Edwards, R. L., G. S. Breschini, T. Haversat, and C. Simpson-Smith 2000
Archaeological Evaluation of Sites CA-MNT-798, CA-MNT-799 and CA-MNT-800, in the
Pfeiffer Beach Day Use Area, Big Sur, Monterey County, California. Archives of
California Prehistory No. 48. Coyote Press, Salinas, CA
CA-MNT-798.—This site was tested during the summer of 1994 by the Cabrillo College
Archaeological Field School, under the direction of Rob Edwards, and with the support
of the U.S. Forest Service. The discovery of a single glass bead (approximately 20 cm
below a Desert-Side-notched point) suggests an historic component for at least a
portion of the deposit. Radiocarbon dates agree with this, and suggest a Late Period
occupation as well.
MNT-798
190 ± 60 AD 1521 (mult) 1953 Beta-82143
310 ± 60 AD 1661 (1834) 1950 Beta-82141
330 ± 50 AD 1658 (1816) 1950 Beta-82142
440 ± 60 AD 1511 (1676) 1950 Beta-82140
Charcoal South face, 134-144 cm
Shell-Mytilus c. Unit A: 60-70 cm
Shell-Mytilus c. Unit A: 100-110 cm
Shell-Mytilus c. Unit A: 40-50 cm
Radiocarbon dates from:
Ethnography of the Esselen - by Gary S. Breschini and Trudy Haversat 2004 in
Ethnographic Overview of the Los Padres National Forest. Prepared for U.S.
Department of Agriculture Southern California Province Angeles National Forest
Arcadia, CA.
https://scvhistory.com/scvhistory/nlf_entradasouth_deir_app5-5.pdf accessed 3/9/2019
PLANT REMAINS FROM PFEIFFER BEACH (CA-MNT-798)
Charles H. Miksicek
BioSystems Analysis, Inc.
Santa Cruz, CA
Six flotation samples and two macrobotanical specimens were analyzed from the
Pfeiffer Beach site (CA-MNT-798) in the Big Sur area of central California. Even though
these samples contained only a relatively low density of charred plant remains, they
yielded an unexpectedly diverse mixture of taxa for what appears to be a small, limited
activity site.
METHODOLOGY
All of the flotation samples were processed using a continuous-flow flotation device
designed by this author which was modeled after the SMAP machine (Watson 1976).
Each soil sample was first measured in a large graduated cylinder to determine the
volume. The matrix was then poured into the float machine and gently stirred. Overflow
from the machine containing carbonized seeds and wood charcoal was collected in
nylon mesh with 0.25 mm openings. Sample processing continued until all charcoal was
collected in the nylon netting which was then hung from a clothesline and dried. The
remaining coarse sediments were then scanned for bone, lithics, and other artifactual
material.
After drying, each sample was first passed through a nested series of geological sieves
with mesh sizes of 4.0, 2.0, and 0.5 mm. This pre-sorting removes many modern
rootlets and produces subsamples with similar-sized particles which are more effectively
scanned by the analyst. Each fraction was then sorted at 7X under a binocular
dissecting microscope into its component parts. Uncharred seeds were counted and
identified to evaluate the modern seed rain and to provide a measure for the degree of
bioturbation and mixing within the soil column. To provide an additional monitor on the
amount of faunalturbation in each sample, rodent fecal pellets and insect parts were
quantified on a relative scale ranging from 0 (none) to 5 (abundant).
All pieces of charcoal large enough to manipulate were identified from each sample.
Each fragment was first fractured to give fresh transverse and radial sections and then
identified at 30x under a binocular dissecting microscope.
All seed and wood identifications were based on modern comparative material collected
from central California and standard seed and wood keys such as Musil (1963), Martin
and Barkley (1973), and Miles (1978). Taxonomic nomenclature follows Hickman
(1993). All botanical materials identified in the Pfeiffer Beach samples are listed in Table
@.1 along with ethnographic uses from Mead (1972) and seasonality data from
Hickman (1993).
