Radiocarbon, Volume 36, Number 1 (1994)
ABOUT THIS COLLECTION
Radiocarbon is the main international journal of record for research articles and date lists relevant to 14C and other radioisotopes and techniques used in archaeological, geophysical, oceanographic, and related dating.
This archive provides access to Radiocarbon Volumes 1-54 (1959-2012).
As of 2016, Radiocarbon is published by Cambridge University Press. The journal is published quarterly. Radiocarbon also publishes conference proceedings and monographs on topics related to fields of interest. Visit Cambridge Online for new Radiocarbon content and to submit manuscripts.
ISSN: 0033-8222
QUESTIONS?
Contact the University Libraries Journal Team with questions.
Recent Submissions
-
Radiocarbon, Volume 36, Number 1 (1993)Department of Geosciences, The University of Arizona, 1994-01-01
-
Radiocarbon DatesDepartment of Geosciences, The University of Arizona, 1994-01-01
-
Radiocarbon After Four Decades: An Interdisciplinary Perspective [Announcement]Department of Geosciences, The University of Arizona, 1994-01-01
-
Radiocarbon 1994 Price ListDepartment of Geosciences, The University of Arizona, 1994-01-01
-
LSC 92Department of Geosciences, The University of Arizona, 1994-01-01
-
Late Quaternary Chronology and Paleoclimates of the Eastern MediterraneanDepartment of Geosciences, The University of Arizona, 1994-01-01
-
Calibration 1993Department of Geosciences, The University of Arizona, 1994-01-01
-
Associate EditorsDepartment of Geosciences, The University of Arizona, 1994-01-01
-
Advances in Liquid Scintillation SpectometryDepartment of Geosciences, The University of Arizona, 1994-01-01
-
15th International Radiocarbon ConferenceDepartment of Geosciences, The University of Arizona, 1994-01-01
-
The Chronology of Coastal Morphogenesis and Human Settlement on Aitutaki, Southern Cook Islands, PolynesiaTwenty-seven 14C determinations from Aitutaki, southern Cook Islands inform on human settlement and Holocene coastal processes. I examine sedimentary, radiometric and archaeological data from Aitutaki with reference to regional evidence for a minor Holocene sea-level regression, which are in general agreement. Related processes of shoreline progradation and aggradation created near-shore environments conducive to human habitation, directly evidenced by ca. AD 900-1200. Nevertheless, biotic materials associated with this early cultural stratum suggest human colonization prior to this time. Archaeological preservation and recovery also may have been affected by changing sea level and related sedimentary processes.
-
Stratigraphic Division of Holocene Loess in ChinaLoess deposition within the Loess Plateau of China records the history of environmental change over the last 2.5 Myr. Loess-paleosol sequences of the last 10 ka, which have preserved information of global climate change, relate closely to human occupation of the area. Hence, studies of the deposition and development of Holocene loess are significant for studying environmental change and problems associated with engineering geology. We present here stratigraphic relations among four profiles from the south, west and center of the Loess Plateau. On the basis of 14C radiometric and AMS dates of organic material extracted from the paleosols, together with magnetic susceptibility measurements down each profile, we discuss Holocene stratigraphic divisions within the Loess Plateau, and suggest that the Holocene optimum, characterized by paleosol complexes, occurred between 10 and 5 ka BP. From 5 ka BP to the present, neoglacial activity is characterized by recently deposited loess.
-
Small Sample Dating in ChinaThe Xi'an Laboratory of Loess and Quaternary Geology has developed a small sample 14C dating facility consisting of a Wallac 1220 Quantulus(TM) liquid scintillation spectrometer, and a miniature benzene synthesis line based on the synthesis procedures used at the Australian National University (ANT). This line can produce ca. 0.3-ml benzene samples, which are then measured for 14C activity using 0.3-ml Teflon vials developed by Wallac Oy. The counting performance of the Quantulus(TM) spectrometer using 0.3-ml vials has been evaluated, and a potential age limit of ca. 45,000 BP has been obtained for samples containing up to 250 mg carbon. This dating facility fills the gap between large sample (2.4-6 g carbon) and microsample (<1 mg carbon) handling to form a 14C dating method sequence.