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Fig. 3 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 3. The lithological succession of the Hangenberg Limestone in the Oberrödinghausen railway cutting section with the occurrence of the ammonoid species of the family Prionoceratidae Hyatt, 1884 and the ammonoid zonation.
Fig. 27 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 27. Kornia acia sp. nov. from the Oberrödinghausen railway cutting; holotype MB.C.31073.1 (Weyer 1993–1994 Coll.) from bed 5a2. Scale bar units = 1 mm.
Fig. 30 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 30. Stockumites kleinerae (Korn, 1984) from the Oberrödinghausen railway cutting. A. Cross section of specimen GPIT-PV-63879 from bed 5. B. Cross section of specimen MB.C.31075.1 from bed 5. C. Suture line of specimen GPIT-PV-64016 from bed 5, at ww = 10.5 mm. D. Growth line course of specimen GPIT-PV-64004 from bed 6, at dm = 23.0 mm, ww = 19.4 mm, wh = 12.8 mm.E –G. Ontogenetic development of the conch width index (ww/dm), umbilical width index (uw/dm), whorl width index (ww/wh) and whorl expansion rate (WER) of selected specimens. Scale bar units = 1 mm.
Fig. 42 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 42. Stockumites voehringeri sp. nov. from the Oberrödinghausen railway cutting; all Vöhringer Coll. A. Holotype GPIT-PV-63995 from unknown bed. B. Paratype GPIT-PV-63885 from bed 3b. C. Paratype GPIT-PV-64005 from bed 2. D. Paratype GPIT-PV-63850 from bed 3e. Scale bar units = 1 mm.
Fig. 35 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 35. Stockumites parallelus sp. nov. from the Oberrödinghausen railway cutting and the Oese section. A. Paratype MB.C.31087 (Weyer 1993–1994 Coll.) from bed 6b of Oberrödinghausen; dorsal reconstruction and lateral view. B. Cross section of paratype GPIT-PV-63890 from bed 5 of Oberrödinghausen. C. Cross section of paratype SMF 43081 (Korn 1982 Coll.) from the Stockum Limestone at Stockum (from Korn 1984). D. Cross section of paratype MB.C.5292 from the lower part of the Hangenberg Limestone at Oese (from Korn & Weyer 2003). E–G. Ontogenetic development of the conch width index (ww/dm), umbilical width index (uw/dm), whorl width index (ww/wh) and whorl expansion rate (WER) of selected specimens (grey = specimens from the type locality Stockum). Scale bar units = 1 mm.
Fig. 22. Paragattendorfia sphaeroides Weyer, 1972 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 22. Paragattendorfia sphaeroides Weyer, 1972, from the Oberrödinghausen railway cutting, (Vöhringer Coll.), holotype GPIT-PV-63909 from bed 3c. Scale bar units = 1 mm.
Fig. 14 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 14. Mimimitoceras perditum sp. nov. from the Oberrödinghausen railway cutting, all Vöhringer Coll. A. Cross section of paratype MB.C.31054.1 from an unknown bed. B. Cross section of paratype MB.C.31052.1 from bed 2. C. Cross section of paratype MB.C.31052.2 from bed 2. D. Cross section of paratype MB.C.31054.2 from an unknown bed. E. Cross section of paratype MB.C.31052.3 from bed 2. F. Suture line of paratype GPIT-PV-64013 from bed 1, at dm = 25.0 mm, ww = 16.5 mm, wh = 13.0 mm. G. Growth line course of paratype GPIT-PV-63862 from bed 5, at ww = 26.0 mm, wh = 25.5 mm. H–J. Ontogenetic development of the conch width index (ww/dm), umbilical width index (uw/dm), whorl width index (ww/wh) and whorl expansion rate (WER) of selected specimens. Scale bar units = 1 mm.
Fig. 17. Mimimitoceras hoennense Korn, 1994 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 17. Mimimitoceras hoennense Korn, 1994 from the Oberrödinghausen railway cutting, all Vöhringer Coll. A. Cross section of paratype GPIT-PV-63867 from bed 3d. B. Suture line of paratype GPIT-PV-63866 from bed 4, at ww = 13.5 mm, wh = 12.0 mm. C. Growth line course of specimen GPIT- PV-63884 from bed 5, at dm = 28.5 mm, ww ~ 15.0 mm, wh = 14.6 mm. D–F. Ontogenetic development of the conch width index (ww/dm), umbilical width index (uw/dm), whorl width index (ww/wh) and whorl expansion rate (WER) of selected specimens. Scale bar units= 1 mm.
Fig. 29 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 29. Stockumites kleinerae (Korn, 1984) from the Oberrödinghausen railway cutting, both Vöhringer Coll. A. Specimen GPIT-PV-63880 from bed 5. B. Specimen GPIT-PV-64004 from bed 6. Scale bar units = 1 mm.