Raw data are reported in Table @.2. This table includes sample volume before flotation,
richness (the average number of charred seed taxa per liter), density (the average
number of charred seeds per liter), the total weight of all charcoal fragments larger than
0.5 mm, the bug part index, the rat pellet index, uncharred seeds, carbonized plant
remains, and wood charcoal. It is most likely that all of the uncarbonized remains are
recent intrusives and are not associated with the prehistoric use of the site. Charred
seeds and non-woody plant parts are summarized in Table @.2 as ubiquities defined as
the percent of analyzed samples that contain a given taxon. Charcoal types are
summarized as relative percentages. Raw data are presented in a "structured table"
format (Van der Maarel, Janssen, and Louppen 1978). This is a semi-graphical method
of data presentation commonly used in European phytosociology (plant ecology). Plant
taxa are grouped by their order of appearance and the depth to which they persist in the
soil column. This method gives a quick visual impression of which categories of plant
remains co-occur which may not be evident from other data presentation formats.
RESULTS AND DISCUSSION
The discussion of the Pfeiffer Beach plant remains will be framed in terms of research
questions relevant to understanding prehistoric activities at the site.
How intact are the cultural deposits at CA-MNT-798?
Based on the archaeobotanical analysis, the Pfeiffer Beach deposits seem relatively
undisturbed. Only a few uncarbonized seeds (lupine, miner's lettuce, catchfly) are
present in the upper samples (above 104 cm, Table @.2). Intrusive insect parts or
uncharred rodent fecal pellets are not very common in the soil samples. Several
carbonized rodent fecal pellets are present in Lot 55, but these macrofossils often
suggest cooking small game or storing plant resources.
What charred plant remains are present in the Pfeiffer Beach samples?
Some carbonized seeds are present in all flotation samples, as are abundant fragments
of charcoal. The most common plant macrofossils are nuts (acorn, baynut, thinshelled
pine), but a few berries (manzanita, nightshade), spinach-like greens (clover,
goosefoot), and edible seeds (grasses, tarweed, goosefoot, buckwheat) are also
represented. Monocot rhizome (root) fragments, which may represent either a utilitarian
or food plant, are present in 67% of the analyzed samples. These fragments are too
small to identify with any greater degree of taxonomic specificity.
Acorn shell fragments are present in half of the float samples even though no oak wood
was identified in the charcoal assemblage. Acorns may have been brought to the site as
a stored food and not collected in the immediate vicinity of the site. Oak often accounts
for almost half of the charcoal assemblage of most central coast archaeological sites,
when acorns are identified with any degree of regularity (Miksicek 1992a, 1992b,
1993a). Even at Wilder Ranch, where no acorn macrofossils were identified, oak
charcoal accounted for 4% of the identified assemblage (redwood, pine, cypress, and
willow were overwhelmingly the dominant taxa, Miksicek 1992b).
Unknown vesicular material (present in four out of six samples) describes amorphous
plant material without diagnostic anatomical details (like vessel elements). It may
represent fragments of nutmeats, starchy roots, or a processed plant food like
seedcakes or gruel.
The nightshade seeds may represent either an edible berry, a medicinal herb, or a
utilitarian plant. Although a few species of Solanum have edible fruits (like the Old World
eggplants, the South American "tree tomato" or tomarillo, or the native local Solanum
douglasii) most species are quite toxic and would probably make a good fish poison.
Nightshade seeds were also identified from Wilder Ranch (CA-SCR-123, Table @.3 and
Miksicek 1993b), a site in a similar coastal setting.
Pine is the dominant charcoal type, accounting for 33% of the identified sample. Willow
(19%), cypress (14%), and shrubby members of the sunflower family (21%, like
coyotebrush) are also abundant. All of the woody taxa could be found in the immediate
vicinity of the site today or they could be collected from the beach as driftwood.
At what season of the year was the site utilized?
Two types of deposits were sampled for plant remains at CA-MNT-798. Lot 104 in Table
@.2 represents a possible hearth; a dense concentration of ash, charcoal, and other
cultural materials. The plant remains from this somewhat amorphous feature are more
likely to reflect a single use event or time period in the past. The other samples (Lots 53,
54, and 55) come from a stratigraphic column that brackets the time period represented
by Lot 104. Although more samples were collected and processed, only six samples
were analyzed because of time and budgetary constraints.
