Initially, four sites were
sampled: Hole 1018A (36°59.300´N,
123°16.653´; 2478
meters below seafloor [mbsf]), Hole 1020C (41°0.051´N,
126°26.063´W; 3038
mbsf), Hole 1021B (39°5.248´N,
127°46.985´W; 4212
mbsf), and Hole 1022C (40°4.842´N,
125°20.558´W; 1926
mbsf) (Fig. 1; Table
1). Sample spacing ranged from one sample per core in Holes 1018A and
1021B to three samples per core in Holes 1020B and 1022C. Standard marine
pollen-processing procedures, including the addition of measured quantities of
an exotic tracer to determine pollen concentration (pollen grains/gram dry
weight sediment [gdws]), were preceded and succeeded by sieving through 7-µm
nylon monofilament screening (Heusser and Stock, 1984). Pollen types
representing 35
taxa were identified to the lowest taxonomic level possible; for example,
specific identification of Tsuga (T.
heterophylla
and T. mertensiana)
and familial identification of grasses (Gramineae), chenopods (Chenopodiaceae),
and composites (Compositae). Excluding the papillate thick-exined grains of S.
sempervirens
(coastal redwood) and inaperturate pollen of other genera in the Taxodiaceae,
Cupressaceae, and Taxaceae (Juniperus,
Torreya, Cupressus,
Libocedrus, Chamaecyparis, and
Thuja), taxa that cannot be satisfactorily separated using light
microscopy are here referred to as juniper-cypress. Other groups of pollen and
spores include herbs (Gramineae, Cyperaceae, and Compositae), chaparral (sclerophylous
shrubs such as Ceanothus,
Adenostoma, Rhus,
and other members of Anacardiaceae, Rhamnaceae, and Rosaceae), and ferns (Polypodiaceae).
For this initial survey,
100
pollen grains were identified in each of 327 samples from Sites 1018, 1020, and
1022. (Data files are available from the ODP Data Librarian.) Because pollen
concentrations in samples from ODP Hole 1021B were extremely low (ranging from
100 to 1000 gdws), pollen data from this hole are not discussed in this report.
Pollen percentages are based on the total number of pollen grains identified in
each sample. Percentages of fern spores (and other pteridophytes such as Lycopodium
spp. and Selaginella
selaginoides) are calculated on the total number of pollen grain and
spores identified in each sample.
Age control varies from the well-constrained chronologies provided by a combination of calcareous nannofossil, planktonic foraminifer, radiolarian, and diatom datums (Sites 1018 and 1020) and by paleomagnetic reversals (Site 1020) to estimated ages of ODP Hole 1022C (M. Lyle, pers. comm., 1998; Lyle et al., Chap. 32, this volume).