δ13C values and radiocarbon dates of microbial biomarkers as tracers for carbon recycling in peat deposits

Geology ◽  
2000 ◽  
Vol 28 (7) ◽  
pp. 663 ◽  
Author(s):  
Richard D. Pancost ◽  
Bas van Geel ◽  
Marianne Baas ◽  
Jaap S. Sinninghe Damsté
Geology ◽  
2000 ◽  
Vol 28 (7) ◽  
pp. 663-666 ◽  
Author(s):  
Richard D. Pancost ◽  
Bas van Geel ◽  
Marianne Baas ◽  
Jaap S. Sinninghe Damsté

1987 ◽  
Vol 67 (2) ◽  
pp. 221-247 ◽  
Author(s):  
K. W. G. VALENTINE ◽  
C. TARNOCAI ◽  
C. R. DE KIMPE ◽  
R. H. KING ◽  
J. F. DORMAAR ◽  
...  

This review describes some aspects of Canadian soils that are relevant to the Quaternary. It includes a description of the Quaternary Period in Canada, including a chronology of the major events that influenced soil formation, and the implication of the Quaternary to Canadian soils. The contribution of relict and buried paleosols to Quaternary stratigraphy and the reconstruction of paleoenvironments is then discussed, including some of the inherent problems. Pedologic evidence of environmental change in the southern Rocky Mountains, including tephrostratigraphy, is followed by a description, with numerous radiocarbon dates, of Holocene peat deposits. The review concludes with a discussion of weathering and saprolites in eastern Canada. Key words: Quaternary, Holocene, paleosols, stratigraphy, paleoenvironments, peat


Radiocarbon ◽  
2007 ◽  
Vol 49 (2) ◽  
pp. 357-367 ◽  
Author(s):  
Maarten Blaauw ◽  
Ronald Bakker ◽  
J Andres Christen ◽  
Valerie A Hall ◽  
Johannes van der Plicht

Recently, Bayesian statistical software has been developed for age-depth modeling (“wiggle-match dating”) of sequences of densely spaced radiocarbon dates from peat cores. The method is described in non-statistical terms, and is compared with an alternative method of chronological ordering of 14C dates. Case studies include the dating of the start of agriculture in the northeastern part of the Netherlands, and of a possible Hekla-3 tephra layer in the same country. We discuss future enhancements in Bayesian age modeling.


Radiocarbon ◽  
2001 ◽  
Vol 43 (2B) ◽  
pp. 527-540 ◽  
Author(s):  
Yurij K Vasil'chuk ◽  
Högne Jungner ◽  
Alla C Vasil'chuk

We present new radiocarbon dates from a number of Holocene peat deposits along a north-south transect across the Yamal Peninsula. The samples were collected from frozen peat deposits with large ice wedges in: the northern tundra near Seyaha Settlement, in the Central Yamal Peninsula, the southern tundra in Shchuch'ya River valley at the Edem'yaha mouth, the southern part of the Yamal Peninsula, and the southern forest tundra near Labytnangi Town. 14C dates of wood remains from the tundra in the Yamal Peninsula could be used to reconstruct a northern limit of forest during the Holocene Optimum. The wood layers at the bottom of the peat give evidence for immigration of trees further north beyond the present boundary. The first forest appearance in the Seyaha River valley area is dated about 9 ka BP according to the oldest peat date in the Seyaha cross section. This suggests that summer temperatures were higher than at present. Very fast accumulation of peat (around 5 m/ka: about 9–8 ka BP at Seyaha and about 7–6 ka BP at Shchuch'ya) also supports this observation.In contrast, oxygen isotope composition of Holocene syngenetic ice wedges from the area (δ18O= −19.1 to −20.3‰ in the Seyaha cross-section and −17.3 to −20.3‰ in the Shchuch'ya River) show that winter temperatures were significantly lower than presently, i.e. the climate during the Holocene Optimum was slightly more continental. The frozen peat near Labytnangi has thawed during the last 20 years, indicating global warming.


2012 ◽  
Vol 77 (1) ◽  
pp. 205-210 ◽  
Author(s):  
Torben C. Rick ◽  
Gregory A. Henkes ◽  
Darrin L. Lowery ◽  
Steven M. Colman ◽  
Brendan J. Culleton

Radiocarbon dates from known age, pre-bomb eastern oyster (Crassostrea virginica) shells provide local marine reservoir corrections (ΔR) for Chesapeake Bay and the Middle Atlantic coastal area of eastern North America. These data suggest subregional variability in ΔR, ranging from 148±46 14C yr on the Potomac River to −109±38 14C yr at Swan Point, Maryland. The ΔR weighted mean for the Chesapeake's Western Shore (129±22 14C yr) is substantially higher than the Eastern Shore (−88±23 14C yr), with outer Atlantic Coast samples falling between these values (106±46 and 2±46 14C yr). These differences may result from a combination of factors, including 14C-depleted freshwater that enters the bay from some if its drainages, 14C-depleted seawater that enters the bay at its mouth, and/or biological carbon recycling. We advocate using different subregional ΔR corrections when calibrating 14C dates on aquatic specimens from the Chesapeake Bay and coastal Middle Atlantic region of North America.


