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Dive into the research topics where Hiroshi Shirahata is active.

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Featured researches published by Hiroshi Shirahata.


The New England Journal of Medicine | 1979

Skeletal concentrations of lead in ancient Peruvians.

Jonathon E. Ericson; Hiroshi Shirahata; Clair C. Patterson

The level of biologic lead (expressed as the ratio of atomic lead to atomic calcium) in bones of Peruvians buried 1600 years ago was found to be 3 x 10(-8), as compared to 2100 to 3500 x 10(-8) in the bones of present-day residents of England and the United States. The ratio of barium to calcium was 2 to 3 x 10(-6) in bones of ancient Peruvians and present-day Americans. Barium and lead have similar morphologic distributions in organisms, so this discrepancy for lead must result from overexposure of present-day people to industrial lead and not from natural variations. The magnitude of this discrepancy has been confirmed by two different lines of investigation not reported in this article. This new evidence suggests that natural interactions of lead in human cells have not yet been determined because reagents, nutrients and controls used in laboratory and field studies have been contaminated with lead far in excess of naturally occurring levels.


Science of The Total Environment | 1991

Natural skeletal levels of lead in Homo sapiens sapiens uncontaminated by technological lead

Clair C. Patterson; Jonathon E. Ericson; Mirela Manea-Krichten; Hiroshi Shirahata

Lead, Ba and Ca concentrations were determined in tooth enamel, femur and rib from buried skeletons of PreColumbian Southwest American Indians, 10 subjects who lived 1000 years ago on the Pacific coast at 34 degrees N, and 13 subjects who lived 700 years ago in a desert valley tributary of the Colorado River at 37 degrees N 111 degrees W, both groups living in environments uncontaminated by technological Pb. For the coastal tribe, average Pb/Ca ratios were 1.1 x 10(-7) in enamel, 2.3 x 10(-7) in femur and 4.7 x 10(-7) in rib, while Ba/Ca ratios were 1.2 x 10(-5) in enamel, 32 x 10(-5) in femur and 38 x 10(-5) in rib (wt ratios). For the desert tribe, average Pb/Ca ratios were 4 x 10(-7) in enamel, 11 x 10(-7) in femur and 37 x 10(-7) in rib, while Ba/Ca ratios were 1.1 x 10(-5) in enamel, 7.5 x 10(-5) in femur and 6.2 x 10(-5) in rib. It is shown that biologic levels of Pb and Ba in buried femur and rib at both burial sites and in buried enamel at the Arizona site are obscured by excessive diagenetic additions of Pb and Ba from soil moisture. It is shown that one-third of the Pb in enamel at the Malibu site is biologic, yielding a skeletal Pb/Ca (wt) ratio of 4 x 10(-8). This is equivalent to a mean skeletal concentration of 13 ng Pb g-1 bone ash, and a mean natural body burden of 40 micrograms Pb/70 kg adult Homo sapiens sapiens, uncontaminated by technological Pb. This value is about one-thousandth of the mean body burden of 40 mg industrial Pb/70 kg adult American today, which indicates the probable existence within most Americans of dysfunctions caused by poisoning from chronic, excessive overexposures to industrial Pb.


Science of The Total Environment | 1987

Lead in ancient human bones and its relevance to historical developments of social problems with lead

Clair C. Patterson; Hiroshi Shirahata; Jonathon E. Ericson

Concentrations of metabolic lead in buried ancient bones are obscured by replacement of calcium in apatite by excessive amounts of soil moisture Pb. Concentrations of metabolic barium in bones are affected in a similar way. Added soil Pb and Ba, expressed as log(Pb/Ca) versus log(Ba/Ca) among various bones at a given burial site, are positively covariant, with about 5-fold more soil Pb added for each unit of added soil Ba. The typical natural metabolic Ba/Ca ratio in contemporary people can be measured unambiguously because it as unaffected by industrial pollution. It applies to ancient people because it has not changed historically. The intercept of the covariance curve for buried bones of a given ancient population at the known metabolic Ba/Ca ratio indexes the corresponding metabolic Pb/Ca ratio in bones of that population. Lead levels which prevailed in Romans appear to have been similar to those in contemporary people, which are approximately 1000-fold above natural levels in humans determined by this method in ancient Peruvians. This indicates that studies of natural biochemical reactions in cells free of industrial Pb should be made, because most present biochemical knowledge is founded on data obtained from systems polluted with Pb 1000 to 100000-fold above natural levels. The 5000 year history of smelting Pb by humans indicates that a system of education fostered by genetically common lower brain center functions operated on hundreds of successive generations in a context of cultural changes invoked by feedback from developments in engineering technologies to give rise to the difference between present typical and prehistoric natural levels of Pb in humans. Archaeological and anthropological studies of early developments in writing, music and metallurgy by ancient Peruvians and Persian peoples should be combined with PET-scan studies of their descendants to discover if, as preliminary archaeological data suggest, the two ancient populations differed on a genetic basis in higher brain functions, yet are indistinguishable as metallurgical engineers. This would demonstrate that higher centers of the human brain did not exercise guiding control, through hundreds of generations, over those developments of engineering technologies which resulted in the extreme pollution of the earths biosphere with poisonous Pb.


The Journal of the Japanese Association of Mineralogists,Petrologists and Economic Geologists | 1985

Variation in the concentrations of trace metals Ba, Sr, Li and Rb in granodiorite from southwestern Hokkaido during chemical weathering

Hiroshi Shirahata; Tetsuo Suzuki


The Journal of the Japanese Association of Mineralogists,Petrologists and Economic Geologists | 1965

Geochemical studies of the granitic rocks from southwestern Hokkaido, Japan.

Humio Sato; Hiroshi Shirahata


The Journal of the Japanese Association of Mineralogists,Petrologists and Economic Geologists | 1982

Lead isotopic composition in the geochemical

Hiroshi Shirahata


室蘭工業大学研究報告. 理工編 = Memoirs of the Muroran Institute of Technology. Science and engineering | 1976

Weathering on granitic rocks in Imagane, Hokkaido

Hiroshi Shirahata; Tetsuo Suzuki


Journal of Japan Society of Air Pollution | 1994

The Relationship of Concentrations of the Major Ion in Rain and Snow Deposition to Meteorological Factors

Hiroaki Oura; Hiroshi Shirahata


Shigen-Chishitsu | 1993

Strontium Isotopic Composition in Barite from the Minamishiraoi Kuroko-type Deposit, Southwestern Hokkaido

Tetsuro Yoneda; Song Yin; Hiroshi Shirahata


Journal of the Japan Society of Engineering Geology | 1987

Relationship between Rock Alteration and Landslides in the Noboribetsu District, Southwest Hokkaido

Hiroshi Shirahata; Hideyasu Asahi; Hiroaki Oura

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Clair C. Patterson

California Institute of Technology

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Hiroaki Oura

Muroran Institute of Technology

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Hideyasu Asahi

Muroran Institute of Technology

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Song Yin

Muroran Institute of Technology

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