The Bruce collection of Eskimo material culture from Kotzebue Sound, Alaska / James W. VanStone.

n.s. no.1(1980)

The Bruce Collection of Eskimo material culture from Port Clarence, Alaska / James W. VanStone, Curator, North American Archaeology and Ethnology, Field Museum of Natural History.

v.67(1976)

The Isaac Cowie collection of Plains Cree material culture from Central Alberta / James W. VanStone.

n.s. no.17(1991)

The Nordenskièold collection of Eskimo material culture from Port Clarence, Alaska / James W. VanStone.

n.s. no.14(1990)

The Simms Collection of Plains Cree material culture from southeastern Saskatchewan / James W. VanStone, Curator, North American Archaeology and Ethnology, Dept. of Anthropology, Field Museum of Natural History.

n.s. no.6(1983)

The Speck collection of Montagnais material culture from the Lower St. Lawrence Drainage, Quebec / James W. VanStone, Curator, North American Archaeology and Ethnology, Field Museum of Natural History.

n.s. no.5(1982)

Descriptions of new Indian lepidopterous insects from the collection of the late Mr. W.S. Atkinson. Rhopalocera, by William C. Hewitson. Heterocera, by Frederic Moore. With an introductory notice by Arthur Grote.

1879

A collection of the most approved pieces of music from various authors: transcribed while member of Harvard University, from July 1789 to July 1793

John Pierce kept this journal while he was a student at Harvard College. It consists of manuscript musical scores with annotations indicating the occasions at which the music was performed. These occasions included commencements, public exhibitions and Dudleian lectures. A note indicates that one anthem was prepared by Samuel Holyoke at Pierce's request, to be performed at Pierce's class commencement exercises, held on July 13, 1793. Several annotations were made in May 1794, the year following Pierce's graduation. There is a table of contents on the last page.

(Tables 1, 3) Component composition of organic particles in samples from ODP Site 131-808

Analysis of the palynofacies and miospore thermal alteration indices (TAI) of sediments from ODP Site 808 in the Nankai Trough was undertaken to determine (1) the source, depositional environment, and diagenesis of organic matter in the accreted sediments, and (2) the thermal structure and history of the prism and its relationship to fluid flow. Using the Hartax classification system, two palynofacies were recognized in the sedimentary sequence. Facies 1 occurs within the upper 600 m of trench-wedge turbidites (sedimentation rate > 1 km/m.y.) and contains >50% inertite particles. The rest of the assemblage is dominated by well-preserved phytoclasts and contains small amounts of poorly preserved phytoclasts and well-preserved scleratoclasts. Facies 2 occurs within the Shikoku Basin hemipelagites (600-1300 m below seafloor; sedimentation rate <150 m/m.y.) and contains over two-thirds inertite particles. The rest of the assemblage is dominated by poorly preserved phytoclasts. Miospores and marine phytoplankton compose only a small percentage of both palynofacies. Degraded organic matter is most noticeable in Facies 2, whereas its presence in Facies 1 is overshadowed by the high influx of well-preserved primary organic matter. Most of the degraded organic matter and inertite is interpreted to be reworked. Some of the degraded organic matter may be primary, and may have experienced more biodegradation and thermal alteration in Facies 2 than in Facies 1. TAI values indicate an immature stage of organic maturation (< 2) down to about 900 mbsf. Below this, samples show an increase with depth to a mature stage, reaching peak levels of about 3 just above basement. Samples from within the thrust fault and decollement zones do not show levels of maturity significantly greater than those of surrounding samples, leaving uncertain whether hot fluids have migrated along these fault boundaries in the past.