scholarly journals Informing Conservation: Towards 14C Wiggle-Matching of Short Tree-Ring Sequences from Medieval Buildings in England

Radiocarbon ◽  
2016 ◽  
Vol 59 (3) ◽  
pp. 985-1007 ◽  
Author(s):  
A Bayliss ◽  
P Marshall ◽  
C Tyers ◽  
C Bronk Ramsey ◽  
G Cook ◽  
...  
Keyword(s):  
Tree Ring ◽  
Historic Buildings ◽  
Calibration Data ◽  
Medieval Period ◽  
Growth Rings ◽  
Comparable Level ◽  
Annual Growth Rings ◽  
Short Tree ◽  
Oak Tree ◽  
Calendar Dates

AbstractThis study tested whether accurate dating by accelerator mass spectrometry (AMS) radiocarbon wiggle-matching of short tree-ring series (~30 annual rings) in the Medieval period could be achieved. Scientific dating plays a central role in the conservation of historic buildings in England. Precise dating helps assess the significance of particular buildings or elements of their fabric, thus allowing us to make informed decisions about their repair and protection. Consequently, considerable weight, both financial and legal, can be attached to the precision and accuracy of this dating. Dendrochronology is the method of choice, but in a proportion of cases this is unable to provide calendar dates. Hence, we would like to be able to use 14C wiggle-matching to provide a comparable level of precision and reliability, particularly on shorter tree-ring sequences (~30 annual growth rings) that up until now would not routinely be sampled. We present the results of AMS wiggle-matching five oak tree-ring sequences, spanning the period covered by the vast majority of surviving Medieval buildings in England (about AD 1180–1540) when currently we have only decadal and bidecadal calibration data.

PERTUMBUHAN LINGKARAN POHON JATI PADA DUA SISTEM KULTUR BERBEDA DI JAWA TIMUR

2008 ◽  
Vol 6 (2) ◽  
Author(s):  
Iriwi Louisa S. Sinon
Keyword(s):  
Tree Ring ◽  
Tectona Grandis ◽  
Annual Growth ◽  
Natural Growth ◽  
Growth Rings ◽  
Climate Effect ◽  
Tropical Regions ◽  
Annual Growth Rings ◽  
Chronological Sequence ◽  
Plantation Teak

<p><em>Study dendrochronology or tree-ring dating is defined as the study of chronological sequence of annual growth rings in trees. Teak (Tectona grandis) is one of various tree species that has been identified for the use of tree-ring studies in tropical regions. Teak is found to be suitable for dendrochronology as it is long-lived and develops defined annual growth rings. In Java, teak cans growth naturally or intensively in plantation. The two silviculture conditions will give different sensitivity on climate effect. Therefore, the effect of silviculturer will on natural teak and plantation teak in Saradan, Madiun, and East Java. As a part of the study, ten core samples from natural- growth teak were measured. The samples of growth rings is spanned from 1832 – 2004. Using the COFECHA program, the correlation of the samples (r) was found to be 0.44 point, which is satisfactory to the standard used in dendrochronology. Thus, from this study it can be concluded that natural teak could still be used in dendrochronology, although the sensitivity are not as high as plantation teak. </em></p>

A New Annual 14C Dataset for Calibrating the Thera Eruption

Radiocarbon ◽  
2020 ◽  
Vol 62 (4) ◽  
pp. 953-961 ◽  
Author(s):  
Ronny Friedrich ◽  
Bernd Kromer ◽  
Lukas Wacker ◽  
Jesper Olsen ◽  
Sabine Remmele ◽  
...  
Keyword(s):  
Quality Control ◽  
Tree Ring ◽  
Tree Rings ◽  
Annual Data ◽  
Calibration Data ◽  
Tree Ring Chronology ◽  
Time Period ◽  
Oak Tree ◽  
Thera Eruption

ABSTRACTAnnually resolved tree-ring samples of the time period 1625–1510 BCE were analyzed from the German oak tree-ring chronology. Blocks of the same tree rings were previously used to generate IntCal calibration data. The new dataset shows an offset to the calibration data IntCal13 of 24 years and resembles annual data for the same time period derived from tree-ring records in other growth locations. A subset of samples of the period 1625–1585 BCE was additionally measured in three other laboratories (ETH, AAR, AA) for quality control.

