A giant Paleodictyon gomezi with a maximum mesh diameter of 13 cm and cover
ing more than 0.5 m(2) occurs in the lower Eocene flysch near Zumaya. The g
iant Paleodictyon occurs with flute casts and, therefore, must have been pr
oduced deeply in the sediment. The lengthening of mesh cells parallel and p
erpendicular to the flute casts implies changing current directions during
trace production. Rows of elongate and offset mesh cells reflect the row-by
-row production of the trace; however: the base line followed by the trace
fossil producer (meandering or spiral) cannot be reconstructed because of i
ncomplete preservation. The extraordinary size of this giant Paleodictyon c
ontradicts the evolutionary trend of deep-sea trace fossils toward optimiza
tion and miniaturization, since similar large Paleodictyon specimens occur
in Silurian flysch. (C) 2000 Elsevier Science B.V. All rights reserved.