Dendrochronology - Knowledge (XXG)

479: 4558: 47: 337: 1153: 311: 4586: 408: 471: 439:), and the age of the wood can thereby be determined precisely. Dendrochronologists originally carried out cross-dating by visual inspection; more recently, they have harnessed computers to do the task, applying statistical techniques to assess the matching. To eliminate individual variations in tree-ring growth, dendrochronologists take the smoothed average of the tree-ring widths of multiple tree-samples to build up a 4626: 4544: 2324: 404:, where the seasons differ more markedly. The inner portion of a growth ring forms early in the growing season, when growth is comparatively rapid (hence the wood is less dense) and is known as "early wood" (or "spring wood", or "late-spring wood"); the outer portion is the "late wood" (sometimes termed "summer wood", often being produced in the summer, though sometimes in the autumn) and is denser. 1222:

been felled and left for many years before use, or could have been used to replace a damaged piece of wood. The dating of building via dendrochronology thus requires knowledge of the history of building technology. Many prehistoric forms of buildings used "posts" that were whole young tree trunks; where the bottom of the post has survived in the ground these can be especially useful for dating.

4636: 1323: 2063:(Both branches that are presented in plate 42, fig. 6 (with the cross-section in fig. 7) and fig. 1 (with the cross-section in fig. 2) had produced, in the defoliation year of 1862, a growth ring that was twice as strong as in the preceding one, and so was the ring of the year-old shoot (not illustrated here) stronger in the case of the defoliated tree than one that was not defoliated.) 4614: 1459: 4572: 3448: 4530: 31: 435:

therefore under similar climatic conditions). When one can match these tree-ring patterns across successive trees in the same locale, in overlapping fashion, chronologies can be built up—both for entire geographical regions and for sub-regions. Moreover, wood from ancient structures with known chronologies can be matched to the tree-ring data (a technique called

4600: 2061:"Die beiden, auf Taf. 42, Fig. 6 (mit dem Durchschnitt Fig. 7) und Fig. 1 (mit dem Durchschnitt Fig. 2) dargestellten Zweige hatten in dem Frassjahre 1862 einen doppelt so starken Jahrring als in dem vorhergehenden angelegt, und auch der (hier nicht abgebildete) Ring des jährigen Triebes war bei den gefressenen stärker as der eines nicht gefressenen." 1169:" (earliest possible) date, and a tentative date for the arrival of a seasoned raw panel using assumptions as to these factors. As a result of establishing numerous sequences, it was possible to date 85–90% of the 250 paintings from the fourteenth to seventeenth century analysed between 1971 and 1982; by now a much greater number have been analysed. 1067:. This can be done by checking radiocarbon dates against long master sequences, with Californian bristle-cone pines in Arizona being used to develop this method of calibration as the longevity of the trees (up to c.4900 years) in addition to the use of dead samples meant a long, unbroken tree ring sequence could be developed (dating back to 136:, which always produces a range rather than an exact date. However, for a precise date of the death of the tree a full sample to the edge is needed, which most trimmed timber will not provide. It also gives data on the timing of events and rates of change in the environment (most prominently climate) and also in wood found in 892: 1221:

is the term for the application of dendrochronology in archaeology. While archaeologists can date wood and when it was felled, it may be difficult to definitively determine the age of a building or structure in which the wood was used; the wood could have been reused from an older structure, may have

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Critical to the science, trees from the same region tend to develop the same patterns of ring widths for a given period of chronological study. Researchers can compare and match these patterns ring-for-ring with patterns from trees which have grown at the same time in the same geographical zone (and

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Many trees in temperate zones produce one growth-ring each year, with the newest adjacent to the bark. Hence, for the entire period of a tree's life, a year-by-year record or ring pattern builds up that reflects the age of the tree and the climatic conditions in which the tree grew. Adequate moisture

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is exceptionally long-lived and slow growing, and has been used extensively for chronologies; still-living and dead specimens of this species provide tree-ring patterns going back thousands of years, in some regions more than 10,000 years. Currently, the maximum span for fully anchored chronology is

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marginal conditions such as aridity or semi-aridity where the ring growth is more sensitive to the environment, rather than in humid areas where tree-ring growth is more uniform (complacent). In addition, some genera of trees are more suitable than others for this type of analysis. For instance, the

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Direct reading of tree ring chronologies is a complex science, for several reasons. First, contrary to the single-ring-per-year paradigm, alternating poor and favorable conditions, such as mid-summer droughts, can result in several rings forming in a given year. In addition, particular tree species

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From p. 423: "Moreover, the wood of the silver-fir has many layers, like an onion; there is always another beneath that which is visible, and the wood is composed of such layers throughout." Although many sources claim that Theophrastus recognized that trees form growth rings annually, this is not

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Bard et al write in 2023: "The oldest tree-ring series are known as floating since, while their constituent rings can be counted to create a relative internal chronology, they cannot be dendro-matched with the main Holocene absolute chronology. However, 14C analyses performed at high resolution on

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Given a sample of wood, the variation of the tree-ring growths not only provides a match by year, but can also match location because climate varies from place to place. This makes it possible to determine the source of ships as well as smaller artifacts made from wood, but which were transported

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Timber core samples are sampled and used to measure the width of annual growth rings; by taking samples from different sites within a particular region, researchers can build a comprehensive historical sequence. The techniques of dendrochronology are more consistent in areas where trees grew in

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There are many different file formats used to store tree ring width data. Effort for standardisation was made with the development of TRiDaS. Further development led to the database software Tellervo, which is based on the new standard format whilst being able to import lots of different data

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are available going back 13,910 years. A new method is based on measuring variations in oxygen isotopes in each ring, and this 'isotope dendrochronology' can yield results on samples which are not suitable for traditional dendrochronology due to too few or too similar rings. Some regions have

611: 1912:..., pp. 273–298. Studhalter (1956), p. 33, stated that Carl Linnaeus (1745, 1751) in Sweden, Friedrich August Ludwig von Burgsdorf (1783) in Germany, and Alphonse de Candolle (1839–1840) in France subsequently observed the same tree ring in their samples. 650: 1122:. However, unlike analysis of samples from buildings, which are typically sent to a laboratory, wooden supports for paintings usually have to be measured in a museum conservation department, which places limitations on the techniques that can be used. 396:

of the year; thus, critical for the title method, one ring generally marks the passage of one year in the life of the tree. Removal of the bark of the tree in a particular area may cause deformation of the rings as the plant overgrows the scar.

