Uranium isotope ratios of Muonionalusta troilite and complications for the absolute age of the IVA iron meteorite core

2018 ◽  
Vol 490 ◽  
pp. 1-10 ◽  
Author(s):  
Gregory A. Brennecka ◽  
Yuri Amelin ◽  
Thorsten Kleine
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.


Author(s):  
J. Randolph ◽  
J. Plescia ◽  
Y. Bar-Cohen ◽  
P. Bartlett ◽  
D. Bickler ◽  
...  
Keyword(s):  

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.


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