Journal articles: 'Dendrochronology'

1

Alverson, Keith. "Dendrochronology." PAGES news 10, no. 1 (April 2002): 2. http://dx.doi.org/10.22498/pages.10.1.2.

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Badger, Darcie Little. ""Dendrochronology"." American Studies 60, no. 3-4 (2021): 51–53. http://dx.doi.org/10.1353/ams.2021.0025.

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Crone, Anne. "Dendrochronology." Scottish Archaeological Internet Reports 102 (January 6, 2023): 39–42. http://dx.doi.org/10.9750/issn.2056-7421.2023.102.39-42.

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Edvardsson, Johannes, Gunnar Almevik, Linda Lindblad, Hans Linderson, and Karl-Magnus Melin. "How Cultural Heritage Studies Based on Dendrochronology Can Be Improved through Two-Way Communication." Forests 12, no. 8 (August 6, 2021): 1047. http://dx.doi.org/10.3390/f12081047.

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A significant part of our cultural heritage consists of wood. Research on historical wooden structures and artefacts thereby provides knowledge of people’s daily lives and the society in which they lived. Dendrochronology is a well-established dating method of wood that can also provide valuable knowledge about climate dynamics, environmental changes, silviculture, and cultural transformations. However, dendrochronology comes with some limitations that end users in cultural heritage sciences must be aware of, otherwise their surveys may not be ultimately performed. We have drawn attention to studies in which dendrochronological results have been misinterpreted, over-interpreted, or not fully utilized. On the other hand, a rigorous dendrochronological survey may not respond to the request of information in practice. To bridge this rigour-relevance gap, this article has considered and reviewed both the dendrochronology’s science-perspective and the practitioner’s and end user’s call for context appropriate studies. The material for this study consists of (i) interviews with researchers in dendrochronology and end users represented by cultural heritage researchers with focus on building conservation and building history in Sweden, and (ii) a review of dendrochronological reports and the literature where results from the reports have been interpreted. From these sources we can conclude that a continuous two-way communication between the dendrochronologists and end users often would have resulted in improved cultural heritage studies. The communication can take place in several steps. Firstly, the design of a sampling plan, which according to the current standard for sampling of cultural materials often is required, is an excellent common starting point for communication. Secondly, the survey reports could be developed with a more extensive general outline of the method and guidance in how to interpret the results. Thirdly, the potential contribution from dendrochronology is often underused, foreseeing historical information on local climate, silviculture, and choice of quality of the wooden resource, as the focus most often is the chronological dating. Finally, the interpretation of the results should consider all the available sources where dendrochronology is one stake for a conciliant conclusion.

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Bridge, Martin. "ELM Dendrochronology." Vernacular Architecture 51, no. 1 (January 1, 2020): 94–102. http://dx.doi.org/10.1080/03055477.2020.1794245.

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Kuniholm, Peter Ian. "Archaeological dendrochronology." Dendrochronologia 20, no. 1-2 (January 2002): 63–68. http://dx.doi.org/10.1078/1125-7865-00008.

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Čufar, Katarina. "Dieter Eckstein, 1939-2021 and his rich legacy of dendrochronology in Slovenia and the world." Les/Wood 70, no. 2 (December 23, 2021): 99–109. http://dx.doi.org/10.26614/les-wood.2021.v70n02a08.

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Prof. Dr. Dieter Eckstein (1939-2021) was a leading scientist, teacher, mentor, leader, promoter and motivatorin the field of dendrochronology and wood biology. After graduating in wood science and receiving a PhD indendrochronology, he was professor of wood biology at the University of Hamburg. From 1995-2004, he was Director of the Department of Wood Biology, University of Hamburg, and of the Institute of Wood Biology and Wood Protection at the Federal Research Centre for Forestry and Forest Products in Hamburg, Germany. His work had a decisive influence on the development of wood anatomy, wood biology and dendrochronology and his laboratory was a reference point for dendrochronology worldwide. He supported dendrochronologists throughout Europe and around the world in their pioneering work to establish dendrochronology laboratories and develop dendrochronology in numerous countries, including Slovenia.

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Linderholm, Hans W., Yu Liu, Steven W. Leavitt, and Eryuan Liang. "Dendrochronology in Asia." Quaternary International 283 (January 2013): 1–2. http://dx.doi.org/10.1016/j.quaint.2012.08.004.