454:. Comparison of radiocarbon and dendrochronological ages supports the consistency of these two independent dendrochronological sequences. Another fully anchored chronology that extends back 8,500 years exists for the bristlecone pine in the 1866:"De la cause de l'excentricité des couches ligneuses qu'on apperçoit quand on coupe horisontalement le tronc d'un arbre ; de l'inégalité d'épaisseur, & de different nombre de ces couches, tant dans le bois formé que dans l'aubier" 1876:(On the cause of the eccentricity of the woody layers that one sees when one horizontally cuts the trunk of a tree ; on the unequal thickness, and on the different number of layers in the mature wood as well as in the sapwood), 1180:

was believed to be an eighteenth-century copy. However, dendrochronology revealed that the wood dated from the second half of the sixteenth century. It is now regarded as an original sixteenth-century painting by an unknown artist.

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occurs in a layer of cells near the bark. A tree's growth rate changes in a predictable pattern throughout the year in response to seasonal climate changes, resulting in visible growth rings. Each ring marks a complete cycle of

1432:). These are used for dating in a manner similar to dendrochronology, and such techniques are used in combination with dendrochronology, to plug gaps and to extend the range of the seasonal data available to archaeologists and 1273:(and being the oldest wood-framed house in North America), core samples of wood taken from a summer beam confirmed the wood was from an oak tree felled in 1637–8, as wood was not seasoned before use in building at that time in 1021:

in Newfoundland were dated by finding the layer with the 993 spike, which showed that the wood is from a tree felled in 1021. Researchers at the University of Bern have provided exact dating of a floating sequence in a

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Since panels of seasoned wood were used, an uncertain number of years has to be allowed for seasoning when estimating dates. Panels were trimmed of the outer rings, and often each panel only uses a small part of the

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The sixteenth century saw a gradual replacement of wooden panels by canvas as the support for paintings, which means the technique is less often applicable to later paintings. In addition, many panel paintings were

270: 215:(1801–1884) suggested in 1833 that patterns among tree rings could be used to synchronize the dendrochronology of various trees and thereby to reconstruct past climates across entire regions. The English polymath 165:"floating sequences", with gaps which mean that earlier periods can only be approximately dated. As of 2024, only three areas have continuous sequences going back to prehistoric times, the foothills of the 1523:

From p. 5: "One can see that in all this we are measuring the lapse of time by means of a slow-geared clock within trees. For this study the name "dendro-chronology" has been suggested, or "tree-time."

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While dendrochronology has become an important tool for dating oak panels, it is not effective in dating the poplar panels often used by Italian painters because of the erratic growth rings in poplar.

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The dendrochronological equation defines the law of growth of tree rings. The equation was proposed by Russian biophysicist Alexandr N. Tetearing in his work "Theory of populations" in the form:

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European chronologies derived from wooden structures initially found it difficult to bridge the gap in the fourteenth century when there was a building hiatus, which coincided with the

199:(1452–1519) was the first person to mention that trees form rings annually and that their thickness is determined by the conditions under which they grew. In 1737, French investigators 1110:

density (MXD) have been shown to be better proxies than simple ring width. Using tree rings, scientists have estimated many local climates for hundreds to thousands of years previous.

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A fully anchored and cross-matched chronology for oak and pine in central Europe extends back 12,460 years, and an oak chronology goes back 7,429 years in Ireland and 6,939 years in

3944: 2174:"Early wood" is used in preference to "spring wood", as the latter term may not correspond to that time of year in climates where early wood is formed in the early summer (e.g. 1309:

overlapped absolute and floating tree-rings series enable one to link them almost absolutely and hence to extend the calibration on annual tree rings until ≈13 900 cal yr BP."

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Proceedings of the Fifth Meeting of the British Association for the Advancement of Science held in Dublin during the week from the 10th to the 15th of August, 1835, inclusive

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deposition in a lake, river, or sea bed). The deposition pattern in the core will vary for a frozen-over lake versus an ice-free lake, and with the fineness of the sediment.

2250:"The 12,460-Year Hohenheim Oak and Pine Tree-Ring Chronology from Central Europe—A Unique Annual Record for Radiocarbon Calibration and Paleoenvironment Reconstructions" 3036: 887:{\displaystyle \Delta L(t)=-{\frac {c_{1}e^{-a_{1}t}+c_{2}e^{-a_{2}t}}{3k_{v}\rho ^{\frac {1}{3}}\left(c_{4}+c_{1}e^{-a_{1}t}+c_{2}e^{-a_{2}t}\right)^{\frac {2}{3}}}}} 3236: 2901: 1277:. An additional sample from another beam yielded a date of 1641, thus confirming the house had been constructed starting in 1638 and finished sometime after 1641 . 3543:

Briand, Christopher H.; Brazer, Susan E.; Harter-Dennis, Jeannine M. (December 2006). "Tree Rings and the Aging of Trees: A Controversy in 19th Century America".

