Holocene floodplain lake sediments in the Amazon: 14C dating and palaeoecological use

1991 ◽  
Vol 10 (4) ◽  
pp. 363-372 ◽  
Author(s):  
Matti E. Räsänen ◽  
Jukka S. Salo ◽  
Högne Jungner
Radiocarbon ◽  
1992 ◽  
Vol 34 (3) ◽  
pp. 557-560 ◽  
Author(s):  
Austin Long ◽  
Owen K. Davis ◽  
Jeanne de Lanois

We have developed and tested a practical device for manually separating pollen from pollen concentrates in sufficient quantity for AMS 14C dating. It is a combination of standard, commercially available equipment handled in a clean room by an individual trained to recognize pollen. A typical example requires about 15–20 h of hand-picking under the microscope. We show the usefulness of this procedure with results on a mid-Holocene segment from a core from Mono Lake. Sediments from this hardwater lake contain pollen and finely disseminated organic matter, but no macrofossils. The pollen dated ca. 1000 yr younger than the bulk sediment. The sediment “date” is most likely affected by incorporation of limestone-derived carbon, and is erroneously old.


2002 ◽  
Vol 13 (1) ◽  
pp. 71-77 ◽  
Author(s):  
José M. Godoy ◽  
Carlos R. Padovani ◽  
Jean R. D. Guimarães ◽  
José C. A. Pereira ◽  
Luis M. Vieira ◽  
...  

The Holocene ◽  
1993 ◽  
Vol 3 (2) ◽  
pp. 161-163 ◽  
Author(s):  
V.J. Jones ◽  
R.W. Battarbee ◽  
R.E.M. Hedges

2002 ◽  
Vol 21 (10) ◽  
pp. 2165-2171 ◽  
Author(s):  
Elske M. De Haas ◽  
Bas Reuvers ◽  
Caroline T. A. Moermond ◽  
Albert A. Koelmans ◽  
Michiel H. S. Kraak

2015 ◽  
Vol 42 (1) ◽  
Author(s):  
Alicja Bonk ◽  
Wojciech Tylmann ◽  
Tomasz Goslar ◽  
Agnieszka Wacnik ◽  
Martin Grosjean

Abstract Varved lake sediments from Lake Zabihskie (northeastern Poland) provide a high- resolution calendar-year chronology which allows validation of 14C dating results. Microscopic analy­sis of the varve microfacies revealed that laminations found in Lake Zabihskie were biogenic (calcite) varves. Three independent counts indicated a good preservation quality of laminae in the 348 cm long sediment profile which contained 1000+12/-24 varves. The varve chronology was validated with the 137Cs activity peaks, the tephra horizon from the Askja eruption at AD 1875 and with the timing of major land-use changes of known age inferred from pollen analysis. 32 AMS 14C dates of terrestrial macrofossils distributed along the profile were compared with the varve chronology. After identifica­tion of outliers, the free-shape model performed with 21 14C dates provided the best possible fit with the varve chronology. We observed almost ideal consistency between both chronologies from the present until AD 1250 while in the lower part (AD 1000-1250) the difference increases to ca. 25 years. We demonstrate that this offset can be explained by too old radiocarbon ages of plant remains trans­ported to the lake by the inflowing creek. Results of this study highlight that careful interpretation of radiocarbon age-depth models is necessary, especially in lakes where no annual laminations are ob­served and no independent method are used for cross-validation.


2005 ◽  
Vol 162 (2) ◽  
pp. 211-228 ◽  
Author(s):  
Elske M. de Haas ◽  
R. van Haaren ◽  
Albert A. Koelmans ◽  
Michiel H.S. Kraak ◽  
W. Admiraal

2012 ◽  
Vol 55 (10) ◽  
pp. 1669-1678 ◽  
Author(s):  
Yu Li ◽  
NaiAng Wang ◽  
ZhuoLun Li ◽  
ChengQi Zhang ◽  
XueHua Zhou

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