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9

Benarie, Michel. "Methods of dendrochronology." Science of The Total Environment 104, no. 3 (May 1991): 249. http://dx.doi.org/10.1016/0048-9697(91)90076-q.

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Kromer, Bernd. "Radiocarbon and dendrochronology." Dendrochronologia 27, no. 1 (January 2009): 15–19. http://dx.doi.org/10.1016/j.dendro.2009.03.001.

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Touchan, Ramzi, and Malcolm K. Hughes. "Dendrochronology in Jordan." Journal of Arid Environments 42, no. 4 (August 1999): 291–303. http://dx.doi.org/10.1006/jare.1999.0507.

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Dobbertin, Michèle Kaennel, and Henri D. Grissino-Mayer. "Bibliografie und Glossar zur Dendrochronologie: zwei neue Informationsquellen für die Jahrringforschung | The «Bibliography of Dendrochronology» and the «Glossary of Dendrochronology»: two new online tools for tree-ring research." Schweizerische Zeitschrift fur Forstwesen 155, no. 6 (June 1, 2004): 238–40. http://dx.doi.org/10.3188/szf.2004.0238.

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Two new online products are available to the international tree-ring research community: the Bibliography of Dendrochronology,which currently has 10 000 references and is the world's largest online bibliography specialised in tree-ring research,and the Glossary of Dendrochronology, a searchable database of 351 terms and definitions in English, German,French, Spanish, Italian and Portuguese. Both databases are the result of the collaboration of numerous tree-ring scientists from around the world.

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13

Biondi, Franco. "From Dendrochronology to Allometry." Forests 11, no. 2 (January 27, 2020): 146. http://dx.doi.org/10.3390/f11020146.

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The contribution of tree-ring analysis to other fields of scientific inquiry with overlapping interests, such as forestry and plant population biology, is often hampered by the different parameters and methods that are used for measuring growth. Here I present relatively simple graphical, numerical, and mathematical considerations aimed at bridging these fields, highlighting the value of crossdating. Lack of temporal control prevents accurate identification of factors that drive wood formation, thus crossdating becomes crucial for any type of tree growth study at inter-annual and longer time scales. In particular, exactly dated tree rings, and their measurements, are crucial contributors to the testing and betterment of allometric relationships.

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Sparks, Jodi K. Farrell, and Graham I. Bishop. "Evaluation ofSassafras albidumfor Dendrochronology." Tree-Ring Research 65, no. 2 (July 2009): 157–61. http://dx.doi.org/10.3959/2008-17.2.

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15

Cruz, Pedro, John Wihbey, Avni Ghael, Felipe Shibuya, and Stephen Costa. "Dendrochronology of U.S. immigration." Information Design Journal 25, no. 1 (December 31, 2019): 6–20. http://dx.doi.org/10.1075/idj.25.1.01cru.

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Abstract Immigrants are central to the identity of the United States, the population of which has grown in number and diversity as a function of new arrivals from around the globe. This article describes a visualization project that uses the visual metaphor of tree rings to explore the contribution of immigrants to the country’s population. Immigrants and native-born persons are represented and differentiated as cells in trees, with layered annual rings capturing patterns of population growth. These rings register, in their shape and color, certain environmental conditions. In order to mimic the natural process by which growth rings are formed, we devised a computational system that simulates the growth of trees as if cells were data-units. Dendrochronology involves dating certain events by analyzing patterns of growth in trees. Analogously, in our visualizations the rings can be counted and dated, showing the chronological evolution of the population. The dendrochronology theme is a poetic take on the data, yet it is also a functional and conceptual space that is used to construct language and rationales on that data. The tree-growth process not only inspires the appearance of the visualizations but also informs the rules of the computational system that creates them.

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Pumijumnong, Nathsuda. "Dendrochronology in Southeast Asia." Trees 27, no. 2 (September 27, 2012): 343–58. http://dx.doi.org/10.1007/s00468-012-0775-7.

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Bill, Jan, Aoife Daly, Øistein Johnsen, and Knut S. Dalen. "DendroCT – Dendrochronology without damage." Dendrochronologia 30, no. 3 (January 2012): 223–30. http://dx.doi.org/10.1016/j.dendro.2011.11.002.

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18

Litton, C. D., and H. J. Zainodin. "Statistical models of dendrochronology." Journal of Archaeological Science 18, no. 4 (July 1991): 429–40. http://dx.doi.org/10.1016/0305-4403(91)90036-o.

