Mk. Gingras et al., The ichnology of modern and Pleistocene brackish-water deposits at WillapaBay, Washington: Variability in estuarine settings, PALAIOS, 14(4), 1999, pp. 352-374
Detailed analysis of modern and Pleistocene deposits at Willapa Bay, Washin
gton concentrated on identifying ichnological and sedimentological characte
ristics of five estuarine subenvironments. These include: (1) intertidal fl
at deposits, which are typically thoroughly bioturbated by a somewhat dimin
utive suite of various vertical and horizontal shafts and burrows that are
locally cross-cut by robust crustacean dwellings; (2) unburrowed to rarely
burrowed tidal creek point-bar deposits, which are sporadically burrowed by
minute Gyrolithes, Skolithos, Cylindrichnus, Planolites, Palaeophycus, and
rare bivalve equilibrichnia; (3) fluvially- through tidally-influenced mai
n point-bar deposits, which are sporadically bioturbated with vertical trac
es superimposed upon inclined heterolithic stratification; (4) well to thor
oughly bioturbated bay deposits, burrowed by relatively robust forms of Oph
iomorpha, Teichichnus, Skolithos and bivalve equilibrichnia; and (5) locall
y bioturbated channel-bar deposits, typically displaying robust bivalve equ
ilibrichnia, rare Ophiomorpha, and deep-penetrating Skolithos. Traces from
both the modern and ancient deposits display a marked reduction in size and
diversity in the upper estuary.
Ongoing research at Willapa Bay confirms the validity of the brackish-water
model and provides data that potentially improve our understanding of thes
e deposits. Our findings suggest that strong textural controls are overprin
ted by salinity stresses; commonly vertical deposit-feeding structures, mad
e by infauna that are mining and/or stoping organic-rich laminae, are prese
nt; and there is a potential for the presence of large diameter crustacean
burrows in brackish deposits. This research emphasizes ichnologic variabili
ty due to autocyclic changes and climatic variability, and urges caution wh
en integrating ichnologic and sedimentologic data into a genetic stratigrap
hic model.