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15 results for “Biofacies”
Figure 10 in Recent Benthic foraminiferal biofacies in the Bakkhali region, West Bengal, India
Figure 10. (a)Variation of Total Foraminiferal Number with depth (C2); (b) Variation of living foraminifera with depth (C2).
Figure 9 in Recent Benthic foraminiferal biofacies in the Bakkhali region, West Bengal, India
Figure 9. (a) Variation of Total Foraminiferal Number with depth (C1); (b) Variation of living foraminifera with depth (C1).
Plate 3.1 7 in Recent Benthic foraminiferal biofacies in the Bakkhali region, West Bengal, India
Plate 3.1 7 – Asterorotalia pulchella (S); 18 - Asterorotalia pulchella (U); 19 – Cribroelphidium hispidulum (U); 20 – Cribroelphidium poeynum (U); Legends: S – Spiral view; U – Umbilical view; Si – Side view.
Figure 6 in Recent Benthic foraminiferal biofacies in the Bakkhali region, West Bengal, India
Figure 6. Biofacies map of the study area based on the living population of foraminifera (yellow representing Ammonia tepida – Ammonia beccarii biofacies, green representing Haynesina germanica – Ammonia tepida biofacies and red representing Ammonia tepida – Haynesina germanica biofacies).
Figure 1 in Recent Benthic foraminiferal biofacies in the Bakkhali region, West Bengal, India
Figure 1. Location map showing the sampling stations (circular shape denotes surface sampling whereas star shape denotes core sampling).
Plate 1. 1 in Recent Benthic foraminiferal biofacies in the Bakkhali region, West Bengal, India
Plate 1. 1 – Ammodiscus evolutus (Si); 2 – Miliammina fusca (Si); 3 – Miliammina petila (Si); 4 – Haplophragmoides wilberti (S); 5 – Ammotium agglutinas. (Si); 6 – Trochammina inflata (S); 7 – Trochammina inflata (U); 8 – Quinqueloculina seminulum (Si). Legends: Si – Side view; S – Spiral view; U – Umbilical view.
Plate 2. 9 in Recent Benthic foraminiferal biofacies in the Bakkhali region, West Bengal, India
Plate 2. 9 - Quinqueloculina sp. (Si); 10 – Haynesina depressula (U); 11 – Haynesina germanica (U); 12 – Nonionella labradorica (U); 13 – Ammonia beccarii (S); 14 - Ammonia beccarii (U); 15 – Ammonia tepida (S); 16 - Ammonia tepida (U). Legends: Si – Side view; U– Umbilical view; S – Spiral view.
Figure 2 in Recent Benthic foraminiferal biofacies in the Bakkhali region, West Bengal, India
Figure 2. Fisher α diversity plot showing surface sampling locations (circle representing Patibhunia marshes; star representing Bakkhali beach and triangle representing Henry's island marshes).
Figure 4 in Recent Benthic foraminiferal biofacies in the Bakkhali region, West Bengal, India
Figure 4. Seasonal variation of Total Foraminifera of the study area.
Figure 7 in Recent Benthic foraminiferal biofacies in the Bakkhali region, West Bengal, India
Figure 7. Ternary plot showing surface sampling locations.
Figure 8 in Recent Benthic foraminiferal biofacies in the Bakkhali region, West Bengal, India
Figure 8. Species richness plot showing surface sampling locations.
Figure 5 in Recent Benthic foraminiferal biofacies in the Bakkhali region, West Bengal, India
Figure 5. Seasonal variation of living foraminifera in the study area.
Figure 3 in Recent Benthic foraminiferal biofacies in the Bakkhali region, West Bengal, India
Figure 3. Species distribution in the sampling locations during pre-monsoon sampling.
Data from: Ecology, biofacies, biogeography and systematics of micromorphic lingulate brachiopods from the Ordovician (Darriwilian–Sandbian) of south-central China
Ordovician (Darriwilian to Sandbian) micromorphic linguliform lingulate brachiopods are described from the Guniutan Formation at the Fenxiang section in Hubei province, and the Maocaopu and Cili sections in Hunan province of south-central China, situated on the Yangtze Platform. A total of 7560 specimens from 155 limestone samples (within the interval of Lenodus variabilis – Pygodus anserinus biozones) are assigned to 22 species, representing a low taxonomic diversity and low abundance fauna. The fauna is dominated by the Acrotretoidea, mainly species of the Torynelasmatidae, with Torynelasma the most abundant (more than 40% of total number of specimens), along with the Eoconulidae and Eoconulus (18% of total) representing the second most common forms. Species of the Ephippelasmatidae are also common (16% of total) diverse, and include representatives of Myotreta and Numericoma, as well as Ephippelasma, whereas species of the Scaphelasmatidae are somewhat less common (13% of total). All three investigated sections represent outer shelf environments, but the Maocaopu section is situated in a relatively deeper position, in proximity of the south-eastern outer margin of the Upper Yangtze Platform, close to its boundary with the Jiangnan Slope. A quantitative analysis of the relative abundance data was carried out in order to investigate the biofacies distribution of the micromorphic brachiopod communities across the Yangtze Platform, something that has not been attempted before with Palaeozoic linguliforms. Six lingulate microbrachiopod communities could be recognized in the sections. The major biofacies shift, which occurred in the Cili section in the upper part of the Microzarkodina ozarkodella Zone, at the time of the onset and initial rise of the Mid Darriwilian Carbon Isotope Excursion (MDICE) suggests that these biofacies may have been depth controlled.
Data from: Ecology, biofacies, biogeography and systematics of micromorphic lingulate brachiopods from the Ordovician (Darriwilian–Sandbian) of south-central China
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