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87 results for “shallow marine”
Data for "Combining 13C, 15N, and 2H tracer to measure feeding and metabolic activity in marine, shallow-water sponges – A pilot study"
<p>This dataset includes raw data used in the paper "Combining <sup>13</sup>C, <sup>15</sup>N, and <sup>2</sup>H tracer to measure feeding and metabolic activity in marine, shallow-water sponges – A pilot study" (JEMBE).</p>
Figure 3 in Culturable fungi associated with the marine shallow-water hydrothermal vent crab Xenograpsus testudinatus at Kueishan Island, Taiwan
Figure 3: Taxonomic classification of all fungi reported (by this study and previously published work) on the crab XenograpsUs testUdinatUs.
Figure 2 in Culturable fungi associated with the marine shallow-water hydrothermal vent crab Xenograpsus testudinatus at Kueishan Island, Taiwan
Figure 2: Taxonomic classification of the fungi isolated from the carapace of the crab XenograpsUs testUdinatUs collected in the hydrothermal vent area of Kueishan Island, Taiwan.
Figure 1 in Culturable fungi associated with the marine shallow-water hydrothermal vent crab Xenograpsus testudinatus at Kueishan Island, Taiwan
Figure 1: (A) Location of Kueishan Island (box) at the northeastern end of the main Taiwan Island. (B) Kueishan Island showing the vent and sampling locations. (C) XenograpsUs testUdinatUs, the hydrothermal vent crab.
Figure 4 in Culturable fungi associated with the marine shallow-water hydrothermal vent crab Xenograpsus testudinatus at Kueishan Island, Taiwan
Figure 4: Comparison of fungal diversity on the vent crab XenograpsUs testUdinatUs, in yellow sediment (with sulfur granules) and in black sediment (with no sulfur granules) collected in the hydrothermal vent area of Kueishan Island, Taiwan.
Fig. 8 in Gyrochorte "highways" and their environmental significance in shallow-marine sediments
Fig. 8. Gyrochorte "highways" documenting a sequorichnial behaviour of the producers from different localities. A, B. Agrio Formation, Cretaceous, Neuquén Basin, Argentina. A. Bed surface showing interference ripples cross-cut by Spongeliomorpha ichsp. (Sp). B. Ripple-trough fill reworked by Chondrites ichsp. (Ch) producers (black doted lines). C. Lajas Formation, Upper Jurassic, Neuquén Basin, Argentina; converging (black arrows), diverging white arrows), and overlapping Gyrochorte ichsp. (white doted line). D. Middle Jurassic, Helvetic realm, exact location not recorded, Switzerland (NMB O157) showing parallel Gyrochorte ichsp., 2 parallel traces (white doted line between them), 3 parallel traces (black doted line between them). Specimens A–C left in the field.
Fig. 6 in Gyrochorte "highways" and their environmental significance in shallow-marine sediments
Fig. 6. Trace fossils co-occurring with "burrowing highways" of Gyrochorte ichsp. A. Mutual cross-cutting of Gyrochorte ichsp. (1, 2) and Phycosiphon incertum Fischer-Ooster, 1856 (Ph) exhibiting typical elbow-shaped turns (white arrows); Gyrochorte comosa Heer, 1865 overprinting Phycosiphon ichsp. (1, white doted line; bilobate crest of Gyrochorte well visible); Phycosiphon ichsp. overprinted by G. comosa (2, white doted line; bilobate crest of Gyrochorte ichsp. not clearly developed while bioturbated); G. comosa showing transition to Gyrochorte variabilis Fürsich, Alberti, and Pandey, 2017 expressed by fan-like appearance (shift of causative tube marked by black arrow). B. Gyrochorte comosa associated with Ptychoplasma ichsp. (P); sequorichnial behaviour of several Gyrochorte ichsp. producers is evidenced by parallel and/or overlapping traces (parallel traces, white doted lines; diverging/converging traces, white arrows). C. Parallel Gyrochorte comosa showing sequorichial behaviour (white arrows) associated with bivalve trace Siphonichnus ichsp. (b) (surrounded by black doted line) and cross-section of Lockeia ichsp. (surrounded by white doted line); G. comosa showing transition to G. variabilis expressed by fan-like appearance (shift of causative tube marked by black arrow). All specimens left in the field.
