scholarly journals Eruption age of the Kutsugata lava flow, Rishiri Volcano, off northern Hokkaido, Japan, based on AMS 14C dating of charred fossil wood immediately beneath the lava flow

2008 ◽  
Vol 47 (5) ◽  
pp. 349-353 ◽  
Author(s):  
Takeyuki Ueki ◽  
Reisuke Kondo
Keyword(s):  
Lava Flow ◽  
Fossil Wood ◽  
14C Dating ◽  
Eruption Age ◽  
Ams 14C Dating

scholarly journals Re-examination of the eruption age of Aira-Tn Ash(AT) obtained from a piston core off Shikoku. Determined by AMS 14C dating of planktonic foraminifera.

1993 ◽  
Vol 99 (10) ◽  
pp. 787-798 ◽  
Author(s):  
Masafumi Murayama ◽  
Eiji Matsumoto ◽  
Toshio Nakamura ◽  
Makoto Okamura ◽  
Hisato Yasuda ◽  
...  
Keyword(s):  
Planktonic Foraminifera ◽  
14C Dating ◽  
Piston Core ◽  
Eruption Age ◽  
Ams 14C Dating

Dynamic of Tridacna spp. population variability in northern SCS over past 4500 years derived from AMS 14C dating

2020 ◽  
Vol 748 ◽  
pp. 141359
Author(s):  
Chengcheng Liu ◽  
Hong Yan ◽  
Haobai Fei ◽  
Ge Shi ◽  
Peng Cheng ◽  
...  
Keyword(s):  
Population Variability ◽  
14C Dating ◽  
Ams 14C Dating

scholarly journals The hardwater effect in AMS 14C dating of food crusts on pottery

2010 ◽  
Vol 268 (7-8) ◽  
pp. 995-998 ◽  
Author(s):  
Bente Philippsen ◽  
Henrik Kjeldsen ◽  
Sönke Hartz ◽  
Harm Paulsen ◽  
Ingo Clausen ◽  
...  
Keyword(s):  
14C Dating ◽  
Ams 14C Dating

U-Th vs. AMS 14C dating of shells from the Achenheim loess (Rhine Graben)

2005 ◽  
Vol 176 (3) ◽  
pp. 249-255 ◽  
Author(s):  
Christophe Innocent ◽  
Christine Flehoc ◽  
Francis Lemeille
Keyword(s):  
14C Dating ◽  
Average Value ◽  
Rhine Graben ◽  
Younger Age ◽  
Isochron Diagram ◽  
Dating Method ◽  
Thorium 232 ◽  
Ams 14C Dating ◽  
Good Agreement

Abstract Shells extracted from loess deposits at Achenheim (Rhine Graben) have been investigated for AMS 14C and for U-Th dating by the isochron method on single shells. The two chronometers provide results that are not in agreement : the obtained 14C date is 38 ka B.P. In contrast, U-Th results provide much older ages. The 238U/232Th –230Th/232Th isochron diagram gives an age of 69 kyr, whereas a slightly younger age of 64 kyr is derived from the other, 234U/232Th – 230Th/232Th, diagram. 234U/238U ratios have not been found to vary from a shell to another : the average value is 1.199, slightly higher than radioactive equilibrium. For both isochrons, the Y-axis intercept is slightly negative, which indicates that there is no evidence for a significant detrital component. Thorium 232 that is present in the shells is probably incorporated in the material. The negative intercepts suggest that the two ages have been probably “aged” resulting from a slight mobilisation of uranium. By constraining the Y-axis intercepts at 0, ages that are in good agreement from one to another, can be calculated at 60.9 kyr and 60.4 kyr, respectively. In both cases, the statistical quality of the alignment is only slightly deteriorated. Since U-Th ages are in agreement with stratigraphic data, in contrast to the 14C date, one may believe that they date the end of early diagenesis, with uranium trapping. In contrast, the AMS 14C date is either thought to reflect analytical limitations of AMS 14C dating for such type of material, or to date a younger geologic event. In this latter case, a possible hypothesis is that this event has triggered the slight opening of the 238U – 234U system. In any case, this study demonstrates once again that surface formations often tell such complex stories that only one single dating method cannot usually be sufficient to describe precisely these histories. Instead, informations derived from different independent chronometers have to be compared.

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