Find research datasets worth reusing

Fig. 7. A in Paleoecology, Taphonomy, and Biogeography of a Coenothyris Community (Brachiopoda, Terebratulida) from the Triassic (Upper Anisian-Lower Ladinian) of Israel

Fig. 7. A. Slab of juvenile specimens of Coenothyris. Note rare disarticulated ventral valve with small hinge teeth (arrow). Subunit 31, AMNH 46519. B. Cross section of Coenothyris Bed showing sparfilled articulated shells (bottom half) indicative of rapid burial that did not allow for the decay of soft tissues with subsequent displacement by sediment. The brachiopods just above the sparfilled zone (upper half) are mud filled, indicative of individuals that had died earlier and decayed to become infilled with sediment; approximately 25% of the shells were spar filled. Subunit 31, AMNH 46520. C. Cross section of Coenothyris Bed showing bivalve hash (composed mainly of the bivalve Myophoria) that served as a pavement for brachiopod spat. Subunit 31, AMNH 46521. Scale bar 5 2 cm.

Fig. 6. A, B in Paleoecology, Taphonomy, and Biogeography of a Coenothyris Community (Brachiopoda, Terebratulida) from the Triassic (Upper Anisian-Lower Ladinian) of Israel

Fig. 6. A, B. Slabs with normal populations of Coenothyris that range from ephebic to gerontic shells. A, Subunit 42, AMNH 46522; B, Subunit 42, NHM 1008. C. Cross section of Coenothyris horizon consisting of jumbled adult specimens similar in appearance to the Triassic German Muschelkalk. Subunit 42, AMNH 46522. Scale bar 5 2 cm.

Fig. 4 in Paleoecology, Taphonomy, and Biogeography of a Coenothyris Community (Brachiopoda, Terebratulida) from the Triassic (Upper Anisian-Lower Ladinian) of Israel

Fig. 4. Slab of juvenile specimens of Coenothyris that represents an obrution deposit. Note brachiopods in a horizontal to subhorizontal attitude relative to the sediment–water interface, many in dorsal side up position. Large bivalves under the brachiopods are Pleuromya. Subunit 31, AMNH 46518. See text for further discussion.

Fig. 1 in Paleoecology, Taphonomy, and Biogeography of a Coenothyris Community (Brachiopoda, Terebratulida) from the Triassic (Upper Anisian-Lower Ladinian) of Israel

Fig. 1. Location map of Precambrian–Oxfordian exposures in the Levant. 1, Precambrian; 2, Paleozoic–Triassic; 3, Jurassic; 4, Mount Hermon; 5, Alpine thrustfront; 6, 7, Neogene sinistral transform; I, Galilee High; II, Judean Embayment; III, Negev High; IV, Sinai Deep; with extension of Lower Oxfordian Majdal Shams shales (shaded area) and Jurassic isopachs (from Hirsch et al., 1998). ''Ramon'' signifies the Triassic Ramon Group, an anticlinorium that was breached through several phases of erosion, beginning in the Late Tertiary (Miocene–Pliocene), resulting in erosional cirques (Parnes, 1986). Tectonic movements since the Late Mesozoic, including reactivation of faults, resulted in the development of WSW–ENE to S–Ntrending reverse and thrust faults that today consist of several secondary monoclinal and domal buckles with an associated fault system (Zak, 1963).

Fig. 3 in Paleoecology, Taphonomy, and Biogeography of a Coenothyris Community (Brachiopoda, Terebratulida) from the Triassic (Upper Anisian-Lower Ladinian) of Israel

Fig. 3. Slab showing bivalve pavement colonized by Coenothyris oweni Feldman, subunit 31, AMNH 46517. Abbreviations: co, Coenothyris; pl, Pleuromya; mo, Modiolus; my, Myophoria; pa, Parallelodon. Note that this slab has relatively few brachiopods (compare with fig. 4). Scale bar 5 4 cm.

Fig. 5 in Paleoecology, Taphonomy, and Biogeography of a Coenothyris Community (Brachiopoda, Terebratulida) from the Triassic (Upper Anisian-Lower Ladinian) of Israel

Fig. 5. Slab of juvenile specimens of Coenothyris. Note the large Pleuromya, just offcenter, under which lie disarticulated Myphoria. Some shells are slightly exfoliated, but most are almost perfectly preserved. Subunit 31, AMNH 46524. See text for further discussion.

Fig. 2 in Paleoecology, Taphonomy, and Biogeography of a Coenothyris Community (Brachiopoda, Terebratulida) from the Triassic (Upper Anisian-Lower Ladinian) of Israel

Fig. 2. Generalized columnar section of the Triassic Saharonim Formation at Har Gevanim, Makhtesh Ramon, southern Israel. For detailed stratigraphy, see Druckman (1974b). Arrows represent occurrences of Coenothyris oweni Feldman at marked subunit intervals. Subunit designations are after Zak (1964) in Parnes (1975).