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19

D. Rumyantsev. "Global Ecopotential of Dendrochronology." Ecology, Environment and Conservation 28, no. 04 (2022): 2214–16. http://dx.doi.org/10.53550/eec.2022.v28i04.086.

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Drought is a meteorological phenomenon that has influenced the life of human society for ages and still has a great impact on it. This phenomenon can be divided into a group of sub-phenomena, e.g. soil and air droughts, winter droughts, etc.… From a physiological point of view, drought may have different consequences in different periods of a growing season. It seems however difficult to describe quantitative characteristics of a physiologically important drought using any meteorological parameters because within an ecosystem the results of the interaction of ecological factors may change the way plants respond to a certain limited number of values of meteorological parameters. Photosynthesis and transpiration characteristics predetermine that the function modelling annual tree ring variability will always and under any conditions have a variable that will depend on drought. The objective of dendroclimatic studies can be either to separate a drought-associated climatic signal from the tree ring chronology or, on the contrary, to search a chronology with a “clear” and easily detected drought-associated signal. Having retrospective aspects, Dendroclimatic studies show considerable promise for the evaluation of droughts including those that have an impact on crop yields. Such studies can give further information for crop yield forecasts.

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20

Towner, Ronald H. "Dateless Dendroarchaeology." Forests 13, no. 2 (February 10, 2022): 281. http://dx.doi.org/10.3390/f13020281.

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The strength of dendrochronology is chronology. No other non-textual dating technique in the world provides the precision, accuracy, and resolution of dendrochronology. Indeed, dendrochronology is famous for dating prehistoric ruins, and Douglass’ “Bridging the Gap” is still considered one of the greatest achievements in archaeology anywhere, but what happens when samples don’t date? Should they simply be discarded as useless, stored until better chronologies and new techniques are available, or do they contain useful information for current research interests? Using undated collections from the southwestern US and northwestern Mexico, this paper discusses a variety of behavioral and environmental information present in samples, even if they cannot contribute to our chronological knowledge.

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21

Pearson, Stuart G., and Matthew John Searson. "High-resolution data from Australian trees." Australian Journal of Botany 50, no. 4 (2002): 431. http://dx.doi.org/10.1071/bt01071.

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Dendrochronology offers data with unparalleled spatial and temporal resolution but the technique has received only sporadic attention in Australia. The techniques deserve wider application in the resolution of contentious issues such as tree population dynamics, fire histories and atmospheric change. Convergence of ecological and palaeoecological research scales, recent technical developments and a growing willingness to experiment mark a watershed in Australian dendrochronology. Progress in dendrochronology in Australia requires transect studies to examine species and site effects by rapid survey techniques, interdisciplinary approaches to extract the full range of proxy data in wood and environmental modelling to calibrate and interpret tree records. Future rewards include annually resolved data across the landscape for the last few hundred years providing answers to questions regarding tree recruitment, fire regimes and the impact of CO2 enrichment.

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22

Boninsegna, Jose A. "Progress in South American Dendrochronology." PAGES news 10, no. 1 (April 2002): 11–13. http://dx.doi.org/10.22498/pages.10.1.11.

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23

Baker, Partick J. "Dendrochronology heats up Down Under." Past Global Changes Magazine 22, no. 2 (October 2014): 108. http://dx.doi.org/10.22498/pages.22.2.108.

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Boninsegna, José Armando. "Dendrochronology for the Third Millennium." PAGES news 9, no. 1 (April 2001): 14. http://dx.doi.org/10.22498/pages.9.1.14.

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LU Xiaoming, 芦晓明, and 梁尔源 LIANG Eryuan. "Progresses in dendrochronology of shrubs." Acta Ecologica Sinica 33, no. 5 (2013): 1367–74. http://dx.doi.org/10.5846/stxb201208031105.

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26

Wigley, T. M. L., P. D. Jones, and K. R. Briffa. "Cross-dating methods in dendrochronology." Journal of Archaeological Science 14, no. 1 (January 1987): 51–64. http://dx.doi.org/10.1016/s0305-4403(87)80005-5.

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27

Hillam, J., C. M. Groves, D. M. Brown, M. G. L. Baillie, J. M. Coles, and B. J. Coles. "Dendrochronology of the English Neolithic." Antiquity 64, no. 243 (June 1990): 210–20. http://dx.doi.org/10.1017/s0003598x00077826.