Fig. 4 in Gyrochorte "highways" and their environmental significance in shallow-marine sediments
Fig. 4. Different ichnospecies of Gyrochorte encountered in the Mulichinco Formation, Lower Cretaceous, Puerto Curaco, Neuquén Province, Argentina field photographs). A. Two parallel Gyrochorte comosa Heer, 1865 (black arrows, lower left), one continuing as such (black arrow, upper right), and one diverging from parallel course and becoming Gyrochorte variabilis Fürsich, Alberti, and Pandey, 2017 (shift of causative tube indicated by white arrow). B. Gyrochorte variabilis exhibiting circular, slightly bilobate pads (black arrows). C. Gyrochorte variabilis composed of elongate pads (black arrow) becoming oblique with slight zigzag pattern (white arrow). For details about G. variabilis see Fürsich et al. (2017). All specimens left in the field.
Fig. 3. Trace fossil Gyrochorte comosa Heer, 1865 in Gyrochorte "highways" and their environmental significance in shallow-marine sediments
Fig. 3. Trace fossil Gyrochorte comosa Heer, 1865 on bed surfaces structured by wave ripples; Mulichinco Formation, Lower Cretaceous, Puerto Curaco, Neuquén Province, Argentina (field photographs). A. Gyrochorte comosa on bed surface exhibiting parallel-crested, symmetric ripples. B. Parallelcrested, slightly asymmetric ripples traversed by G. comosa being more frequent at the stoss-side and the crest of the ripples. C. Bed surface structured by interfering symmetric ripples documenting sequorichnial behaviour of G. comosa producers (black arrows, "converging" traces; white arrows, "diverging" traces); note acute angle between diverging or converging traces. D. Bed surface exhibiting parallel-crested, slightly asymmetric ripples; G. comosa is overtopped by sand at the lee side of the ripples (white arrows). All specimens left in the field.
Fig. 1 in Gyrochorte "highways" and their environmental significance in shallow-marine sediments
Fig. 1. Location map (based on Schwarz 2012), asterisk marks the study area within the Neuquén Basin (highlighted) while the inset refers to the location of the detailed map within South America.
Fig. 7 in Gyrochorte "highways" and their environmental significance in shallow-marine sediments
Fig. 7. "Burrowing highways" of Gyrochorte comosa Heer, 1865 in the Mulichinco Formation, Lower Cretaceous, Puerto Curaco, Neuquén Province, Argentina (field photographs). Crowded parallel and overlapping G. comosa concentrated at ripple crest (A–E). Note acute angle between sequorichnial Gyrochorte ichsp. (arrows, traces converging to and diverging from a parallel course; doted lines, parallel/overlapping traces). All specimens left in the field.
Text-fig. 3. Palaeogeographic distribution of Schloenbachia lymensis (red dots) in the Upper Cenomanian Calycoceras guerangeri through the Metoicoceras geslinianum Zones. Light blue – shallow epicontinental sea, dark blue – deep marine settings, yellow – land. * asterisk – occurrence in the BCB (modified after Wilmsen 2012). in Taxonomy And Stratigraphic Distribution Of The Ammonite Schloenbachia Neumayr, 1875 From The Bohemian Cretaceous Basin
Text-fig. 3. Palaeogeographic distribution of Schloenbachia lymensis (red dots) in the Upper Cenomanian Calycoceras guerangeri through the Metoicoceras geslinianum Zones. Light blue – shallow epicontinental sea, dark blue – deep marine settings, yellow – land. * asterisk – occurrence in the BCB (modified after Wilmsen 2012).
FIG. 15 in Three new species of Macrocyprina Triebel, 1960 (Crustacea, Ostracoda, Macrocyprididae) from Brazilian shallow marine waters
FIG. 15. — Geographic distribution of Macrocyprina along Brazilian coast; 1, Macrocyprina sp. of Coimbra (1995) and Coimbra et al. (1999); 2, M. rocas n. sp.; 3, M. coimbrai n. sp.; 4, M. youngi n. sp.; 5, M. sp. of Dias-Brito et al. (1988).