Useful Strategies for the Development of Tropical Tree-Ring Chronologies

IAWA Journal ◽  
1999 ◽  
Vol 20 (3) ◽  
pp. 249-253 ◽  
Author(s):  
David W. Stahle
Keyword(s):  
Tree Ring ◽  
Ring Width ◽  
Tropical Species ◽  
Growth Rings ◽  
Seasonally Dry ◽  
Effective Strategies ◽  
Annual Growth Rings ◽  
Individual Trees ◽  
The Tropics ◽  
Cross Dating

This paper outlines efficient strategies for the development of long, climatically sensitive tree-ring chronologies in the tropics. Effective strategies include sampling useful temperate or subtropical species that extend naturally into the tropics; sampling species in botanical families that have already provided examples useful for dendrochronology (e. g., Pinaceae, Taxodiaceae, Verbenaceae); targeting deciduous species in seasonally dry forests; and sampling species described in the literature or found in xylaria that have promising anatomical features such as ring porosity and marginal parenchyma. Dendrochronology can also be used to test the annual nature of growth banding in tropical species. The cross-dating oflong ring-width time series between individual trees and between multiple sites in a region is strong evidence that the growth rings are indeed synchronized with the annual calendar. This can be confirmed if the ring-width data are also strongly correlated with long annual or seasonalized records of climate variability. Blind cross-dating tests to identify the cutting dates of known-age timbers can provide a final proof that a species produces reliable annual growth rings.

Radiocarbon Ages of Annual Rings from Japanese Wood: Evident Age Offset Based on IntCal09

Radiocarbon ◽  
2013 ◽  
Vol 55 (2) ◽  
pp. 763-770 ◽  
Author(s):  
Toshio Nakamura ◽  
Kimiaki Masuda ◽  
Fusa Miyake ◽  
Kentaro Nagaya ◽  
Takahiro Yoshimitsu
Keyword(s):  
Tree Ring ◽  
Data Sets ◽  
Calibration Data ◽  
Annual Rings ◽  
Air Masses ◽  
Japanese Archipelago ◽  
The Past ◽  
Asian Summer ◽  
The Japanese Archipelago ◽  
Calendar Dates

To investigate the radiocarbon concentration of atmospheric CO2 over the past few millennia in Japan, we measured the 14C age of annual rings from 3 Japanese trees with calendar dates ranging from ∼2000 yr old to present, and we compared the tree-ring 14C age with the corresponding 14C age from IntCal09. In some instances, the 14C ages of the annual rings of Japanese trees are not consistent with the IntCal09 data sets. Often, the 14C ages of tree rings are older than those from IntCal09, but younger than those from the SHCal04 data sets. The average shifts in the Nagoya 14C age from IntCal09 data sets and 1σ errors were determined to be +26 ± 36, +24 ± 30, +16 ± 22, +5 ± 21, and +14 ± 22 14C yr for the intervals AD 72– 382, 589–1072, 1413–1615, 1617–1739, and 1790–1860, respectively. The Japanese Archipelago is situated near the boundary of the Intertropical Convergence Zone in summer, and the 14C concentration of atmospheric CO2 over Japan can be influenced by air masses of the Southern Hemisphere with lower 14C concentrations during periods of higher solar activity and heightened East Asian summer monsoons. Our results suggest that the Japanese Archipelago is located in a critical zone where it is difficult to calibrate the 14C age of tree-ring samples using existing calibration data sets. It should be noted that calibration of the 14C dates of Japanese samples with IntCal09 may induce additional systematic shifts of calibrated ages toward older ages by about 30 yr compared with the sample optimum calendar ages.

scholarly journals 14C Concentrations of Single-Year Tree Rings from About 22,000 Years Ago Obtained Using A Highly Accurate Measuring Method