85:, the study of climate and atmospheric conditions during different periods in history from the wood of old trees. Dendrochronology derives from the Ancient Greek 2687:

A previous version "Marking time: Cosmic ray storms can pin precise dates on history from ancient Egypt to the Vikings" appeared in Science, Vol 380, Issue 6641.

1832:(The rings around the branches of trees that have been sawed show the number of its years and which were the wetter or drier the more or less their thickness.) 1517:. Vol. II. A Study of the Annual Rings of Trees in relation to Climate and Solar Activity. Washington, D.C., USA: Carnegie Institute of Washington. p. 482:

A typical form of the function of the wood ring (in accordance with the dendrochronological equation) with an increase in the width of wood ring at initial stage

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During the latter half of the nineteenth century, the scientific study of tree rings and the application of dendrochronology began. In 1859, the German-American

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Dendrochronology allows specimens of once-living material to be accurately dated to a specific year. Dates are often represented as estimated calendar years

1897: 1869: 3504: 1830:"Li circuli delli rami degli alberi segati mostrano il numero delli suoi anni, e quali furono più umidi o più secchi la maggiore o minore loro grossezza." 3652: 478: 256:(1839–1901), a German professor of forest pathology, wrote a series of papers on the anatomy and ecology of tree rings. In 1892, the Russian physicist 3388:"A radiocarbon spike at 14 300 cal yr BP in subfossil trees provides the impulse response function of the global carbon cycle during the Late Glacial" 3103: 1290:, where, between the tenth and the fifteenth century, numerous consecutive layers of wooden log pavement have been placed over the accumulating dirt. 2677:"Marking time: Radiocarbon timestamps left in ancient tree rings by cosmic ray bombardments can date historical events with unprecedented precision" 3539:, the academic site of Prof. Henri D. Grissino-Mayer, Department of Geography, The University of Tennessee, and the Laboratory of Tree-Ring Science 3081: 2248:

Friedrich, Michael; Remmele, Sabine; Kromer, Bernd; Hofmann, Jutta; Spurk, Marco; Felix Kaiser, Klaus; Orcel, Christian; Küppers, Manfred (2004).

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Spronk, Ron (1996). "More than Meets the Eye: An Introduction to Technical Examination of Early Netherlandish Paintings at the Fogg Art Museum".

2288: 240:(1801–1871) observed the effects on tree rings of defoliation caused by insect infestations. By 1882, this observation was already appearing in 423:

may present "missing rings", and this influences the selection of trees for study of long time-spans. For instance, missing rings are rare in

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Die Waldverderbniss oder dauernder Schade, welcher durch Insektenfrass, Schälen, Schlagen und Verbeissen an lebenenden Waldbäumen entsteht.

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in tree rings for that year all round the world, they can be used to date historical events to the year. For example, wooden houses in the

986:. However, there do exist unbroken chronologies dating back to prehistoric times, for example the Danish chronology dating back to 352 BC. 51: 2027: 1766:

Studhalter, R. A.; Glock, Waldo S.; Agerter, Sharlene R. (1963). "Tree Growth: Some Historical Chapters in the Study of Diameter Growth".

248:(1851–1922) was using crossdating to reconstruct the climates of the Netherlands and Germany. In 1881, the Swiss-Austrian forester Arthur 2306: 1976: 1958: 1925: 1300:

formats. The desktop application can be attached to measurement devices and works with the database server that is installed separately.

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Andrej Maczkowski et al, "Absolute dating of the European Neolithic using the 5259 BC rapid 14C excursion", Nature Communications, 2024

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tree rings (also called growth rings) to the exact year they were formed in a tree. As well as dating them, this can give data for

1895:"Observations des différents effets que produisent sur les végétaux les grandes gelées d'hiver et les petites gelées du printemps" 1009:, can provide fixed reference points in an unknown time sequence as they are due to cosmic radiation. As they appear as spikes in 4856: 3631: 2949: 1060: 283: 145: 3949: 1934: 1616:

Loader, Neil J.; Mccarroll, Danny; Miles, Daniel; Young, Giles H. F.; Davies, Darren; Ramsey, Christopher Bronk (August 2019).

204: 3051: 1348: 200: 5266: 3299: 3244: 2898: 1904:(Observations on the different effects that the severe frosts of winter and the minor frosts of spring produce on plants), 5014: 4022: 3214: 3134: 324: 2227: 1923:"On the growth of timber — Extract of a letter from Mr. Alexander C. Twining, to the Editor, dated Albany, April 9, 1833" 1544: 5517: 5009: 2850: 1126: 459: 1006: 1002: 447:. It can be anchored by cross-matching a section against another chronology (tree-ring history) whose dates are known. 5542: 5199: 5069: 3832: 3638: 1200: 606:{\displaystyle \Delta L(t)={\frac {1}{k_{v}\,\rho ^{\frac {1}{3}}}}\,{\frac {d\left(M^{\frac {1}{3}}(t)\right)}{dt}},} 1852:, who in 1581 was touring Italy, where he encountered a carpenter who explained that trees form a new ring each year. 1333: 236:) in order to study the record of climate in western Texas. In 1866, the German botanist, entomologist, and forester 219:

proposed using dendrochronology to date the remains of trees in peat bogs or even in geological strata (1835, 1838).

