Urey: to measure the absolute age of mars

Author(s):  
J. Randolph ◽  
J. Plescia ◽  
Y. Bar-Cohen ◽  
P. Bartlett ◽  
D. Bickler ◽  
...  
Keyword(s):  
2020 ◽  
Vol 10 (1) ◽  
Author(s):  
Sergi Trias-Llimós ◽  
Lisa Pennells ◽  
Aage Tverdal ◽  
Alexander V. Kudryavtsev ◽  
Sofia Malyutina ◽  
...  

AbstractSurprisingly few attempts have been made to quantify the simultaneous contribution of well-established risk factors to CVD mortality differences between countries. We aimed to develop and critically appraise an approach to doing so, applying it to the substantial CVD mortality gap between Russia and Norway using survey data in three cities and mortality risks from the Emerging Risk Factor Collaboration. We estimated the absolute and relative differences in CVD mortality at ages 40–69 years between countries attributable to the risk factors, under the counterfactual that the age- and sex-specific risk factor profile in Russia was as in Norway, and vice-versa. Under the counterfactual that Russia had the Norwegian risk factor profile, the absolute age-standardized CVD mortality gap would decline by 33.3% (95% CI 25.1–40.1) among men and 22.1% (10.4–31.3) among women. In relative terms, the mortality rate ratio (Russia/Norway) would decline from 9–10 to 7–8. Under the counterfactual that Norway had the Russian risk factor profile, the mortality gap reduced less. Well-established CVD risk factors account for a third of the male and around a quarter of the female CVD mortality gap between Russia and Norway. However, these estimates are based on widely held epidemiological assumptions that deserve further scrutiny.


2016 ◽  
Vol 463 ◽  
pp. 126-135 ◽  
Author(s):  
Ivar Midtkandal ◽  
Henrik H. Svensen ◽  
Sverre Planke ◽  
Fernando Corfu ◽  
Stephane Polteau ◽  
...  

2019 ◽  
pp. 89-118
Author(s):  
Jae Youn Kim

Misongri site is the oldest relic in the currently known Amrok River basin, and can be compared with the lower layer of Xiaozhushan culture. The period of this remains was studied to be the same as that of lower layer of Xiaozhushan culture in the southern part of the Liaodong Peninsula, due to the zigzag pattern pottery. However, as the ruins of Suzhou have been re-excavated recently, the absolute age of Xiaozhushan culture and the contents of middle layer of Xiaozhushan culture have also changed. Based on the measurement date, the age of the lower layer of Xiaozhushan culture is between 6700 and 6300 years ago, and middle layer of Xiaozhushan culture is between 5500 and 5300 years ago. In comparison with Misongri site, only the culture of the lower layer of Xiaozhushan were compared. But, compared to the newly known data, it can be divided into the first stage of Misongri site and the second stage of Misongri site. It can be seen as the ruins of the same period as the lower layer of Xiaozhushan culture and the Xiaozhushan middle-layer culture. In addition, the earthenware of the first phase of Misongri site is confirmed in the lower Houwa culture of the northern part of the Liaodong area and the lower layer of Xiaozhushan in the south of the Liaodong peninsula. To the Amrok River culture area. The first stage of the Amrok River cultural Area is between 6700 and 6300 years ago, and the west is the northern part of the Liaodong to the southern part of the Liaodong Peninsula. The second stage of the Amrok River Cultural Zone is between 5500-5300 years ago. The western range extends from the northern part of the Liaodong to the southern part of Liaodong and the basin of the Taizhe River.


1971 ◽  
Vol 37 (2) ◽  
pp. 15-33 ◽  
Author(s):  
H. T. Waterbolk

C-14 datings can not only provide us with estimates of the absolute age of objects or occupation layers, but also, when available in sufficient numbers, with initial and terminal datings for cultural phases, thus defining their duration. The value of this is obvious: differential duration in different areas can at last provide definitive answers to long-disputed questions concerning the direction of cultural movement.Working with large numbers of C-14 dates is, however, not entirely free of problems. We are, for example, regularly confronted with larger differences between datings expected to be of similar age than can be accounted for by mere statistical error (Vogel, 1969a) or which can be explained by contamination or other simple causes. One can stop at this point and accept a limited testimonial value for C-14 dates (e.g. Steuer and Tempel, 1968), or one can try to go further by calculating average dates, assuming (for the most part incorrectly) that the chance of a date being too young is equal to its chance of being too old (Neustupný, 1968). The danger in this procedure is that one loses sight of the individual character of each determination: in fact one sample is much more securely associated and more closely contemporary with finds of a particular cultural phase than another, and the chance of contamination or admixture is different for each sample.Another problem is that the number of C-14 dates that one must take into consideration is often so large that they cannot be digested without some form of graphic presentation, and for this there is as yet no uniformity of practice.


2015 ◽  
Vol 812 (1) ◽  
pp. 25 ◽  
Author(s):  
M. Monelli ◽  
V. Testa ◽  
G. Bono ◽  
I. Ferraro ◽  
G. Iannicola ◽  
...  

1990 ◽  
Vol 98 (2) ◽  
pp. 282-285 ◽  
Author(s):  
Mary K. Roden ◽  
Randall R. Parrish ◽  
Donald S. Miller
Keyword(s):  

Radiocarbon ◽  
1980 ◽  
Vol 22 (2) ◽  
pp. 545-555 ◽  
Author(s):  
Jacques Evin ◽  
Joëlle Marechal ◽  
Christiane Pachiaudi ◽  
J J Puissegur

Mollusks living only on ground surface can be expected to give the most reliable results in 14C dating from carbonates of continental origin. One may assume they have a homogeneous biotope and are not affected by any hard-water effect. In order to verify these assumptions and to test shells as routine dating material, results from terrestrial gastropods are compared with other 14C dates from classic biologic material, such as peat, charcoal, or bone, collected in the same archaeologic or geologic levels in miscellaneous places. Two sites were selected for which other chronologic data, such as prehistoric industries or malacologic diagrams were available.All results indicate older values for 14C shell dates. The discrepancy between “normal” and snail dates amounts to 300 to 1200 14C years and remains the same whatever the absolute age of the sample. All 13C values of perfectly cleaned shells are between —5 to —10%, versus PDB. The initial 14C content of shells that is too low may be different according to species, as suggested by 13C variations.Although fairly constant, this deviation of 14C ages generally makes such samples unreliable for most archaeologic studies, which often need more precise results. However, some measurements were performed on microfauna shells from several Würmian loess to show that dating of shells may be useful in fairly ancient geologic sediments for lack of better carbonaceous samples. Good agreement of some snail dates with expected sediment ages point to the importance of proper sample selection and pretreatment that might be checked by 13C measurements.


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