Radiocarbon ◽  
2004 ◽  
Vol 46 (2) ◽  
pp. 949-955 ◽  
Author(s):  
Toshiyuki Gandou ◽  
Hirohisa Sakurai ◽  
Wataru Katoh ◽  
Yousuke Takahashi ◽  
Syuichi Gunji ◽  
...  
Keyword(s):  
Mass Spectrometry ◽  
Tree Ring ◽  
Tree Rings ◽  
Measuring Method ◽  
Time Profile ◽  
Calibration Data ◽  
Ring Sample ◽  
Standard Deviations ◽  
Counting Statistics ◽  
Calendar Dates

We have measured the radiocarbon concentrations in single-yr tree rings of old wood by accelerated mass spectrometry (AMS) using a multicathode. The 14C concentrations of 10 single-yr tree rings were measured in 100 tree rings at intervals of 10. For each single-yr tree-ring sample, typically 80 measurements of the 14C concentrations were carried out using multicathodes. The sample standard deviations indicated that there are other fluctuations of typically 1.5%, in addition to the fluctuation of the Poisson counting statistics which is typically 3% for each measurement. The average 14C date of the tree rings was 22,130 ± 306 BP for all 624 data of single-yr tree-ring samples measured by the multicathodes. From the calibration data of Lake Suigetsu, the calendar dates of these 100 tree rings were located between 25,400 cal BP and 26,150 cal BP. The 14C dates changed between 21,979 BP and 22,272 BP, with an error of approximately 50 BP, corresponding to a precision of approximately 0.5%. There was a step with a change of approximately 144 BP for each 10 yr in the time profile.

scholarly journals Dendroclimatological potential of the Australian red cedar

2005 ◽  
Vol 53 (1) ◽  
pp. 21 ◽  
Author(s):  
I. Heinrich ◽  
J. C. G. Banks
Keyword(s):  
Tree Ring ◽  
Site Index ◽  
Deciduous Tree ◽  
Growth Rings ◽  
Tree Ring Analysis ◽  
Red Cedar ◽  
Annual Growth Rings ◽  
Toona Ciliata ◽  
Ring Analysis ◽  
Instrumental Records

We examined Toona ciliata M.Roemer (Australian red cedar) for its potential to deliver annually resolved tree-ring proxy data. Such proxies are valuable and sought-after sources for reconstructing climate beyond instrumental records, especially in Australia. T. ciliata was chosen because it is one of the few deciduous tree species in Australia experiencing a seasonally dormant period of the cambium. This was confirmed by a preliminary tree-ring analysis which revealed distinct growth rings. Because of initial uncertainties regarding reliable annual growth rings in the wood of T. ciliata, a dendrometer-band study was conducted in addition to the tree-ring analysis. Stem increments revealed a common period of dormancy during winter and the measurements were found to correlate with both precipitation and temperature, depending on the site. For the first time, our tree-ring analysis demonstrated that samples from different individuals can be cross-dated and the resulting site index from Upper Kangaroo Valley (New South Wales) has the potential to reconstruct early season temperatures and late-season rainfall.

scholarly journals Calibration Commentary

Radiocarbon ◽  
2009 ◽  
Vol 51 (1) ◽  
pp. 287-290 ◽  
Author(s):  
S P E Blockley ◽  
R A Housley
Keyword(s):  
Tree Ring ◽  
Tree Rings ◽  
Late Quaternary ◽  
Climatic Changes ◽  
Growth Rings ◽  
Last Glaciation ◽  
Calibration Curves ◽  
Annual Growth Rings ◽  
Late Evolution ◽  
In The Beginning

Radiocarbon is by far and away the most widely used dating tool in the Late Quaternary. Hundreds of key papers rely on the method to provide absolute and relative chronological information on important topics, including the late evolution of our own species (e.g. Higham et al. 2006a) and the timing and nature of abrupt climatic changes during the last glaciation (Lowe et al. 2001). Calibration of 14C determinations is an essential part of the dating process, and the implications of calibration can lead to significant differences in the interpretation of important processes (Blockley et al. 2006). Any development that enhances the accuracy, precision, or time coverage of the calibration curves is therefore to be welcomed. Since the early 1980s, there has been periodic publication of carefully vetted data in the form of internationally recognized consensus calibration curves that have allowed 14C users to convert their raw 14C determinations into calendar ages (Klein et al. 1982; Stuiver and Reimer 1986, 1993; Stuiver et al. 1998; Reimer et al. 2004). In the beginning, the basis on which this was done was easy to understand, 14C measurements were made on tree rings and the absolute calendar age came from counting annual growth rings. Although not without its complexities, the terrestrial tree-ring approach remains the most certain method and is at the heart of calibration process in the period 0–12.4 cal kyr. However, for periods beyond the limit of the tree-ring sequences the situation was significantly more problematic, and at times, even controversial.