Lot 104 yielded all of the acorn, tarweed, baynut, hairgrass, and ryegrass macrofossils
identified from the site. If these remains represent fresh resources, collected locally,
then this deposit could have been produced between early summer and the middle of
fall (during the dry season). If these macrofossils represent stored and imported foods,
which is possible since oak is not present in the charcoal assemblage, then Lot 104
could represent a winter visit to the area.
The charred plant remains from Lots 53 through 55 seem to be more characteristic of
the types of plant resources that could be collected locally from early spring (clover,
tules, monocot roots) through middle summer (goosefoot seeds, nightshade and
manzanita berries). There just aren't any clear-cut botanical indicators for winter
occupation on the central coast of California, other than perhaps toyon or Christmas
berry (Heteromeles) which is found at higher elevations. In general, the CA-MNT-798
plant remains seem to suggest short-term visits at just about any time of the year, and
not a focused use of the locality at one particular season.
How do the archaeobotanical remains from Pfeiffer Beach compare to other sites in the
South-Central Coast Region of California?
Table @.3 summarizes data from ten other sites in the region. CA-MNT-229, with an
occupation from 2700 to 900 B.P., is on Monterey Bay, near Elkhorn Slough (Honeysett
1988). Wilder Ranch (CA-SCR-123) is a coastal midden site located just west of Santa
Cruz, with seven radiocarbon dates ranging from 3250 to 2200 B.P. (Miksicek 1993b).
CA-MNT-567 and 515 are Late Period habitation sites on Fort Hunter Liggett; CAMNT-540 may be a slightly earlier midden site in the same area (Miksicek 1992b). CAMNT-1486/H and 1485/H are two Late Period sites in the Carmel Valley (Miksicek
1992a). CA-SCL-690 (the Lick Site) is a large, Middle to Late Period cemetery in the
San Jose area (Miksicek, analysis in progress). CA-SCL-732/H is another large
cemetery site in the southern San Jose area (Miksicek 1993a). The "Gilroy sites"
include fourteen sites ranging in age from the Early to Late Periods (Hildebrandt and
Mikkelsen (1993).
Intuitively we would expect the Pfeiffer Beach assemblage to be most like Elkhorn
Slough or Wilder Ranch, the two coastal sites, but both are much larger midden sites.
Although more taxa were identified from Wilder Ranch overall, the MNT-798 samples
have slightly higher average density and richness values (2.70 and 1.56 respectively for
Pfeiffer, 1.33 and 0.74 for Wilder). We should keep in mind however that the Wilder
values may be reduced somewhat by the greater age of the samples and the larger
analyzed soil volumes (eight versus three to four liters). Nevertheless acorns were not
identified from either Wilder Ranch or Elkhorn Slough, even though they do occur at
Pfeiffer Beach.
Two other small coastal sites have recently yielded charred plant remains, CA-SMA-134
and CA-MNT-1765 (Moro Cojo). These are not included in Table @.3 because too few
flotation samples were analyzed from both sites for reliable ubiquity calculations. A
single sample from a hearth at Moro Cojo yielded an unexpectedly diverse assemblage
(richness = 0.77, density = 2.22) with charred monocot rhizome fragments and native
barley, reedgrass, lupine, and tarweed seeds. Also present in the sample were fish
bones and scales, mussel shell, clamshell, and small animal bones. This feature, with
two calibrated radiocarbon dates with midpoints averaging around AD 1650, seems to
suggest a single event, late spring deposit (Miksicek 1994a). Two very small samples
(both around 0.5 liter) from CA-SMA-134 yielded only a few charred elderberry and
bentgrass seeds (richness and density both = 1.82), but they did contain abundant
shellfish, fish, and larger animal remains. The SMA-134 deposits yielded five calibrated
and marine reservoir corrected radiocarbon dates (both bone and shell) with midpoints
around AD 650 (Miksicek 1994b).
Including the two small sites mentioned above (SMA-134 and MNT-1765), Pfeiffer
Beach is the only reported coastal site with nut remains (acorn, pine, baynut), except
perhaps the possible gray pine from MNT-229 (Table @.3), which could actually be the
thinshell pine identified at MNT-798, since the macrofossils are only listed as "pine" by
Honeysett (1988). Pfeiffer Beach is also the only coastal site that may have been used
at various times of the year, the others seem to have been visited between early spring
and late summer.
