Distinguishing Autochthony, Parautochthony and Allochthony Using Taphofacies Analysis: Can Cold Seep Assemblages Be Discriminated from Assemblages of the Nearshore and Continental Shelf?

Identifying ancient cold seep faunas is intertwined with the problem of distinguishing autochthony from parautochthony. Cold seep faunas are autochthonous assemblages. Taphofacies from an allochthonous microtidal inlet, a parautochthonous inner shelf and an autochthonous upper slope (representing cold seep faunas) were compared to identify their distinguishing characteristics and to facilitate cold seep recognition. The taphonomic signature of the allochthonous inlet assemblage is dominated by abrasion and edge alteration. Bivalves are completely disarticulated

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