FIGURE 1 in Melvicalathis, a new brachiopod genus (Terebratulida: Chlidonophoridae) from deep sea volcanic substrates, and the biogeographic significance of the midocean ridge system *

FIGURE 1. The midocean ridge systems and geographic distributions of Melvicalathis macroctena (Zezina, 1981), and species of the related chlidonophorid brachiopod, Bathynanus (star symbols). Note the concentration along areas of probable hard rock substrates. The two stations of "Academic Kurchatov" (type locality) are adjacent to and on the Nazca Ridge. Key to symbols: "Academic Kurchatov", RV " Melville", FS "SONNE", "Eltanin" Cruise.

FIGURE 4 in Melvicalathis, a new brachiopod genus (Terebratulida: Chlidonophoridae) from deep sea volcanic substrates, and the biogeographic significance of the midocean ridge system *

FIGURE 4. Melvicalathis macroctena (Zezina, 1981) from the Galapagos Spreading Centre. A. Interior of dorsal valve of ZMB Bra 2014 showing descending branches of crura with incomplete transverse band, and internal ridges corresponding to external costal troughs. B. Closeup of previous photograph to show details of descending branches and incomplete loop. C. Spicular skeleton after dissolution of soft tissue. D. Closeup of triangular costae showing numerous closely spaced growth lines. E. Closeup of a valve of Eucalathis to show typical beaded tuberculate costae for comparison with D.

FIGURE 5. A–B in Melvicalathis, a new brachiopod genus (Terebratulida: Chlidonophoridae) from deep sea volcanic substrates, and the biogeographic significance of the midocean ridge system *

FIGURE 5. A–B. Line drawings of Melvicalathis macroctena (Zezina, 1981) from the type locality, south east Pacific. A. View of lophophore from the ventral side. B. View of lophophore from the dorsal side. C. Schematic illustration of the cryptic habit of Melvicalathis macroctena around the walls of small tabular voids immediately beneath basalt flow surfaces. The tubes with the brachiopods were found in larger boulders of fresh, glassy basalt at RV Melville Stn #116, Southeast Indian Ridge. D. Sketch of attachment of Melvicalathis on hard substrate and probable current system around lophophore. Key. 1, place where the lophophore was removed from the mantle and the dorsal body wall—internal details are seen through the transparent ventral wall of the lophophore; 2, mouth; 3, lip; 4, transparent (soft) dorsal wall of the

FIGURE 3 in Melvicalathis, a new brachiopod genus (Terebratulida: Chlidonophoridae) from deep sea volcanic substrates, and the biogeographic significance of the midocean ridge system *

FIGURE 3. Melvicalathis macroctena (Zezina, 1981) from the Southeast Indian Ridge. A. Interior of AU B320 showing small cardinal process, internal view of costae, and correspondence between costae and scalloped margin. B. Lateral view of AU B320 showing slightly biconvex valves and strongly attrite beak. C. Posterior view of AU B320 to show hypothyrid foramen and costae. D. Closeup of C, showing pedicle collar, teeth and punctae. E. Closeup of ventral valve of AU B321 showing pedicle collar, teeth, and very narrow deltidial plates. F. Closeup of dorsal valve of AU B321 showing retracted dried pedicle, sockets and socket ridges, proximal end of crura, and part of dried lophophore. G. Lateral view of AU B321 to show rounded, ventrallydirected crural processes and dried lophophore.

FIGURE 6 in Melvicalathis, a new brachiopod genus (Terebratulida: Chlidonophoridae) from deep sea volcanic substrates, and the biogeographic significance of the midocean ridge system *

FIGURE 6. Melvicalathis macroctena (Zezina, 1981) from the Southeast Indian Ridge A. Closeup of AU B320 to show detail of angular costae, triangular in cross section, numerous closely spaced growth lines, and small, evenly spaced punctae. B. Closeup of costae showing quincunx arrangement of punctae. C. Interior of valve margin to show shell fibres, punctae and slightly tuberculate margin.

FIGURE 11. Rhaetina rainei n in Otapirian (Rhaetian) Terebratulida (Brachiopoda) of Zealandia

FIGURE 11. Rhaetina rainei n. sp. (Nelson). 1 BR 3430 (N28/f7454) internal mould (a) dorsal (b) ventral. 2 BR 3461 (N28/f7454) internal mould (a) dorsal (b) ventral. 3 BR 3490 (N28/f7454) latex of dorsal valve interior. 4 BR 3452 (N28/f7454 internal mould (a) dorsal (b) ventral (c) lateral (d) anterior. 5 BR 1014 (N28/f7522) ventral view (Specimen figured by Marwick (1953) as Coenothyris sp.; photo Marianna Terezow). 6 BR 3456 (N28/f7454) internal mould (a) dorsal (b) ventral (c) lateral (d) posterior. 7 BR 3424 (N28/f7454) internal mould with remnant shell (a) dorsal (b) ventral (c) lateral (d) posterior (e) anterior. 8 BR3500 (N28/f7455) internal mould, ventral. 9 BR 3498 (N28/f7454) latex of ventral valve interior and beak. 10 BR 3439 (N28/f7454) ventral view. 11 BR 3422 (N28/f7454) internal mould (a) dorsal (b) ventral.