Fig. 16. Mimimitoceras hoennense Korn, 1993 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 16. Mimimitoceras hoennense Korn, 1993 from the Oberrödinghausen railway cutting, both Vöhringer Coll. A. Holotype GPIT-PV-63884 from bed 2. B. Paratype GPIT-PV-63866 from bed 2. Scale bar units = 1 mm.
Fig. 34 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 34. Stockumites intermedius (Schindewolf, 1923) from bed 5 of the Oberrödinghausen railway cutting. A. Cross section of specimen MB.C.31078.3 (Vöhringer Coll.). B. Cross section of specimen MB.C.31080.1 (Weyer 1993–1994 Coll.) from bed 5a2. C. Cross section of specimen GPIT-PV-64000 (Vöhringer Coll.). D. Cross section of specimen MB.C.31078.4 (Vöhringer Coll.) from bed 5. E. Cross section of specimen GPIT-PV-63860 (Vöhringer Coll.). Scale bar units = 1 mm.
Fig. 20 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 20. Paragattendorfia patens (Vöhringer, 1960) from the Oberrödinghausen railway cutting. A. Holotype GPIT-PV-63912 (Vöhringer Coll.) from bed 2. B. Paratype GPIT-PV-63914 (Vöhringer Coll.) from bed 2. C. Specimen MB.C.31067 (Weyer 1993–1994 Coll.) from bed 3d2. Scale bar units = 1 mm.
Fig. 1 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 1. The geographic position of the Oberrödinghausen railway cutting section and other Devonian–Carboniferous boundary sections at the northern margin of the Rhenish Mountains east of the Rhine. Abbreviations: APR = Apricke; DRE = Drewer; EFF = Effenberg; HAS = Hasselbachtal; KAT = Kattensiepen; MÜS = Müssenberg; OES = Oese; O-R = Oberrödinghausen; STO = Stockum; WOC = Wocklum.
Fig. 19 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 19. Globimitoceras globiforme (Vöhringer, 1960) from the Oberrödinghausen railway cutting. A. Cross section of paratype GPIT-PV-63923 from bed 2. B. Cross section of paratype GPIT-PV-63934 from bed 3e. C. Suture line of holotype GPIT-PV-63925 from bed 2, at ww = 20.5 mm, wh = 9.4 mm. D. Constriction course of specimen MB.C.31061, at dm = 32.5 mm, ww = 30.0 mm, wh =18.5 mm. E–G. Ontogenetic development of the conch width index (ww/dm), umbilical width index (uw/ dm), whorl width index (ww/wh) and whorl expansion rate (WER) of selected specimens. Scale bar units = 1 mm.
Fig. 11 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 11. The morphological terms used in the description of the ammonoid conchs and suture lines.
Data from: Positive relationship between genetic- and species diversity on limestone outcrops in the Carpathian Mountains
We asked if the genetic diversity of Saponaria bellidifolia (a habitat specialist plant) and the species diversity of its habitat are driven by parallel landscape-level processes in an island-like system of limestone outcrops in the Carpathian Mountains. We tested the relationship of these two diversity levels at local and regional geographic scales. Local genetic and species diversity showed parallel patterns influenced by the number of plant communities. Likewise, at regional level there was strong evidence for parallel equilibrial dynamics of genotypes and species. However, a superimposed matrix effect enhanced the regional species diversity only. Genetic diversity of habitat specialist organisms and species diversity of these limestone outcrop islands on mainland are modulated by parallel landscape-level processes at different geographic scales, and mechanisms may be identified at very high spatial resolutions.
Data from: Late Triassic (Julian) conodont biostratigraphy of a transition from reefal limestones to deep-water environments on the Cimmerian terranes (Taurus mountains, southern Turkey)
Sections at Aşağiyaylabel and Yukariyaylabel, Taurus Mountains, southern Turkey, provide a rare opportunity to investigate conodont faunas in detail across a reef to slope transition. Intensive sampling of limestone beds (wackestones to packstones) through approximately 3 m at these locations has led to the recognition of a new lower Carnian (Julian 1/2) conodont fauna within the Kartoz and Kasimlar formations. Members of the subfamilies Paragondolellinae and Pseudofurnishiinae are recognized. The genus Kraussodontus is reported for the first time from the Taurus Mountains. Mosherella postkockeli and Mosherella praebudaensis sp. nov. occur within the lower Carnian Carbonate Member of the Kasimlar Formation from the Taurus Platform Units. The discovery of the new conodont assemblages from Aşağiyaylabel and Yukariyaylabel facilitates a correlation with faunal assemblages worldwide.