Overall, 31% of the 48 economic plant taxa listed in Table @.3 are present at Pfeiffer
Beach. The presence of possible imported plant foods like acorns makes the Pfeiffer
Beach site look more like interior sites such as those found in the Gilroy area or
SCL-690, but MNT-798 has a much shorter and less intensive occupation. Most of the
common central coast plant taxa, those present in at least half of the sites listed in Table
@.3, are represented at MNT-798.
In general small, coastal, limited activity sites like Pfeiffer Beach, Moro Cojo, and
SMA-134 seem to be more than just shellfish gathering or fishing camps. Flotation
sample assemblages from these sites demonstrate that a full range of subsistence
related endeavors occurred at these sites including shellfish gathering, fishing, small
game and/or bird hunting, large mammal procurement, and even some plant gathering
and processing activities. At least at CA-MNT-798 some non-local plant resources could
have been imported to be used at that locality. These sites were probably never
occupied for very long at any one time, but they were visited repeatedly year after year.
At least Pfeiffer Beach may have been utilized at several different seasons.
Table @.1. Plant Taxa Identified from Pfeiffer Beach (CA-MNT-798).
Common Name
Scientific Name
Part
Use
Catchfly **
Lupine
Miner's Lettuce
Monocot Rhizome
Clover
Fescue Grass
Hairgrass
Ryegrass
Goosefoot
Nightshade
Tarweed
Wild Buckwheat
Tule
Manzanita
Oak
Baynut
Pine
Grass Stems
Buckthorn Family
Sunflower Family
Cypress
Redwood
Sycamore
Willow
Coralline Algae
Silene sp.
Lupinus sp.
Claytonia perfoliata
Monocotyledoneae
Trifolium sp.
Vulpia or Festuca
Deschampsia sp.
Elymus sp.
Chenopodium sp.
Solanum sp.
Madia or Hemizonia
Eriogonum sp.
Scirpus sp.
Arctostaphylos sp.
Quercus sp.
Umbellularia californica
Pinus sp.
Poaceae
Ceanothus or Rhamnus
Asteraceae
Cupressus sp.
Sequoia sempervirens
Platanus racemosa
Salix sp.
Bossiella or Corallina
u
u
u
m
s
s
s
s
s
s
s
s
s,m
s,w
s
s,w
s,w
m
w
w
w
w
w
w
m
G
G
R
G
S?
S
S
S,G
F?,M?
S
S,M
U,S?
F,M,W
N,U,W
N,M,W
N?,W
U
W
W
W
W
W
M,U,W
M?,U?
Season Indicated
spring
spring
late spring-summer
late spring-summer
late spring-summer
late spring-summer
summer
summer
summer
spring-fall
late summer-fall
fall
fall
fall
Key: ** - introduced species, u - uncarbonized seed s - carbonized seed, m - miscellaneous parts
w - wood charcoal, S - edible seeds, G - edible greens, F - edible fruit, N - edible nut, M - medicinal
U - utilitarian (fiber, basketry, etc.), W - wood, ? - possible use, R - edible root
Table @.2. Plant Remains from Pfeiffer Beach (CA-MNT-798).