FIGURE 6 in Otapirian (Rhaetian) Terebratulida (Brachiopoda) of Zealandia

FIGURE 6. Detailed view of beak area, Tibetothyris johnstoni n. sp. A Holotype BR 3420 (N28/f7454), dorsal view of internal mould showing pedicle collar, ridged septalium, broad median septum and short, widely divergent dental plates. B C1970 (E45/f6635) dorsal view of internal mould, showing small cardinal process.

FIGURE 10. Rhaetina rainei n in Otapirian (Rhaetian) Terebratulida (Brachiopoda) of Zealandia

FIGURE 10. Rhaetina rainei n. sp. (New Caledonia). 1 Holotype B876 (NC/f0519) shelly specimen (a) dorsal (b) ventral (c) lateral (d) posterior (e) anterior. 2 B875 (NC/f0519) shelly specimen (a) dorsal (b) lateral. 3 B871 (NC/f0503) shelly specimen, ventral. 4 B844 (NC/f0007A) shelly specimen, ventral. 5 B881 (NC/f0005A) partly shelly specimen (a) dorsal (b) ventral (c) lateral. 6 BR 3414 (NC/f0020) shelly specimen (a) dorsal (b) ventral (c) lateral. 7 B880 (NC/f0005A) dorsal view of beak. 8 B820 (NC/f0087A) shelly specimen, anterior.

FIGURE 17. Zeilleria n in Otapirian (Rhaetian) Terebratulida (Brachiopoda) of Zealandia

FIGURE 17. Zeilleria n. sp. (x1) 1 B832 (NC/f0007A) shelly specimen (a) dorsal (b) ventral (c) lateral (d) anterior

FIGURE 3. A in Otapirian (Rhaetian) Terebratulida (Brachiopoda) of Zealandia

FIGURE 3. A Zealandia, showing the area of submerged continental crust surrounding New Zealand and extending to New Caledonia. Base map: NIWA (National Institute of Water and Atmospheric Research). B New Caledonia, showing location of Moindou-Téremba area and Baie de St Vincent (Fig. 4A). C New Zealand, showing Kawhia, (Fig. 4B) Nelson and Southland (Fig. 4C) synclines, Alpine Fault and plate boundary.

FIGURE 5. Tibetothyris johnstoni n in Otapirian (Rhaetian) Terebratulida (Brachiopoda) of Zealandia

FIGURE 5. Tibetothyris johnstoni n. sp. 1 Holotype BR 3420 (N28/f7454) (a) dorsal (b) ventral (c) lateral (d) posterior (e) anterior. 2 BR 3419 (N28/f7454) (a) dorsal (b) ventral (c) lateral (d) posterior. 3 B890 (NC/f0109B) shelly specimen, ventral. 4 C1963 (E45/f6635) partly shelly specimen (a) dorsal (b) ventral (c) lateral (d) anterior. 5 C1965 (E45/f6635) internal mould, distorted, dorsal. 6 C1967 (E45/f6635) internal mould (a) dorsal (b) ventral (c) lateral (d) posterior (e) anterior. 7 C1970 (E45/f6635) internal mould (a) dorsal (b) ventral (c) lateral (d) posterior (e) anterior. 8 C1971 (E45/f6635) internal mould (a) dorsal (b) ventral (c) lateral.

FIGURE 14 in Otapirian (Rhaetian) Terebratulida (Brachiopoda) of Zealandia

FIGURE 14. Detailed views of beak area, Lobothyris richardsi n. sp. A holotype, BR3286 (R15/f8585) dorsal view of partly shelly specimen showing beak, foramen and deltidial plates. B OU 17887 (F45/f0217) dorsal view of internal mould showing foramen surrounded by pedicle collar. C C2009 (E45/f6635) dorsal view of partly shelly specimen showing beak, foramen and deltidial plates, and low muscle scars on dorsal valve. D C2014 (E45/f6635) dorsal view internal mould, showing beak, foramen and beak ridges. Left side of ventral valve damaged.

FIGURE 2 in Otapirian (Rhaetian) Terebratulida (Brachiopoda) of Zealandia

FIGURE 2. Late Triassic - Jurassic timescale and range chart showing correlations between New Zealand and international stages (adapted from Raine et al. 2015) and ranges of Zealandian terebratulide species.