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

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