FIG. 13. — Macrocyprina coimbrai n in Three new species of Macrocyprina Triebel, 1960 (Crustacea, Ostracoda, Macrocyprididae) from Brazilian shallow marine waters
FIG. 13. — Macrocyprina coimbrai n. sp.; A, paratype (MNRJ 15714), spm 7; B-F, holotype (MNRJ 15706); A, female appendage V; B, male right appendage V; C, male left appendage V; D, appendage VI; E, appendage VII; F, furca. Scale bars: 0.2 mm.
FIG. 11. — Macrocyprina coimbrai n in Three new species of Macrocyprina Triebel, 1960 (Crustacea, Ostracoda, Macrocyprididae) from Brazilian shallow marine waters
FIG. 11. — Macrocyprina coimbrai n. sp.; A, B, E, holotype (MNRJ 15706); C, D, paratype (MNRJ 15713), spm 2; F, G, paratype (MNRJ 15714), spm 5; A, right valve; B, left valve; C, right valve; D, left valve; E, adductor muscle scars; F, dorsal view of carapace; G, ventral view of carapace. The arrows point towards the anterior of the animal. Scale bars: A-D, F, G, 1 mm; E, 0.1 mm.
FIG. 10. — Macrocyprina rocas n in Three new species of Macrocyprina Triebel, 1960 (Crustacea, Ostracoda, Macrocyprididae) from Brazilian shallow marine waters
FIG. 10. — Macrocyprina rocas n. sp., paratypes (MNRJ 15703); A, spm 7,; B, D, spm 3,; C, spm 1,; A, B, hemipenis; C, D, Zenker's organs. Scale bars: 0.3 mm.
FIG. 4. — Macrocyprina youngi n in Three new species of Macrocyprina Triebel, 1960 (Crustacea, Ostracoda, Macrocyprididae) from Brazilian shallow marine waters
FIG. 4. — Macrocyprina youngi n. sp., paratypes (MNRJ 15701); A-D, F-H, spm 8,; E, spm 6,; A, male right appendage V; B, anterior lobe of male right appendage V; C, male left appendage V; D, podomere II male left appendage V; E, female appendage V; F, appendage VI; G, appendage VII; H, furca. Scale bars: A-D, 0.1 mm; E, H, 0.2 mm; F, G, 0.3 mm.
FIG. 3. — Macrocyprina youngi n in Three new species of Macrocyprina Triebel, 1960 (Crustacea, Ostracoda, Macrocyprididae) from Brazilian shallow marine waters
FIG. 3. — Macrocyprina youngi n. sp., paratype (MNRJ 15701) spm 8; A, mandible; B, masticatory jaw of mandible; C, exopodite of mandible; D, podomere II of palp of mandible; E, podomere III of palp of mandible; F, podomere IV of palp of mandible; G, maxilla I; H, vibratory plate of maxilla I; I, endite I of maxilla I; J, endite II of maxilla I; K, endite III of maxilla I; L, podomere III of palp of maxilla I. Scale bars: 0.1 mm.
FIG. 5. — Macrocyprina youngi n in Three new species of Macrocyprina Triebel, 1960 (Crustacea, Ostracoda, Macrocyprididae) from Brazilian shallow marine waters
FIG. 5. — Macrocyprina youngi n. sp., paratypes (MNRJ 15701); A, spm 4,; B, C, spm 8,; D, spm 10,; A, B, hemipenis; C, D, Zenker's organs. Scale bars: 0.4 mm.
FIG. 14. — Macrocyprina coimbrai n in Three new species of Macrocyprina Triebel, 1960 (Crustacea, Ostracoda, Macrocyprididae) from Brazilian shallow marine waters
FIG. 14. — Macrocyprina coimbrai n. sp.; A, C, holotype (MNRJ 15706); B, D, paratype (MNRJ 15714), spm 5,; A, B, hemipenis; C, D, Zenker's organs. Scale bars: 0.5 mm.
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Allen Brain Atlas
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International Brain Laboratory public data
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OpenNeuro
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