摘要：Cold-seep carbonate concretions were preserved in the Chiahsien paleoseep remnant within the Pliocene Yenshuiken Formation of southwestern Taiwan foreland sequence. Compared to the non-seep controls in the Yenshuiken Formation, muddy host rocks that were 30 cm away from such ACCs have normal marine assemblages (low agglutinated foraminifera percentages, 80 cm away from the chimneys have normal assemblages. Host rocks between pipe-shaped ACCs have similar characteristics to mudstone samples from control sites. Low percentages of calcareous foraminiferal fossils in the paleoseep remnant are due to pore water acidification within the taphonomically active zone (TAZ), which is triggered and accelerated by oxidation of sulfide [HS - , the product of anaerobic oxidation of methane (AOM)] in the methane seep environments. We suggest that foraminiferal assemblages can be influenced by methane seep activities taphonomically and that, therefore, ratios between calcareous and agglutinated foraminifera can reflect and record geochemical interface [e.g., TAZ; sulfate-methane interface (SMI) where AOM occurs] shifts on a subtler scale (only few decimeters) in paleoseep remnants.
关键词：Cold seep remnant; Foraminifera; Taphonomically active zone; Pliocene; Southwestern Taiwan;