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In the period 1970–85, tree-ring research in Europe had resulted in the production of long oak chronologies for both Ireland and Germany going back over 7000 years (e.g. Brown et al. 1986; Leuschner & Delorme 1984). In England, there was a network of regional chronologies covering the historic period, and almost no chronological coverage for the prehistoric. For the archaeologist this meant that, provided a site from the historic period produced a replicated site chronology, the chances of dating by dendrochronology were very high. The chances of this happening for a prehistoric site were poor by comparison, although some sites were successfully dated, for example the Iron Age causeway from Fiskerton in Liricolnshire and the Hasholme log boat found in North Humberside (Hillam 1987).The period 1985–88 saw an intense effort to outline a prehistoric oak tree-ring chronology in England (Baillie & Brown 1988). This work centred on sub-fossil oaks from East Anglia and Lancashire and built on a previous chronology from Swan Carr, near Durham which spanned 1155–381 BC (Baillie et al. 1983). The approach to chronology-building was to produce wellreplicated chronology units which could be located precisely in time against the existing Irish (Pilcher et al. 1984) and North German (Leuschner & Delorme 1984) chronologies.

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28

Dobbertin, Michéle Kaennel, and Henri D. Grissino-Mayer. "The online bibliography of dendrochronology." Dendrochronologia 21, no. 2 (January 2004): 85–90. http://dx.doi.org/10.1078/1125-7865-00042.

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29

Brown, D. M., M. A. R. Munro, M. G. L. Baillie, and J. R. Pilcher. "Dendrochronology—The Absolute Irish Standard." Radiocarbon 28, no. 2A (1986): 279–83. http://dx.doi.org/10.1017/s0033822200007372.

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Since the 11th International Radiocarbon Conference considerable advances have been made in European dendrochronology giving several long continuous absolute chronologies. Recent collaboration between European laboratories provides confirmation of the accuracy of these chronologies and, thus, of the standards used for radiocarbon calibration.

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30

Smith, Kevin T. "An organismal view of dendrochronology." Dendrochronologia 26, no. 3 (December 2008): 185–93. http://dx.doi.org/10.1016/j.dendro.2008.06.002.

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31

Pourtahmasi, Kambiz, Qi-Bin Zhang, and Binod Dawadi. "Asian Dendrochronology Association (ADA) 2015." Dendrochronologia 41 (January 2017): 1. http://dx.doi.org/10.1016/j.dendro.2016.11.003.

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Meko, D. M., C. A. Woodhouse, and K. Morino. "Dendrochronology and links to streamflow." Journal of Hydrology 412-413 (January 2012): 200–209. http://dx.doi.org/10.1016/j.jhydrol.2010.11.041.

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33

Sánchez-Calderón, Oscar David, Teodoro Carlón-Allende, Manuel E. Mendoza, and José Villanueva-Díaz. "Dendroclimatology in Latin America: A Review of the State of the Art." Atmosphere 13, no. 5 (May 6, 2022): 748. http://dx.doi.org/10.3390/atmos13050748.

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The application of dendrochronology for understanding climatic variations has been of great interest to climatologists, ecologists, geographers, archeologists, among other sciences, particularly in recent decades when more dendrochronological studies have been developed. We analyzed and identified the current state and recent advances in dendroclimatology in Latin America for the period 1990 to 2020. We carried out reviews in ScienceDirect, Web of Science, and Scopus databases with the keywords “dendrochronology”, “dendroclimatology”, “dendrochronology and climatic variability”, “dendroclimatology and climatic variability”, “dendrochronology and trend”, and “dendroclimatology and trend” for each Latin American country. Results show that dendroclimatological research in the last 11 years has increased and has been mainly developed in temperate climate zones (83%) and tropical or subtropical areas (17%), where conifer species have been the most used with over 59% of the studies. However, broadleaf species for dendrochronological studies have also increased in the last decade. Dendroclimatological research in Latin America has provided important advances in the study of climatic variability by defining the response functions of tree-rings to climate and developing climatic reconstructions. Our research identified areas where it is necessary to increase dendroclimatic studies (e.g., dry and tropical forests), in addition to applying new techniques such as isotope analysis, blue intensity, dendrochemistry, among other tree-ring applications.