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Ignoring the natural sinusoidal oscillations in tree mass, the formula for the changes in the annual ring width is:

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produced a distinctly dark tree ring, which served as a reference for subsequent European naturalists. In the U.S.,

5409: 5389: 4346: 3988: 3939: 3624: 2626: 1665:"Researchers succeed for first time in accurately dating a 7,000-year-old prehistoric settlement using cosmic rays" 1617: 1440: 455: 291: 1352: 1337: 5399: 5371: 4983: 4309: 4129: 3998: 3659: 1664: 257: 132:

Dendrochronology is useful for determining the precise age of samples, especially those that are too recent for

46: 5466: 4665: 4448: 4134: 3742: 3707: 3120: 2768:"Cold adaptation recorded in tree rings highlights risks associated with climate change and assisted migration" 974:

dated sequence going back 55,000 years. The most recent part, going back 13,900 years, is based on tree rings.

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primarily from the properties of the annual tree rings. Other properties of the annual rings, such as maximum

1894: 1864: 443:, a process termed replication. A tree-ring history whose beginning- and end-dates are not known is called a 94: 5532: 5404: 5141: 4988: 4277: 4168: 4064: 4059: 2099: 1185: 166: 3522: 3095: 298:

would affect climate patterns on earth, which would subsequently be recorded by tree-ring growth patterns (

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cells in tree ring analysis. They are formed when air temperature falls below freezing during a period of

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In addition to dating, dendrochronology can also provide information as to the source of the panel. Many

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A typical form of the function of the wood ring width in accordance with the dendrochronological equation

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is added in each growing season, thickening the stem, existing branches and roots, to form a growth ring.

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The only recorded instance of a missing ring in oak trees occurred in the year 1816, also known as the "

1806:(Tucson, Arizona: University of Arizona Press, 2010), Chapter 3: History of Dendrochronology, pp. 28–42. 287: 5339: 2249: 1259:

a large structure was built with more than two hundred posts. The central oak post was felled in 95 BC.

1074:). Additional studies of European oak trees, such as the master sequence in Germany that dates back to 1018: 419:

and a long growing season result in a wide ring, while a drought year may result in a very narrow one.

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On the other hand, dendrochronology was applied to four paintings depicting the same subject, that of

275:(1841–1905) wrote that he had used patterns found in tree rings to predict droughts in 1882 and 1891. 108: 5522: 5280: 5256: 5251: 4438: 4178: 4119: 4089: 3959: 3747: 3399: 3348: 2864:

Sheppard, Paul R. (May 2010). "Dendroclimatology: extracting climate from trees: Dendroclimatology".

2779: 2552: 2413: 2362: 2264: 2179: 1632: 1578: 1173: 249: 160:, or one year, in the tree's life. As of 2020, securely dated tree-ring data for some regions in the 78: 55: 1156:

A portrait of Mary Queen of Scots, determined to date from the sixteenth century by dendrochronology

5537: 5366: 5261: 5204: 5179: 5169: 4944: 4841: 4831: 4658: 4639: 4010: 3954: 3827: 3795: 1849: 1256: 1188:. The results showed that the age of the wood was too late for any of them to have been painted by 208: 161: 5491: 5471: 5349: 5334: 5319: 5241: 5040: 5004: 4806: 4590: 4109: 4104: 3934: 3897: 3852: 3805: 3712: 3702: 3570: 3010: 2926: 2881: 2844: 2741: 2580: 2280: 1791: 1783: 1754: 1746: 1433: 1166: 1064: 935: 133: 124: 2156:Шведов, Ф. (Shvedov, F.) (1892) "Дерево, как летопись засух" (The tree as a record of drought), 1518: 1217:

The dating of buildings with wooden structures and components is also done by dendrochronology;

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Taft, W. Stanley; Mayer, James W.; Newman, Richard; Kuniholm, Peter Ian; Stulik, Dusan (2000).

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also exhibit similar seasonal patterns in the isotopes of carbon and oxygen in their spines (

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activity. They can be used in dendrochronology to indicate years that are colder than usual.

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Van der Plecht, J; Bronck Ramsey, C; Heaton, T. J.; Scott, E. M.; Talamo, S (August 2020).

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settlement in northern Greece by tying it to a spike in cosmogenic radiocarbon in 5259 BC.

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at known dates, are visible in trees rings and can fix the dating of a floating sequence.

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examined the effect of growing conditions on the shape of tree rings. They found that in

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IntCal20 is the 2020 "Radiocarbon Age Calibration Curve", which provides a calibrated

5511: 5246: 5164: 5159: 5110: 5100: 4861: 4740: 4604: 4510: 4470: 4423: 4262: 4234: 4099: 4037: 3976: 3971: 3780: 3732: 3574: 3124: 2885: 2745: 2584: 381: 253: 2284: 1838:(1954) "Queries and Answers: Query 145. — When was tree-ring analysis discovered?", 1795: 1758: 5324: 5122: 4836: 4811: 4796: 4762: 4722: 4618: 4453: 4149: 4139: 4124: 4094: 4017: 3993: 3907: 3872: 3837: 3752: 3727: 3683: 3059: 2967: 2598: 2541:"The IntCal20 Northern Hemisphere Radiocarbon Age Calibration Curve (0–55 cal kBP)" 1464: 1387: 1281: 1266:

in Dedham, Massachusetts. While the house had long been claimed to have been built

998: 186: 170: 42:. Each ring represents one year; the outside rings, near the bark, are the youngest 1618:"Tree ring dating using oxygen isotopes: a master chronology for central England" 1567:"Recent Developments in Calibration for Archaeological and Environmental Samples" 62:

in the 1890s. The markings indicating historical events were added in the 1920s.