Lot
53
54
55
104
Depth (cm) or Feature 94-104 104-114 114-124 Hearth
104
Hearth
104
Hearth
47
34-44
48
44-54
Sample Volume (L)
Rat Pellet Index
Bug Part Index
Charred Seeds/Liter
Charred Taxa/Liter
3.0
0
0
3.00
1.33
3.0
0
0
2.67
1.33
M
M
3.5
1
0
2.28
2.00
3.5
0
1
2.28
1.71
4.0
0
0
2.50
1.50
4.0
0
1
3.50
1.50
Site
Mean
2.70
1.56
Uncharred (Intrusive) Seeds:
Miner's Lettuce
Catchfly
Lupine
1
1
9
Carbonized Seeds (etc.):
Goosefoot
Nightshade
Tule Seed
Seed Fragments
Monocot Rhizome
Thinshell Pine
Vesicular Material
Fescue Grass
Wild Buckwheat
Manzanita
Clover
Acorn Shell
Tarweed
Baynut Shell
Hairgrass
Ryegrass
Tule Stem
Grass Stem
Charred Rat Pellet
Coralline Algae
1
1
1
1
1
1
2
Ubiquity
1
1
5
4
2
19
2
16.7
33.3
50.0
33.3
66.7
50.0
66.7
33.3
16.7
33.3
16.7
50.0
33.3
16.7
16.7
16.7
33.3
50.0
16.7
33.3
2.1
1.7
0.9
%
5
2
1
1
3
4
7
1
18.9
2.3
0.8
33.3
14.4
1.5
0.8
2.3
21.2
4.5
2
4
1
3
1
1
3
1
1
2
1
1
1
1
1
1
6
1
2
1
1
1
1
Wood Charcoal:
0.8
Willow
Sycamore
Baynut
Pine
Cypress
Redwood
Manzanita
Buckthorn Family
Sunflower Family
California Sage
11
1
3
5
1
1
1
4
0.3
7
0.3
3
15
5
1
13
10
1
1
1
9
1
3
Indeterminate Charcoal 3
1
2
1
2
2
1
4
2
2
1
3
5
8
3
Key: M - Macrobotanical Specimen
Table @.3. Comparative Data from the South-Central Coast Region (Ubiquity).
Site
MNT
229
SCR
123
MNT SCL
1486/H 690
Gilroy Gilroy SCL
MNT
Area Area 732/H 540
MNT
567
MNT
515
Period
Number of Samples
Volume (Liters)
Charred Taxa/Liter
Charred Seeds/Liter
M
11
2
3.21
15.58
EM
8
1-14
0.74
1.33
L
4
2-5
10.93
42.03
E-M
14
8-19
1.21
23.34
L
9
5-17
1.47
34.11
L
14
4
3.00
6.22
L
8
1-4
3.46
7.70
Sedge/Tule
Grass Family
Elderberry
Bedstraw
Tarweed
Borage
Clover
Ryegrass
Wild Buckwheat
Gray Pine
Farewell-to-Spring
Goosefoot
Miner's Lettuce
Fescue Grass
Chia
Roots/Tubers
Spanish Clover
Bentgrass-Type
Monocot Fibers
Reedgrass-Type
Bluegrass
Coralline Algae
Lupine
Coffee Berry
Coyote Tobacco
Hairgrass
Maygrass
Hazelnut
Deer Vetch
Manzanita
Native Barley
Nightshade
Acorns
Large Goosefoot
Needlegrass
Madrone
Bromegrass
Pigweed
Baynut
Peppergrass
Panic Grass
Filaree
Bulbs
Red Maids
Allscale
Wild Cucumber
Buckeye
cf. Eelgrass
9
82
45
18
54
9
18
73
9
18?
57
93
21
57
7
57
36
78
100
22
78
33
67
44
21
14
62
38
25
38
12
25
38
12
50
50
12
100
75
75
12
62
12
12
M-L
26
1-6
6.89
14.74
4
62
25
38
50
12
38
38
25
25
25
75
12
25
25
12
12
12
25
12
12
12
12
12
50
25
12
25
50
75
75
25
50
75
8
23
15
8
31
15
75
75
25
100
8
42
46
35
100
50
75
100
4
31
62
19
23
8
50
25
75
75
100
50
75
50
25
25
100
50
50
25
75
25
100
50
25
19
4
8
31
19
5
4
15
50
31
7
57
86
14
50
21
78
100
11
78
11
M-L
9
8
0.96
1.74
M-L?
8
4
0.59
2.47
11
22
22
22
11
11
44
11
11
11
22
78
11
44
36
12
100
12
25
38
11
48
50
50
44
43
22
44
100
100
14
14
14
33
11
22
44
67
25
7
19
36
33
23
8
4
4
64
78
86
28
14
62
25
25
38
28
28
21
17
21
43
14
50
14
50
43
57
7
50
21
93
86
50
14
50
22
44
28
14
57
21
33
11
7
Key: E - Early, M - Middle, L - Late, ? - Identified to genus only.
12
12
References
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