FIGURE. In situ photos of Paphiopedilum charlesworthii var. lannaense. A. limestone mountain at 1,100–1,200 m elevation, B. P. charlesworthii var. lannaense living on vertical cliffs of limestone, C. P. charlesworthii var. lannaense plant, D. flowering plant with flower bud, E., F. flowering plant (flower color was faded because these photos were taken toward the end of flowering period) (photo. By S. Somboonphon) in Paphiopedilum charlesworthii var. lannaense, a new slipper orchid from Northern Thailand identified by morphological and AFLP analyses
FIGURE. In situ photos of Paphiopedilum charlesworthii var. lannaense. A. limestone mountain at 1,100–1,200 m elevation, B. P. charlesworthii var. lannaense living on vertical cliffs of limestone, C. P. charlesworthii var. lannaense plant, D. flowering plant with flower bud, E., F. flowering plant (flower color was faded because these photos were taken toward the end of flowering period) (photo. By S. Somboonphon)
On following pages: 631. Ryukyu Islands Tree Rat (Diplothrix legata); 632. Lesser Bandicoot Rat (Bandicota bengalensis); 633. Greater Bandicoot Rat (Bandicota indica); 634. Savile's Bandicoot Rat (Bandicota savilei), 635. Mackenzie's White-toothed Rat (Berylmys mackenziel); 636. Manipur White-toothed Rat (Berylmys manipulus); 637. Bowers's White-toothed Rat (Berylmys bowersii); 638. Berdmore's White-toothed Rat (Bery/mys berdmorei); 639. Millard's Rat (Dacnomys millard)); 640. Brahman White-bellied Rat (Niviventer brahma); 641. Smoke-bellied White-bellied Rat (Niviventer eha); 642. Anderson's White-bellied Rat (Niviventer andersoni), 643. Sichuan White-bellied Rat (Niviventer excelsion); 644. South China White-bellied Rat (Niviventer huang); 645. Hainan White-bellied Rat (Niviventer lotipes); 646. Himalayan White-bellied Rat (Niviventer niviventen; 647. Spiny Taiwan White-bellied Rat (Niviventer coninga); 648. Soft-furred Taiwan White-bellied Rat (Niviventer culturatus), 649. Cameron Highlands White-bellied Rat (Niviventer cameron); 650. Indochinese White-bellied Rat (Niviventer fulvescens); 651. Bukit White-bellied Rat (Niviventer bukit); 652. Confucian White-bellied Rat (Niviventer confucianus); 653. Limestone White-bellied Rat (Niviventer hinpoon); 654. Indochinese Mountain White-bellied Rat (Niviventer tenaster); 655. Sundaic Arboreal White-bellied Rat (Niviventer cremoriventer); 656. Montane Sumatran White-bellied Rat (Niviventer fraternus);, 657. Montane Javan White-bellied Rat (Niviventer lepturus); 658. Montane Bornean White-bellied Rat (Niviventer rapit). in Muridae
On following pages: 631. Ryukyu Islands Tree Rat (Diplothrix legata); 632. Lesser Bandicoot Rat (Bandicota bengalensis); 633. Greater Bandicoot Rat (Bandicota indica); 634. Savile's Bandicoot Rat (Bandicota savilei), 635. Mackenzie's White-toothed Rat (Berylmys mackenziel); 636. Manipur White-toothed Rat (Berylmys manipulus); 637. Bowers's White-toothed Rat (Berylmys bowersii); 638. Berdmore's White-toothed Rat (Bery/mys berdmorei); 639. Millard's Rat (Dacnomys millard)); 640. Brahman White-bellied Rat (Niviventer brahma); 641. Smoke-bellied White-bellied Rat (Niviventer eha); 642. Anderson's White-bellied Rat (Niviventer andersoni), 643. Sichuan White-bellied Rat (Niviventer excelsion); 644. South China White-bellied Rat (Niviventer huang); 645. Hainan White-bellied Rat (Niviventer lotipes); 646. Himalayan White-bellied Rat (Niviventer niviventen; 647. Spiny Taiwan White-bellied Rat (Niviventer coninga); 648. Soft-furred Taiwan White-bellied Rat (Niviventer culturatus), 649. Cameron Highlands White-bellied Rat (Niviventer cameron); 650. Indochinese White-bellied Rat (Niviventer fulvescens); 651. Bukit White-bellied Rat (Niviventer bukit); 652. Confucian White-bellied Rat (Niviventer confucianus); 653. Limestone White-bellied Rat (Niviventer hinpoon); 654. Indochinese Mountain White-bellied Rat (Niviventer tenaster); 655. Sundaic Arboreal White-bellied Rat (Niviventer cremoriventer); 656. Montane Sumatran White-bellied Rat (Niviventer fraternus);, 657. Montane Javan White-bellied Rat (Niviventer lepturus); 658. Montane Bornean White-bellied Rat (Niviventer rapit).
FIGURE 11. Polystichum paucicarpum.—A. Limestone mountains where the new species was discovered.—B, C in Seven new species of Polystichum (subg. Haplopolystichum; Dryopteridaceae) from southern China
FIGURE 11. Polystichum paucicarpum.—A. Limestone mountains where the new species was discovered.—B, C. Habitats and plants.— D. Portions of adaxial laminae.—E. Portion of stipe showing scales.—F, G. Polar views of spores under SEM.
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