm); 74 = sternite 5, profile

Figs 59–64 in Geographic Distribution Of Lispocephala Pokorny (Diptera: Muscidae), With Descriptions Of New Species From China

Figs 59–64. Lispocephala subcurvilobata sp. n.: 59 = phallosome (scale bar: 0.2 mm); 60 = sternite 5 (scale bar: 0.2 mm); 61 = cerci, posterior view (scale bar: 0.2 mm); 62 = lobe of sternite 5, profile view

Figs 53–58 in Geographic Distribution Of Lispocephala Pokorny (Diptera: Muscidae), With Descriptions Of New Species From China

Figs 53–58. Lispocephala curvilobata sp. n.: 53 = terminalia, profile view (scale bar: 0.2 mm); 54 = cerci, posterior view (scale bar: 0.2 mm); 55 = paramere (scale bar: 0.1 mm); 56 = lobe of sternite 5, profile view (scale bar: 0.2 mm); 57 = phallosome (scale bar: 0.2 mm); 58 = sternite 5 (scale bar: 0.2 mm)