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    Late Devonian benthic ostracods from western Junggar, NW China: Implications for palaeoenvironmental reconstruction
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    Abstract:
    This study focuses on the palaeoecology of the Late Devonian ostracods based on more than 4,500 carapaces and valves collected from stratal sections in western Junggar, NW China. According to the ostracod faunas from the Hongguleleng Formation, 3 ecological assemblages are proposed for open oceanic island arc context, that is, Ostracod Assemblage‐1, Ostracod Assemblage‐2, and Ostracod Assemblage‐3. They characterize the foreshore, nearshore, and offshore environments, respectively. The water energy should be the first environmental factor controlling the composition of the ostracod assemblages from the Lower Member of the Hongguleleng Formation, and salinity fluctuations could be also involved.
    Keywords:
    Ostracod
    Paleoecology
    Assemblage (archaeology)
    Late Devonian extinction
    This text presents the proceedings of the 12th International Symposium on the subclass Ostracoda and ostracod biostratigraphy. Topics covered include: structural elements on the surface of ostracod shells; early Cretaceous ostracods; and taphonomy of ostracods from metamorphic rocks.
    Ostracod
    Taphonomy
    Citations (74)
    SUMMARY An interdisciplinary biostratigraphical study of Tournaisian–early Viséan sedimentary rocks from six sections in central Scotland has established the ranges of important palynomorph and ostracod taxa that can be used to refine the existing palynomorph-based biozonation scheme. The work highlights the value of joint ostracod-palynomorph studies in correlating sequences where a single biostratigraphical discipline alone cannot provide the resolution needed. To this end, a new joint palynomorph/ostracod stratigraphical assemblage, the Acanthotriletes cf. macrogaleatus – Sulcella affiliata Assemblage, has been established. This assemblage correlates with the upper part of the CM Biozone and allows the CM–Pu biozonal boundary to be positioned more reliably in the Midland Valley of Scotland (MVS) than previously. The distribution of the assemblage, and the palaeontological characteristics of the Ballagan Formation and stratigraphically higher formations in the Dinantian of the MVS, show that significant but localized hiatuses, correlating with the Pu, TS and TC biozones, occur in parts of the western MVS, while generally smaller hiatuses, correlating with the TS Biozone and possibly part of the Pu Biozone, exist in the east of the MVS and in parts of the Cockburnspath Outlier (Dunbar-Oldhamstocks Basin).
    Ostracod
    Citations (23)