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Manning, Sturt W., Mike Barbetti, Bernd Kromer, Peter Ian Kuniholm, Ingeborg Levin, Maryanne W. Newton, and Paula J. Reimer. "No Systematic Early Bias to Mediterranean 14C Ages: Radiocarbon Measurements from Tree-Ring and Air Samples Provide Tight Limits to Age Offsets." Radiocarbon 44, no. 3 (2002): 739–54. http://dx.doi.org/10.1017/s0033822200032197.

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Existing data and theory do not support a recent assertion that upwelling of old carbon has led to systematically 100–300 yr too old radiocarbon ages for the Mediterranean region. Similarly, the prehistoric tree-ring record produced over 3 decades by the Aegean Dendrochronology Project is shown to provide robust, well-replicated data, contrary to a recent unfounded assertion. 14C and dendrochronology provide an accurate and precise chronometric framework for the Mediterranean region.

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35

Perez Antelo, A. "Current situation of dendrochronological research in Spain. Review note." Forest Systems 3, no. 2 (December 1, 1994): 221–35. http://dx.doi.org/10.5424/533.

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The article discuss papers dealing with dendrochronology published before 1994, and on some major data of the series they include, in order to get a general view of the dendrochonological coverage of Spain. It also presents a list of the Spanis Research Institutions that are working on dendrochronology at present, as well as another one of research studies carried out on the topic by foreign scientists in Spain. Most chronologies have been carried out on mountain areas and on species belonging to the genus Pinus, specially Pinus uncinata and Pinus sylvestris. They have been carried out with a clear dendroclimatological objective, and sometimes for historial datation. The number of species utilized in dendrochronological studies has increased in the last years, even with broadleaved trees, and new methodological orientations aimed at establishing relationships between dendrochronology and phytoclimatology have arisen thus opening new and interesting possibilities.

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36

Sheppard, Paul R. "Web-Based Tools for Teaching Dendrochronology." Journal of Natural Resources and Life Sciences Education 31, no. 1 (2002): 123–30. http://dx.doi.org/10.2134/jnrlse.2002.0123.

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Kennedy Sutherland, Elaine, P. Brewer, and W. Gross. "Paleo-event data standards for dendrochronology." Past Global Changes Magazine 25, no. 3 (December 2017): 163. http://dx.doi.org/10.22498/pages.25.3.163.

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SPEER, JAMES H., and KARLA M. HANSEN-SPEER. "ECOLOGICAL APPLICATIONS OF DENDROCHRONOLOGY IN ARCHAEOLOGY." Journal of Ethnobiology 27, no. 1 (March 2007): 88–109. http://dx.doi.org/10.2993/0278-0771(2007)27[88:eaodia]2.0.co;2.

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Penoyre, John, and Jane Penoyre. "The Somerset Dendrochronology Project: Phase 3." Vernacular Architecture 30, no. 1 (June 1999): 54–57. http://dx.doi.org/10.1179/vea.1999.30.1.54.

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Alcock, N. W., P. A. Leggett, M. K. Hughes, and I. Tyers. "List 106: Lancashire and Merseyside Dendrochronology." Vernacular Architecture 31, no. 1 (June 2000): 89–90. http://dx.doi.org/10.1179/vea.2000.31.1.89.

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41

Miles, Daniel, and Michael Worthington. "List 129: Horsham Area Dendrochronology Project." Vernacular Architecture 33, no. 1 (June 2002): 99–101. http://dx.doi.org/10.1179/vea.2002.33.1.99.

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Grant, M. E. "Dendrochronology in South Asia, an Update." South Asian Studies 8, no. 1 (January 1992): 115–23. http://dx.doi.org/10.1080/02666030.1992.9628450.

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Ababneh, Linah N., Ronald H. Towner, Mary M. Prasciunas, and Karen T. Porter. "The Dendrochronology of Palluche Canyon, Dinétah." KIVA 66, no. 2 (December 2000): 267–89. http://dx.doi.org/10.1080/00231940.2000.11758432.

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Stein, Mordechai, Steven L. Goldstein, and Alexandra Schramm. "Radiocarbon Calibration Beyond the Dendrochronology Range." Radiocarbon 42, no. 3 (2000): 415–22. http://dx.doi.org/10.1017/s0033822200030344.