2007 ◽  
Vol 29 (2) ◽  
pp. 113-154
Author(s):  
ALAN LESLIE ◽  
GAVIN MACGREGOR ◽  
PAUL R. J. DUFFY ◽  
J. S. DUNCAN ◽  
J. MILLER ◽  
...  

Excavation by GUARD in 1999 on the southern defences of Balmuildy Roman fort exposed small sections of three ditches: two to the W of the S gate of the fort, one to the E. All were found in locations consistent with Miller's 1922 excavation plan of the site, though, contrary to expectations, none of these features appeared to have been previously excavated. The limited investigations produced no information which would substantially alter our understanding of the chronological context or occupational history of the Roman fort, though the undisturbed character of the evidence was surprising. The waterlogged conditions in the innermost ditch to the W of the S gate preserved organic material within the fill, and it was considered worthwhile attempting to study the environmental material in some detail, presenting as it did an opportunity to provide some stratigraphically secure evidence for the fort's contemporary environment with the original excavation report, which – in common with others of its time – largely ignored this type of evidence. The terminal of the middle ditch to the W of the S gate produced pottery of Antonine date from the primary fill. Two radiocarbon dates were also obtained from the fill of the inner ditch: one, of 37 BC-AD 217, was derived from early in the sequence of ditch fills, while a second, of AD 439–661, was obtained from a later, charcoal-rich layer sealing accumulated peat deposits.


Radiocarbon ◽  
1983 ◽  
Vol 25 (2) ◽  
pp. 381-391 ◽  
Author(s):  
C V Haynes ◽  
Minze Stuiver ◽  
Herbert Haas ◽  
J E King ◽  
F B King ◽  
...  

From 1966 to 1979, the University of Missouri, the University of Arizona, and the Illinois State Museum conducted extensive interdisciplinary investigations of Late Pleistocene peat deposits associated with springs, some extinct, in the Pomme de Terre River Valley of the Ozark Highland, Missouri (fig 1). Most of the sites are now beneath the waters of the Harry S Truman reservoir. Archaeologic investigations in the area produced a remarkably long sequence of cultural change and development during the Holocene but produced no evidence of human presence in the area prior to 11,000 years ago despite diligent excavation of favorable bone-bearing deposits.


Radiocarbon ◽  
1970 ◽  
Vol 12 (1) ◽  
pp. 130-155 ◽  
Author(s):  
P. M. Dolukhanov ◽  
Ye. N. Romanova ◽  
A. A. Semyontsov

The present list covers samples measured between 1963 and July, 1967. Three previous lists have been published in Leningrad I (Sovetskaya arkheologiya, 1961, p. 3); Leningrad II (The Absolute Geochronology of the Quaternary Period, 1963); and Leningrad III (New Methods in Archaeological Investigations, 1963, p. 9–56). The samples measured include charcoal from cultural layers and hearths, wood from barrows [kurgans] and cemeteries, wooden tools from peat deposits, and mounds, as well as peat and animal tissue.


2002 ◽  
Vol 68 ◽  
pp. 185-213 ◽  
Author(s):  
A.D. Crockett ◽  
Michael J. Allen ◽  
Robert G. Scaife

Excavations at Fort Street, Silvertown, London revealed a short length of a prehistoric trackway constructed within the floodplain of the Thames. Two pollen profiles were obtained through peat together with four radiocarbon dates; two from the trackway itself, one from near the bottom and one from near the top of the peat. These dates indicate that the trackway was constructed in the Early Neolithic and that peat formation took place in the Neolithic and Bronze Ages. The trackway is of considerable importance in that it represents the earliest known structure of this kind yet discovered in the London area.


Radiocarbon ◽  
2017 ◽  
Vol 59 (6) ◽  
pp. 1771-1778 ◽  
Author(s):  
Mitsuru Okuno ◽  
Pavel Izbekov ◽  
Kirsten P Nicolaysen ◽  
Eiichi Sato ◽  
Toshio Nakamura ◽  
...  

ABSTRACTWe obtained radiocarbon (14C) dates with accelerator mass spectrometry (AMS) of vascular plant samples and a charcoal sample collected from peat deposits near the prehistoric village site informally designated CR-03 on Carlisle Island in the Islands of Four Mountains group, Alaska, to determine the eruption age of the CR-02 tephra. A fine vitric ash erupted from Okmok caldera, Umnak Island (ca. 2 ka BP) was also discovered in the bog. The ages of the CR-02 tephra and Okmok II ash are estimated to be 1050 and 2000 cal BP, respectively. Because both tephras are distinctive and widespread, these are important chronostratigraphic markers for archaeological sites in this island group. The 14C dates obtained from this bog are 800 years younger than the dates of the charcoal fragments from cultural layers in the Unit 3 of prehistoric village site CR-02 (AMK-0003).


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