5024: 4921: 4883: 4866: 4801: 4782: 4715: 4695: 4485: 4465: 4458: 4418: 4385: 3966: 3717: 1322: 1274: 1234: 983: 411: 174: 137: 35: 3514: 3210: 2792: 2719: 2663: 4791: 4786: 4681: 4480: 4475: 4201: 3822: 3556: 3494: 3489: 2426: 2401: 2375: 2339: 2276: 2223: 1538: 1472: 1454: 1252: 1230: 1039: 189:(c. 371 – c. 287 BC) first mentioned that the wood of trees has rings. In his 3152: 1149:. Wooden supports other than oak were rarely used by Netherlandish painters. 5481: 5461: 5194: 5154: 4891: 4700: 4363: 4341: 4242: 4184: 4084: 3929: 3800: 3666: 3361: 3336: 1395: 1238: 1023: 1010: 971: 4613: 3429: 3411: 2811: 2737: 1458: 30: 17: 3292: 1505:

The term "dendrochronology" was coined in 1928 by the American astronomer

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have turned out to be painted on panels of "Baltic oak" shipped from the

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Dendrochronology has become important to art historians in the dating of

1107: 1035: 241: 3565: 3371: 2634: 2575: 2565: 2540: 2436: 2385: 1974:"On the age of strata, as inferred from rings of trees embedded in them" 1721: 1601: 1591: 1566: 116: 5486: 4710: 4705: 4599: 4433: 4329: 4299: 4294: 4282: 4272: 4257: 3810: 3014: 2930: 2122:

Seckendorff, Arthur von (1881) "Beiträge zur Kenntnis der Schwarzföhre

1992: 1787: 1779: 1750: 1742: 1686: 1444: 1246: 1146: 1138: 1130: 1099: 1081:, can also be used to back up and further calibrate radiocarbon dates. 1043: 934:

The formula is useful for correct approximation of samples data before

451: 39: 1284:, who died c. 958, was constructed from wood of timbers felled in 958. 1034:

Frost ring is a term used to designate a layer of deformed, collapsed

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Video & commentary on medullary rays, heart wood, and tree rings.

2517:. Switzerland: ETH Forest Snow and Landscape Research. Archived from 2175: 1988: 1729:

Studhalter, R. A. (1955). "Tree Growth I. Some Historical Chapters".

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Medieval Scandinavia: from conversion to Reformation, circa 800–1500

2829:(7th ed.). London, WCIV 7QX: Thames & Hudson. p. 144. 2351:

Age Matching of the German Oak and US Bristlecone Pine Chronologies"

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Stuiver, Minze; Kromer, Bernd; Becker, Bernd; Ferguson, C W (1986).

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showing idealised vertical and horizontal sections. A new layer of

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Fletcher, John (1982). "Panel Examination and Dendrochronology".

2196:(2nd ed.). Portland, OR: Timber Publishing. pp. 66–67. 1137:. Oak panels were used in a number of northern countries such as 4845: 4727: 4378: 4353: 4027: 3519: 2012:( August 6, 1859) "Das Klima von Texas" (The climate of Texas), 1707:

Studhalter, R. A. (April 1956). "Early History of Crossdating".

1165:

of the trunk. Consequently, dating studies usually result in a "

1103: 958:, for before present, where "present" refers to 1 January 1950. 365: 349: 345: 331: 152: 27:

Method of dating based on the analysis of patterns of tree rings

4654: 3585: 3531: 990:

long distances, such as panels for paintings and ship timbers.

278:

During the first half of the twentieth century, the astronomer

4745: 3509: 1316: 428: 424: 252:-Gudent (1845–1886) was using crossdating. From 1869 to 1901, 227: 4650: 2340:"Radiocarbon Age Calibration back to 13,300 Years BP and the 1848:(4): 383–384. Sarton also cites a diary of the French writer 122: 106: 92: 3495:

Video & commentary on Tree Rings – Formation and Purpose

3052:"Tree Rings, the Barcodes of Nature, Illuminate Art History" 314:

Drill for dendrochronology sampling and growth ring counting

3581: 2701:"Evidence for European presence in the Americas in AD 1021" 946:) of annual growth of wood ring are shown in the figures. 3510:

Digital Collaboratory for Cultural Dendrochronology (DCCD)

3170:

Brunning, Richard (February 2001). "The Somerset Levels".

58:. The tree was over 500 years old when it was cut down in 2402:"Dendrochronology of Bristlecone Pine: A Progress Report" 2128:

Mitteilung aus dem forstlichen Versuchswesen Oesterreichs

2048:, vol. 1, (Berlin, (Germany): Nicolaische Verlag, 1866), 1540:

The Science of Tree Rings: Principles of Dendrochronology

2968:"Dendrochronology (Tree-Ring Dating) of Panel Paintings" 1543:, Department of Geography, The University of Tennessee, 400:

The rings are more visible in trees which have grown in

169:, the southwestern United States and the British Isles. 3323: 3532:

Laboratory of Tree-Ring Research University of Arizona

3279: 2946:

Dendrochronology (Tree-Ring Dating) of Panel Paintings

2489:(4th ed.). London: Thames & Hudson. pp. 2130:(Vienna, Austria: Carl Gerold Verlag, 1881), 66 pages. 144:. It is also used as a check in radiocarbon dating to 3337:"Data Management in Dendroarchaeology Using Tellervo" 653: 494: 3483:

Dendrochronology and Art History of Painted Ceilings

3174:. XV (4) (172 (Special issue on Wetlands)): 139–143. 323:"Tree ring" redirects here. Not to be confused with 5454: 5438: 5422: 5380: 5290: 5279: 5234: 5226:

Global Boundary Stratotype Section and Point (GSSP)