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The radiocarbon timescale has been calibrated by dendrochronology back to 11.8 ka cal BP, and extended to 14.8 ka cal BP using laminated marine sediments from the Cariaco Basin. Extension to nearly 23.5 ka cal BP is based on comparison between 14C and U-Th ages of corals. Recently, attempts to further extend the calibration curve to >40 kyr are based on laminated sediments from Lake Suigetsu, Japan, foraminifera in North Atlantic sediments, South African cave deposits, tufa from Spain, and stalagmites from the Bahamas. Here we compare these records with a new comparison curve obtained by 234U-230Th ages of aragonite deposited at Lake Lisan (the last Glacial Dead Sea). This comparison reveals broad agreement for the time interval of 20–32 ka cal BP, but the data diverge over other intervals. All records agree that Δ14C values range between ∼250–450‰ at 20–32 ka cal BP. For ages >32 ka cal BP, the Lake Suigetsu data indicate low Δ14C values of less than 200‰ and small shifts. The other records broadly agree that Δ14C values range between ∼250 and 600‰ at 32–39 ka cal BP. At ∼42 ka cal BP, the North Atlantic calibration shows low Δ14C values, while the corals, Lisan aragonites, and the Spanish tufa indicate a large deviations of 700–900‰. This age is slightly younger than recent estimates of the timing of the Laschamp Geomagnetic Event, and are consistent with increased 14C production during this event.

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Turkon, Paula, Sturt W. Manning, Carol Griggs, Marco Antonio Santos Ramírez, Ben A. Nelson, Carlos Torreblanca Padilla, and Eva Maria Wild. "APPLICATIONS OF DENDROCHRONOLOGY IN NORTHWESTERN MEXICO." Latin American Antiquity 29, no. 1 (December 14, 2017): 102–21. http://dx.doi.org/10.1017/laq.2017.60.

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Although dendrochronological methods have the potential to provide precise calendar dates, they are virtually absent in Mesoamerican archaeological research. This absence is due to several long-standing, but erroneous, assumptions: that tree rings in this region do not reflect annual growth and environmental variability, that an adequate number of samples do not exist, and that tree-ring measurements cannot be useful without modern trees to link prehispanic chronologies. In this article we present data from the sites of La Quemada and Los Pilarillos, located in the Malpaso Valley, Zacatecas, to demonstrate that suitable archaeologically derived samples of dendrochronologically useful species do exist, that the samples from these sites are measurable and cross-datable, and that the tree rings can yield precise calendar dates using a method that “wiggle-matches” radiocarbon dates on tree-ring sequences. The work demonstrates the potential of these methods to address chronological, and, in the future, climatic questions, which have so far eluded archaeological work in the region.

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Sabir, Mohammad Amjad, Muhammad Umar, Muhammad Farooq, and Faridullah Faridullah. "Computing soil creep velocity using dendrochronology." Bulletin of Engineering Geology and the Environment 75, no. 4 (January 8, 2016): 1761–68. http://dx.doi.org/10.1007/s10064-015-0838-2.

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Brookhouse, Matthew. "Eucalypt dendrochronology: past, present and potential." Australian Journal of Botany 54, no. 5 (2006): 435. http://dx.doi.org/10.1071/bt05039.

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Dendrochronology has the capacity to provide unique insights into natural vegetation dynamics and yield climatological reconstructions. However, because of a persistent belief that eucalypts are unsuited to dendrochronological analysis, research interest in the genus has been limited. A thorough review of the eucalypt dendrochronological literature reveals that perceived limitations may be locally overcome. However, methodological problems associated with many studies mean that results are often difficult to interpret. Consequently, the dendrochronological potential of the eucalypts remains unresolved. To overcome this, a detailed dendrochronological reconnaissance of the eucalypts, drawing on established datasets, systematic study of individual species and sites and examination of non-width-based tree-ring properties, is recommended.

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48

Schia, Erik. "Dendrochronology on material from medieval Oslo." Norwegian Archaeological Review 23, no. 1-2 (January 1990): 38–42. http://dx.doi.org/10.1080/00293652.1990.9965505.

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49

Lüttge, Ulrich. "From dendrochronology and dendroclimatology to dendrobiochemistry." Trees 31, no. 6 (September 7, 2017): 1743–44. http://dx.doi.org/10.1007/s00468-017-1608-5.

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Büntgen, Ulf. "Re-thinking the boundaries of dendrochronology." Dendrochronologia 53 (February 2019): 1–4. http://dx.doi.org/10.1016/j.dendro.2018.10.012.

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Journal articles on the topic 'Dendrochronology'

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