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FIGURE 4 Lower offshore silty mudstones with ichnological suites consistent with a distal expres-
sion of the Cruziana Ichnofacies. (A) Unit shows BI ¼ 5, with abundant Phycosiphon ( Ph ), with
Chondrites ( Ch ), and rare, muddy Zoophycos ( Z ). (B) Unit shows BI ¼ 5, with robust Zoophycos
( Z ), Helminthopsis ( H ), Planolites ( P ), Phycosiphon ( Ph ), Chondrites ( Ch ), Teichichnus ( T ), and
Thalassinoides ( Th ). (C) Unit shows BI ¼ 5, with Asterosoma ( As ), Thalassinoides ( Th ), Zoophycos
( Z ) (example cut oblique to the chevrons), Phycosiphon ( Ph ), Chondrites ( Ch ), Schaubcylindrichnus
freyi ( Sf ), and Planolites ( P ). (D) Bioturbated silty mudstone showing BI ¼ 5, interbedded with thin,
wavy parallel-laminated sandstone beds with BI ¼ 0-2. Laminated sandstone beds correspond to dis-
tal tempestites. Trace fossils include Phycosiphon ( Ph ), Cosmorhaphe ( Cr ), Helminthopsis ( H ), Pla-
nolites (P), and Chondrites ( Ch ). Scale bars in centimeters.
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