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(12 August 2020). 1488:Timeline of dendrochronology timestamp events 1059:Dates from dendrochronology can be used as a 376:. Growth rings result from new growth in the 368:can reveal growth rings, also referred to as 8: 2160:(Meteorological Herald), (5) : 163–178. 1863:du Hamel & de Buffon (27 February 1737) 3211:"A Grand House in 17th-Century New England" 2827:Archaeology: Theories, Methods and Practice 2485:Archaeology: Theories, Methods and Practice 1351:. Unsourced material may be challenged and 5287: 5184: 4963: 4758: 4673: 4659: 4651: 3604: 3590: 3582: 2899:English Heritage Guide to Dendrochronology 2766:David Montwé; et al. (Apr 23, 2018). 2224:"Useful Tree Species for Tree-Ring Dating" 2104:Recueil des Travaux Botaniques Néerlandais 1985:The Ninth Bridgewater Treatise: A Fragment 1910:Histoire de l'Académie royale des sciences 1882:Histoire de l'Académie royale des sciences 1703:For the history of dendrochronology, see: 1532: 1530: 1401:. Similar seasonal patterns also occur in 642:) is function of mass growth of the tree. 3564: 3505:Multilingual Glossary of Dendrochronology 3419: 3370: 3360: 3293:"TRiDaS 1.1: The tree-ring data standard" 3237:"The Royal Lineage – The Danish Monarchy" 2801: 2791: 2727: 2574: 2564: 2435: 2425: 2400:Ferguson, C. W.; Graybill, D. A. (1983). 2384: 2374: 1906:Mémoires de l'Académie royale des science 1878:Mémoires de l'Académie royale des science 1720: 1644: 1600: 1590: 1371:Learn how and when to remove this message 1249:, have been dated to 3838 BC and 3807 BC. 1201:transferred onto canvas or other supports 870: 854: 846: 836: 818: 810: 800: 787: 766: 756: 736: 728: 718: 700: 692: 682: 675: 652: 564: 549: 548: 534: 529: 523: 513: 493: 5221:Global Standard Stratigraphic Age (GSSA) 2100:"Tree-growth and meteorological factors" 309: 226:(1823–1893) used crossdating to examine 2919:Harvard University Art Museums Bulletin 2455:. Moscow: SSO Foundation. p. 583. 1677:Theophrastus with Arthur Hort, trans., 1498: 290:. Douglass sought to better understand 3485:(Historic Environment Scotland, 2017). 3472:Nottingham Tree-Ring Dating Laboratory 2842: 1893:du Hamel & de Buffon (4 May 1737) 1658: 1656: 388:; this growth in diameter is known as 1547:from the original on November 4, 2016 7: 1689:: William Heinemann, 1916), Book V, 1349:adding citations to reliable sources 302:, sunspots → climate → tree rings). 4529: 3291:Jansma, Esther (30 November 2009). 3267:"Я послал тебе бересту (Янин В.Л.)" 3217:from the original on March 16, 2012 3213:. Fairbanks House Historical Site. 3133:. The Nordic Series. Vol. 17. 2825:Renfrew, Colin; Bahn, Paul (2016). 1098:is the science of determining past 414:cross section showing annual rings. 50:A "tree cookie" cross-section of a 5020:Adoption of the Gregorian calendar 2515:"Bibliography of Dendrochronology" 2307:"5.2.3 Dendrochronological Series" 1995:: John Murray, 1837), pp. 226-234. 1804:Fundamentals of Tree-ring Research 1663:University of Bern (21 May 2024). 654: 495: 238:Julius Theodor Christian Ratzeburg 25: 3878:Global Forest Information Service 3515:International Tree-Ring Data Bank 3050:Läänelaid, Alar (June 19, 2013). 2605:. London: Batsford. p. 124. 2481:Renfrew Colin; Bahn Paul (2004). 2019:"The droughts of western Texas", 1537:Grissino-Mayer, Henri D. (n.d.), 1478:International Tree-Ring Data Bank 1178:National Portrait Gallery, London 4634: 4625: 4624: 4612: 4598: 4584: 4570: 4556: 4542: 4528: 3500:Bibliography of Dendrochronology 3446: 3187:Navan Fort: Archaeology and Myth 3159:from the original on 2015-05-18. 3106:from the original on 2013-11-23. 3084:from the original on 2013-10-17. 3058:. Il Sole 24 Ore. Archived from 3039:from the original on 2013-10-17. 3003:The J. Paul Getty Museum Journal 2990:from the original on 2017-04-22. 2755:from the original on 2022-10-09. 2675:Price, Michael (13 April 2023). 2327:from the original on 2016-11-28. 2294:from the original on 2022-10-09. 1956:"Evening meeting at the Rotunda" 1457: 1321: 967:a little over 11,000 years B.P. 284:Laboratory of Tree-Ring Research 4902:English and British regnal year 4635: 3305:from the original on 2011-04-28 2230:from the original on 2008-11-08 1935:The American Journal of Science 1514:Climatic Cycles and Tree Growth 1439:A similar technique is used to 205:Georges-Louis Leclerc de Buffon 2976:. Springer. pp. 206–215. 2451:Alexandr N. Tetearing (2012). 