scholarly journals Radiocarbon Calibration Data for the 6th to the 8th Millennia BC

Radiocarbon ◽  
1986 ◽  
Vol 28 (2B) ◽  
pp. 954-960 ◽  
Author(s):  
Bernd Kromer ◽  
Monika Rhein ◽  
Michael Bruns ◽  
Hildegard Schoch-Fischer ◽  
Karl Otto Münnich ◽  
...  
Keyword(s):  
Tree Ring ◽  
Data Sets ◽  
Calibration Data ◽  
Calibration Curves ◽  
Oak Tree ◽  
Existing Data ◽  
Radiocarbon Calibration

14C calibration curves derived from South German oak tree-ring series are presented. They cover the interval between 4400 and 7200 BC complementing existing data sets and extending them to older periods. The atmospheric 14C level before 6200 BC no longer follows the long-term sinusoidal trend fitted to the bristlecone data. This observation is supported by a tentative match of the Main 9 series.

scholarly journals A Guarneri violin in the attic: the power of dendrochronology for analysing musical instruments

2021 ◽  
Vol 9 (1) ◽  
Author(s):  
Mauro Bernabei
Keyword(s):  
Tree Ring ◽  
Ring Width ◽  
Musical Instrument ◽  
Musical Instruments ◽  
Annual Growth ◽  
Growth Rings ◽  
Non Invasive ◽  
Annual Growth Rings ◽  
Privately Owned ◽  
Supply Information

AbstractDendrochronology is the science that dates wooden artefacts by measuring annual growth rings visible in the wood. And, in the case of musical instruments, the method is non-invasive. In addition, dendrochronology can also help to identify the wood’s provenance and to supply information on how the soundboard was made, giving details of ring width and regularity. This study also demonstrates the effectiveness of dendrochronology in attributing a musical instrument to an important luthier. It deals with a privately owned violin, whose date and origin had previously remained uncertain, despite various attempts to authenticate, at least, its technical and stylistic characteristics. The outermost tree-ring of the instrument’s soundboard was dendrochronologically dated to the year 1696 and attributed, with certainty, to the Italian luthier Giuseppe Guarneri filius Andreae, father of the famous Bartolomeo Giuseppe Guarneri "del Gesù". Thanks to dendrochronology, in this way, a twin of an already existing violin has been identified that was made by the same luthier. Both violins are identical in construction, having the same veining and dimensions, and the wood from the same tree was used in all parts, including the soundboard. Dendrochronology has, thus, been proven to be an extremely useful method, which has transformed a violin of uncertain value into a museum piece.

scholarly journals Cariaco Basin Calibration Update: Revisions to Calendar and 14C Chronologies for Core Pl07-58Pc

Radiocarbon ◽  
2004 ◽  
Vol 46 (3) ◽  
pp. 1161-1187 ◽  
Author(s):  
Konrad A Hughen ◽  
John R Southon ◽  
Chanda J H Bertrand ◽  
Brian Frantz ◽  
Paula Zermeño
Keyword(s):  
Tree Ring ◽  
Cariaco Basin ◽  
Calibration Data ◽  
Data Set ◽  
Varve Chronology ◽  
Pine Tree ◽  
Tree Ring Data ◽  
Calibration Data Set ◽  
Recent Version ◽  
Radiocarbon Calibration

This paper describes the methods used to develop the Cariaco Basin PL07-58PC marine radiocarbon calibration data set. Background measurements are provided for the period when Cariaco samples were run, as well as revisions leading to the most recent version of the floating varve chronology. The floating Cariaco chronology has been anchored to an updated and expanded Preboreal pine tree-ring data set, with better estimates of uncertainty in the wiggle-match. Pending any further changes to the dendrochronology, these results represent the final Cariaco 58PC calibration data set.

Sign in / Sign up

Export Citation Format

Share Document