scholarly journals 7
Rethinking Polity Formation: A Gendered Perspective on Formative Period Household Development in the Pacific Coast Region of Guatemala

2008 ◽  
Vol 18 (1) ◽  
pp. 87-101 ◽  
Author(s):  
Ana S. Tejeda
Keyword(s):  
Pacific Coast ◽  
Formative Period ◽  
The Pacific ◽  
Coast Region

Soils of the Pacific Coast Region: LRRs A and C

2016 ◽  
pp. 77-100
Author(s):  
Susan Burlew Southard ◽  
Randal J. Southard ◽  
Scott Burns
Keyword(s):  
Pacific Coast ◽  
The Pacific ◽  
Coast Region

New Zealand exports: Pseudosphaeroma Chilton, 1909 (Isopoda: Sphaeromatidae), a Southern Hemisphere genus introduced to the Pacific coast of North America

Zootaxa ◽  
2008 ◽  
Vol 1908 (1) ◽  
pp. 51-56 ◽  
Author(s):  
NIEL L. BRUCE ◽  
REGINA WETZER
Keyword(s):  
New Zealand ◽  
North America ◽  
Southern Hemisphere ◽  
San Francisco ◽  
Coastal Waters ◽  
Pacific Coast ◽  
First Record ◽  
The Pacific ◽  
First Time ◽  
Coast Region

Collections made along the coast of California have revealed the presence of a species of Pseudosphaeroma Chilton, 1909, a genus common in New Zealand coastal waters. The genus is entirely Southern Hemisphere in distribution, and this record reports the introduction of a species of Pseudosphaeroma into the San Francisco and Central Coast region of California, the first reported occurrence of the genus as an invasive taxon, and the first record of the genus from the Northern Hemisphere. The genus is also recorded for the first time from the Galapagos and Argentina.

Late Pleistocene stratigraphy of south-central British Columbia

1978 ◽  
Vol 15 (6) ◽  
pp. 971-980 ◽  
Author(s):  
Robert J. Fulton ◽  
Geoffrey W. Smith
Keyword(s):  
British Columbia ◽  
North America ◽  
Great Lakes ◽  
Late Pleistocene ◽  
Pacific Coast ◽  
Coastal Regions ◽  
South Central ◽  
The Pacific ◽  
Valley Area ◽  
Coast Region

The late Pleistocene deposits of south-central British Columbia record two major glacial and two major nonglacial periods of deposition. The oldest recognized Pleistocene deposits, called Westwold Sediments, were deposited during a nonglacial interval more than 60 000 years ago. Little information is available on the climate of this period, but permafrost may have been present at one time during final stages of deposition of Westwold Sediments. The latter part of this nonglacial period is probably correlative with the early Wisconsin Substage of the Great Lakes – St. Lawrence Valley area. However, deposition of the Westwold Sediments may have begun during the Sangamon Interglacial.Okanagan Centre Drift is the name applied to sediments deposited during the glaciation that followed deposition of Westwold Sediments. Okanagan Centre Drift is known to be older than 43 800 years BP and probably is older than 51 000. It is considered to correlate with an early Wisconsin glacial period.Bessette Sediments were deposited during the last major nonglacial period, which in south-central British Columbia persisted from at least 43 800 years BP (possibly more than 51 000) to about 19 000 years BP. This episode corresponds to Olympia Interglaciation of the Pacific Coast region and the mid-Wisconsin Substage of the Great Lakes – St. Lawrence Valley area. During parts of Olympia Interglaciation the climate was probably as warm as the present-day climate in the interior of British Columbia. Information from coastal regions indicates that there may have been periods of cooler and moister climate.Kamloops Lake Drift was deposited during the last major glaciation of south-central British Columbia. Ice occupied lowland areas from approximately 19 000 to 10 000 years BP. This period corresponds approximately to the Fraser Glaciation of the Pacific Coast region and the late Wisconsin Substage of central and eastern parts of North America.

REDISTRIBUTION AND GROWTH OF THE CASPIAN TERN POPULATION IN THE PACIFIC COAST REGION OF NORTH AMERICA, 1981–2000

The Condor ◽  
10.1650/7508 ◽  
2004 ◽  
Vol 106 (4) ◽  
pp. 777 ◽  
Author(s):  
Robert M. Suryan ◽  
David P. Craig ◽  
Daniel D. Roby ◽  
Nathan D. Chelgren ◽  
Ken Collis ◽  
...  
Keyword(s):  
North America ◽  
Pacific Coast ◽  
The Pacific ◽  
Caspian Tern ◽  
Coast Region

Leishmania Braziliensis from the Pacific Coast Region of Colombia: Foci of Transmission, Clinical Spectrum and Isoenzyme Phenotypes

1986 ◽  
Vol 35 (4) ◽  
pp. 722-731 ◽  
Author(s):  
Kristen A. Weigle ◽  
A. D'Alessandro ◽  
Luis H. Moreno ◽  
Nancy G. Saravia ◽  
Matilde de DÁvalos
Keyword(s):  
Pacific Coast ◽  
Clinical Spectrum ◽  
Leishmania Braziliensis ◽  
The Pacific ◽  
Coast Region

Shell-Ornament Production in Ejutla

1993 ◽  
Vol 4 (1) ◽  
pp. 103-119 ◽  
Author(s):  
Gary M. Feinman ◽  
Linda M. Nicholas
Keyword(s):  
Pacific Coast ◽  
Formative Period ◽  
Recent Survey ◽  
The Pacific ◽  
Monte Alban ◽  
Marine Shell ◽  
Lowland Maya

AbstractFindings from recent survey and excavation projects in Ejutla, Oaxaca, enable a broader examination of marine shell use and exchange in ancient Mesoamerica. A variety of shell ornaments were manufactured from Pacific Coast species at the Ejutla site during the Terminal Formative/Early Classic periods. Comparisons of the Ejutla mollusc assemblage with shell ornaments found at other highland Oaxaca sites indicate shifts in the nature of shell-ornament manufacture and exchange during the Formative and Early Classic periods. These changes, in conjunction with other findings, signal shifting relationships late in the Formative period among Monte Albán, the Ejutla Valley, and the Pacific Coast. The recognized shifts in highland-lowland Oaxaca relations generally coincide with an expanded importance of Pacific Coast shell at Teotihuacan and in the Lowland Maya region.

Formative Period Obsidian Exchange along the Pacific Coast of Mesoamerica

Archaeometry ◽  
2014 ◽  
Vol 57 ◽  
pp. 54-73 ◽  
Author(s):  
C. E. Ebert ◽  
M. Dennison ◽  
K. G. Hirth ◽  
S. B. McClure ◽  
D. J. Kennett
Keyword(s):  
Pacific Coast ◽  
Formative Period ◽  
The Pacific
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