1055:Radiocarbon dating calibration 666: 660: 581: 575: 507: 501: 201:Henri-Louis Duhamel du Monceau 34:The growth rings of a tree at 1: 5015:Old Style and New Style dates 3135:University of Minnesota Press 1625:Journal of Quaternary Science 1267: 1127:Early Netherlandish paintings 1075: 1068: 384:that botanists classify as a 325:Tree ring (landscape feature) 294:and reasoned that changes in 4967:Pre-Julian / Julian 3520:Ultimate Tree-Ring Web Pages 3392:Philosophical Transactions A 3096:"Panel Paintings Initiative" 1921:Alexander C. Twining (1833) 466:Dendrochronological equation 380:, a layer of cells near the 173:, which are major spikes in 115: 101: 87: 5200:Geological history of Earth 5070:Astronomical year numbering 3477:Oxford Tree-Ring Laboratory 2633:(in Danish). Archived from 2178:) or in autumn, as in some 2016:(San Antonio, Texas), p. 2. 1824:... (Rome, (Italy): 1817), 5564: 3989:Growth and yield modelling 2793:10.1038/s41467-018-04039-5 2720:10.1038/s41586-021-03972-8 2664:10.1038/s41467-024-48402-1 2629:[WM Tree dating]. 2021:The Texas Almanac for 1861 1386:is the analysis of annual 1210: 1088: 329: 322: 292:cycles of sunspot activity 258:Fedor Nikiforovich Shvedov 146:calibrate radiocarbon ages 123: 107: 93: 5372:Thermoluminescence dating 5267:Samarium–neodymium dating 4563:Earth sciences portal 4549:Climate change portal 4524: 4130:Great Green Wall (Africa) 3619: 3557:10.3959/1536-1098-62.2.51 3335:Brewer, Peter W. (2014). 3189:. Spain: Wordwell Books. 3033:National Portrait Gallery 2427:10.1017/S0033822200005592 2376:10.1017/S0033822200060252 2311:Quaternary Dating Methods 2277:10.1017/S003382220003304X 2158:Метеорологический Вестник 2023:, pp. 136–137 ; see 619:is width of annual ring, 5086:Chinese sexagenary cycle 4135:Great Green Wall (China) 3708:Close to nature forestry 2973:The Science of Paintings 2849:: CS1 maint: location ( 2077:The Elements of Forestry 1507:Andrew Ellicott Douglass 1441:estimate the age of fish 1133:region via ports of the 931:are positive constants. 213:Alexander Catlin Twining 195:(Treatise on Painting), 5300:Amino acid racemisation 4169:Million Tree Initiative 3362:10.2458/azu_rc.56.18320 2313:. John Wiley and Sons. 2144:Speer (2010), p. 36–37. 1972:Charles Babbage (1838) 1511:Douglass, A.E. (1928). 917:are some coefficients, 113:), meaning "time", and 5305:Archaeomagnetic dating 4817:Era of Caesar (Iberia) 4591:Environment portal 4023:Sustainable management 3918:Trillion Tree Campaign 3412:10.1098/rsta.2022.0206 3029:"Mary, Queen of Scots" 2222:Lori Martinez (1996). 2098:Kapteyn, J. C. (1914) 1822:Trattato della Pittura 1280:The burial chamber of 1157: 1001:, such as the ones in 888: 607: 483: 475: 415: 353: 315: 192:Trattato della Pittura 63: 54:tree displayed in the 43: 5205:Geological time units 4516:Wood process engineer 4220:Urban forest inequity 2772:Nature Communications 2453:Theory of populations 2305:Walker, Mike (2013). 2218:Year Without a Summer 2192:Capon, Brian (2005). 1928:May 14, 2015, at the 1155: 1061:calibration and check 889: 634:is some coefficient, 608: 481: 473: 410: 339: 330:Further information: 313: 288:University of Arizona 209:1709, a severe winter 49: 33: 5257:Law of superposition 5252:Isotope geochemistry 4179:Shifting cultivation 4120:Forest fragmentation 4090:Carbon sequestration 3960:Woodland Carbon Code 3925:Forest certification 3833:Even-aged management 3748:Sustainable forestry 3185:Lynn, Chris (2003). 3078:The National Gallery 3035:. Dendrochronology. 2943:Peter Ian Kuniholm, 2603:A Slice Through Time 2194:Botany for Gardeners 2163:Speer (2010), p. 37. 2133:Speer (2010), p. 36. 2044:J. T. C. Ratzeburg, 2014:Texas Staats-Zeitung 1345:improve this section 1313:Related chronologies 1174:Mary, Queen of Scots 651: 627:is density of wood, 623:is time (in years), 492: 56:Royal Ontario Museum 5518:American inventions 5390:Fluorine absorption 5367:Luminescence dating 5262:Luminescence dating 5170:Milankovitch cycles 5010:Proleptic Gregorian 4842:Hindu units of time 3984:Formally designated 3828:Ecological thinning 3738:Plantation forestry 3646:Research institutes 3537:"Tree Ring Science" 3404:2023RSPTA.38120206B 3353:2014Radcb..56S..79B 3172:Current Archaeology 2784:2018NatCo...9.1574M 2637:on 21 December 2014 2566:10.1017/RDC.2020.41 2557:2020Radcb..62..725R 2418:1983Radcb..25..287F 2367:1986Radcb..28..969S 2269:2004Radcb..46.1111F 1850:Michel de Montaigne 1820:Leonardo da Vinci, 1679:Enquiry into Plants 1637:2019JQS....34..475L 1592:10.1017/RDC.2020.22 1583:2020Radcb..62.1095V 1434:paleoclimatologists 1304:Continuous sequence 1257:Prehistoric Ireland 978:Reference sequences 950:Sampling and dating 445:floating chronology 185:The Greek botanist 162:Northern Hemisphere 129:), "the study of". 