Baja California's pioneering prehistorian, William C. Massey
(1961a, 1966), propounded what has been termed the “layer cake” model for the
region’s past. Elaborating on similar ideas developed earlier by Malcolm J.
Rogers (1939, 1945) and Paul Kirchhoff (1942), Massey sketched a view of culture
history characterized by waves of migration and cultural diffusion entering the
peninsula through its northern continental gateway. Successive waves had penetrated
shorter distances to the south, overlaying progressively smaller portions of
the region. The image was in reality less culinary than geological, with the northern
areas, as they were encountered at the time of Spanish contact, being underlain
by earlier prehistoric cultural strata, while those same earlier strata still outcropped
on the ethnohistoric surface farther to the south.
Arguably, Massey's model was a legitimate first
approximation toward an explanation for Baja California's archaeological and
ethnohistoric records. The peninsula did receive waves of cultural diffusion and
perhaps migration that came south from mainland North America, and areas lying
farther down the peninsula were isolated from the effects of some of those
waves. However, several decades of archaeological investigations now require us
to adopt a more complex picture of the region's past.
Key elements in the "layer cake" model concern the
peninsula's extreme south. One of the sources for the idea that an older
stratum had survived in the south was the image of that area's people as being extremely
"primitive" in their lifeways at the time of colonial contact. The
main source for this idea was an entertaining but highly acerbic account written
by an eighteenth-century Jesuit missionary, Jakob Baegert (1952, 1982). Baegert
found little to praise in either Baja California or its inhabitants. However,
it's notable that Baegert's main experiences were not with the Pericú in the
Cape Region of the extreme south but with the Guaycura, living a little farther
north on the relatively sterile Magdalena Plains. He was also not observing Guaycura
lifeways as they had existed at the time of initial European contact; he knew
these people only after two centuries of intermittent contacts and after more
than a decade of incorporation within the local mission system.
The cultures of the extreme south were distinctive in some
details of their technology (Massey (1961a). Most notably, they had retained
the use of the atlatl and dart in place of or alongside the bow and arrow down
to early contact times (Massey 1961b; but see also Laylander 2007a). In general,
however, it's not clear that these cultures were more "primitive" or
more conservative than those elsewhere in Baja California or the Desert West.
Another apparent anomaly in the extreme south of Baja
California was the extremely long (hyperdolichocephalc) skull shape of people
represented in Cape Region burials. An early suggestion, which is still occasionally
heard, was that a population had reached the Cape Region directly from across
the Pacific (e.g., Rivet 1909). No persuasive evidence has ever been advanced
in support of this idea, and it appears unlikely to be true. The "layer
cake" model suggests instead that the anomaly reflected an extreme genetic
conservatism among an isolated remnant of the continent's first occupants (e.g.,
Rogers 1939:71; González-José et al. 2003). However, an alternative explanation
may be that it represented genetic drift or other mechanisms of localized
divergence arising from the region's relative isolation, rather than the conservation
of an early pattern.
Movements in prehistoric Baja California were not exclusively
unidirectional, leading south from the northern gateway. An alternative external
link has been plausibly suggested as bridging the central Gulf of California, across
the chain of the Midriff Islands that lie between the coasts of Sonora and Baja
California (Kowta 1984). Evidence for the prehistoric occupation of the islands
is now well-established, although the timing, character, extent, and direction
of trans-Gulf interactions are still not clearly known (Bowen 2009).
An element of north-to-south movement that was perhaps not
encompassed within the original "layer cake" model was a terminal
Pleistocene maritime or littoral migration down the Pacific shores. Early radiocarbon
dates from Isla Cedros, off the central peninsula's western coast, and from
Isla Espíritu Santo, in the southern Gulf, lend plausibility to the idea that
the region's first settlers may have had a maritime orientation (Des Lauriers
2010; Fujita 2010). Such coastal movements were probably not exclusively
north-to-south. If the initial settlers followed the coast south from Alta California,
it's likely that they reversed direction upon reaching Cabo San Lucas and continued
to follow the coast from south to north up the Gulf, at least as far as the
Midriff Islands, before they would have recognized the possibility of crossing
the Gulf eastward to Sonora (Bowen 2009:84).
A linguistic hypothesis that still enjoys support is that speakers
of the Cochimí, Kiliwa, Delta-California Yuman (Tipai and Cocopa), and Paipai languages
each entered the peninsula in a separate migration through the northern gateway
(Mixco 2006). However, a contrary scenario, which is at least equally plausible
according to the available evidence, is that the original homeland of the Cochimí
and Yuman linguistic families lay within the northern part of the peninsula,
and that south-to-north movements carried Yuman groups northward, out of the
peninsula, during the last 2,000 years of prehistory (Laylander 2010). The Pai
branch of Yuman, which is represented by two languages, the widely separated
Paipai in northern Baja California and Upland Yumans (Yavapai, Walapai, and
Havasupai) in western Arizona, is particularly intriguing. The Pai distribution
evidently attests to a very late migration, either southward into the
peninsula, or northward out of it, or in both directions from an intermediate
location in the Colorado River delta or on the shores of now-extinct Lake
Cahuilla (Laylander 2007b).
Goods moved in multiple directions both within and beyond
Baja California. The most readily traced material is obsidian, the volcanic
glass so highly valued for flaking into refined tools such as projectile
points. At least a dozen chemically distinct geological obsidian sources have
been identified along the eastern margins of the peninsula. Artifacts derived
from these sources are found in archaeological sites lying to the north of
their source locations, extending into southern Alta California, at least as
often as they're found at sites to the south of the sources (Laylander 2012;
Panich and Porcayo 2012). Pottery has generally been seen as representing one
of the final prehistoric waves of cultural diffusion from the north, reaching only
a short distance down the peninsula before Spanish contact. However, an alternative
hypothesis has been proposed, according to which the manufacturing of the brownware
pottery characteristic of the mountains and west coast was initiated in
northern Baja California and then spread north into southern Alta California
(Griset 1996:273).
In Massey's day, migration and diffusion loomed large as preferred
explanations of cultural patterning. In subsequent decades, archaeology in
general, and studies of Baja California's prehistory in particular, have tended
to give more credence to local innovation as an important mechanism of cultural
change. The peninsula's best known prehistoric remains, the life-size or large-than-life
Great Mural paintings of humans, deer, and other animals found in the rockshelters
of the central sierras, can't be explained as something copied from elsewhere;
they're evidently an original, local creation (e.g., Gutiérrez and Hyland
2002). The elaborate and diverse burial practices of the Cape Region are
evidently not explicable as holdovers from an initial colonization, but instead
represent a set of practices that evolved locally through time (see, for
example, Rosales-López et al. 2007). The social complexity of the
archaeologically documented maritime adaptations on Isla Cedros and Isla
Espíritu Santo, for instance, belie the image of cultural impoverishment,
simplicity, or conservatism in these remote areas (Des Lauriers 2010; Fujita
2010).
There's a lesson to be drawn from the layer cake model. Useful
as such a model may be as a first approximation, the real stories of the past are
almost certainly going to be much more complex, more multidimensional, more
regionally variegated, and more interesting.
Don Laylander
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