Table 3. Eocene to lower Miocene Tofino Basin ichthyoliths also occurring in deep-sea strata (cores). An interpretation (based on lithologies and faunas) of approximate in situ Tofino Basin ichthyolith/sediment deposition or transport/reworking is indicated.
Ichthyolith subtype |
Ichthyolith subtype deep-sea strata occurrence |
Overlap occurrence |
Tofino Basin ichthyolith occurrence and deposition |
No. spec. |
triangle transverse line across Doyle et al., 1974 |
upper Paleocene to lower Miocene |
Oligocene, lower Miocene |
mainly Oligocene;
possibly lower Miocene; ~ in situ |
7 |
cf. rhombus kite Gupta, 1991 |
Eocene to Oligocene |
Oligocene |
Oligocene; in situ |
1 |
ogee lanceolate Tway et al., 1985 |
Eocene to middle Miocene |
Oligocene |
Oligocene; in situ |
3 |
triangle one canal above Doyle et al., 1974 |
Eocene to middle Miocene |
upper Eocene, Oligocene |
upper Eocene and
Oligocene; possibly lower Miocene; in situ |
5 |
triangle double flex Dunsworth et al., 1975 |
middle Eocene to middle Miocene |
upper Eocene, Oligocene |
upper Eocene and
Oligocene; possibly lower-middle Miocene; ~ in situ |
4 |
short side peaks differentiated margin Doyle et al., 1974 |
upper Eocene to middle Miocene |
upper Eocene, Oligocene |
upper Eocene and
Oligocene; in situ |
7 |
kite-shaped longitudinal line Doyle et al., 1974 |
Maastrichtian to Oligocene |
Upper Cretaceous to Oligocene |
lithologies indicate common reworked Cretaceous-Paleogene materials |
13 |
pointed and skirted Doyle et al., 1978 |
Cretaceous to lower Eocene; rare (reworked?): middle Eocene to lower Pliocene |
Cretaceous to lower Eocene |
lithologies indicate common reworked Cretaceous-Paleogene materials |
42 |