Dataset - B2FIND

Major oxides for tektites and for conglomerate clast of the Upper Eocene ejec...

Evidence for the Chesapeake Bay Crater as the source for New Jersey continental margin ejecta is provided by fine-grained tektites and coarse-grained unmelted ejecta. The Upper...

Chronostratigraphic summary for Middle Miocene through Pliocene dinoflagellat...

This dataset has no description

(Table 5) Stratigraphic distribution of dinocyst taxa in ODP Hole 150-905A

X = present, - = absent, R = reworked, ? = questionable occurrence.

(Table 6) Stratigraphic distribution of dinocyst taxa in ODP Hole 150-906A

X = present, - = absent.

(Table 4) Stratigraphic distribution of dinocyst taxa in ODP Hole 150-904A

X = present, - = absent.

(Table 3) Stratigraphic distribution of dinocyst taxa in ODP Hole 150-903C

X = present, - = absent.

(Table 2) Stratigraphic distribution of dinocyst taxa in ODP Hole 150-903A

X = present, - = absent.

(Table 1) Stratigraphic distribution of dinocyst taxa in ODP Site 150-902

X = present, - = absent.

(Table 1) Nannofossil biohorizons and their depth of occurrence in ODP Hole 1...

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(Figure 1) Calcareous nannofossil abundances in ODP Hole 150-905A

Species abundance: - = not present; r = very rare, R = rare, F = few, C = common, A = abundant, W = very abundant, and ( ) = redeposited. Nannofossil abundance is the number of...

(Table 3) Diatom abundances in ODP Hole 150-906A

Species abundance: A = abundnat, C = common, R = rare, -= absent.

(Table 2) Diatom abundances in ODP Hole 150-903A

Species abundance: A = abundnat, C = common, R = rare, -= absent.