99:), meaning "tree", 5543:Incremental dating 5492:Terminus post quem 5472:Synchronoptic view 5439:Linguistic methods 5400:Obsidian hydration 5335:Radiometric dating 5320:Incremental dating 5242:Chronostratigraphy 4577:Ecology portal 4110:Forest degradation 4105:Ecosystem services 3713:Community forestry 3545:Tree-Ring Research 3525:2013-08-07 at the 3456:has a profile for 3074:"Dendrochronology" 2956:Cornell University 2952:2013-10-17 at the 2904:2013-10-23 at the 2086:2015-10-01 at the 2055:2015-10-01 at the 2030:2015-11-02 at the 2025:especially p. 137. 1979:2015-05-15 at the 1961:2015-05-14 at the 1900:2015-05-09 at the 1872:2015-05-09 at the 1780:10.1007/BF02860823 1743:10.1007/BF02872376 1709:Tree-Ring Bulletin 1167:terminus post quem 1158: 1065:radiocarbon dating 1019:L'Anse aux Meadows 936:data normalization 884: 603: 484: 476: 416: 354: 316: 134:radiocarbon dating 64: 44: 5505: 5504: 5418: 5417: 5275: 5274: 5136: 5135: 5091:Geologic Calendar 4953: 4952: 4648: 4647: 4605:Plants portal 4391:green woodworking 3462: 3459:dendrochronology 3196:978-1-869857-67-7 3144:978-0-8166-1739-5 2983:978-0-387-98722-4 2836:978-0-500-29210-5 2714:(7893): 388–391. 2612:978-0-7134-7654-5 2500:978-0-500-28441-4 2462:978-1-365-56080-4 2203:978-0-88192-655-2 2073:Franklin B. Hough 1884:..., pp. 121–134. 1727:(Condensed from: 1430:acanthochronology 1399:herbaceous plants 1381: 1380: 1373: 1219:dendroarchaeology 1213:Dendroarchaeology 1096:Dendroclimatology 1091:dendroclimatology 882: 878: 774: 598: 572: 546: 542: 197:Leonardo da Vinci 83:dendroclimatology 75:scientific method 52:Coast Douglas-fir 16:(Redirected from 5555: 5497:ASPRO chronology 5446:Glottochronology 5362:Tephrochronology 5310:Dendrochronology 5288: 5185: 4984:Proleptic Julian 4974:Pre-Julian Roman 4964: 4759: 4675: 4668: 4661: 4652: 4638: 4637: 4628: 4627: 4619:Trees portal 4617: 4616: 4603: 4602: 4589: 4588: 4575: 4574: 4573: 4561: 4560: 4559: 4547: 4546: 4545: 4532: 4531: 4253:Forest gardening 4210:Timber recycling 4157:Invasive species 4045:Tree measurement 3606: 3599: 3592: 3583: 3578: 3568: 3460: 3450: 3449: 3434: 3433: 3423: 3383: 3377: 3376: 3374: 3364: 3332: 3326: 3324:Tellervo website 3321: 3315: 3314: 3312: 3310: 3304: 3297: 3288: 3282: 3277: 3271: 3270: 3263: 3257: 3256: 3254: 3252: 3243:. Archived from 3233: 3227: 3226: 3224: 3222: 3207: 3201: 3200: 3182: 3176: 3175: 3167: 3161: 3160: 3117: 3108: 3107: 3092: 3086: 3085: 3070: 3064: 3063: 3047: 3041: 3040: 3025: 3019: 3018: 2998: 2992: 2991: 2963: 2957: 2941: 2935: 2934: 2914: 2908: 2896: 2890: 2889: 2861: 2855: 2854: 2848: 2840: 2822: 2816: 2815: 2805: 2795: 2763: 2757: 2756: 2754: 2731: 2705: 2696: 2690: 2689: 2672: 2666: 2656: 2647: 2646: 2644: 2642: 2627:"WM Trædatering" 2623: 2617: 2616: 2595: 2589: 2588: 2578: 2568: 2536: 2530: 2529: 2527: 2526: 2511: 2505: 2504: 2488: 2478: 2467: 2466: 2448: 2442: 2441: 2439: 2429: 2397: 2391: 2390: 2388: 2378: 2350: 2348: 2347: 2335: 2329: 2328: 2302: 2296: 2295: 2293: 2263:(3): 1111–1122. 2254: 2245: 2239: 2238: 2236: 2235: 2214: 2208: 2207: 2189: 2183: 2172: 2166: 2151: 2145: 2142: 2136: 2117: 2111: 2096: 2090: 2070: 2064: 2042: 2036: 2004: 1998: 1949: 1943: 1942: : 391–393. 1919: 1913: 1891: 1885: 1861: 1855: 1815: 1809: 1802:James H. Speer, 1799: 1768:Botanical Review 1762: 1731:Botanical Review 1726: 1724: 1701: 1695: 1675: 1669: 1668: 1660: 1651: 1650: 1648: 1646:10.1002/jqs.3115 1622: 1613: 1607: 1606: 1604: 1594: 1577:(4): 1095–1117. 1562: 1556: 1555: 1554: 1552: 1534: 1525: 1522: 1503: 1467: 1462: 1461: 1417:is the study of 1415:Sclerochronology 1376: 1369: 1365: 1362: 1356: 1325: 1317: 1272: 1269: 1239:timber trackways 1190:Hieronymus Bosch 1135:Hanseatic League 1080: 1077: 1073: 1070: 964:bristlecone pine 893: 891: 890: 885: 883: 881: 880: 879: 871: 869: 865: 864: 863: 859: 858: 841: 840: 828: 827: 823: 822: 805: 804: 792: 791: 776: 775: 767: 761: 760: 747: 746: 745: 741: 740: 723: 722: 710: 709: 705: 704: 687: 686: 676: 612: 610: 609: 604: 599: 597: 589: 588: 584: 574: 573: 565: 550: 547: 545: 544: 543: 535: 528: 527: 514: 462:of California). 390:secondary growth 386:lateral meristem 378:vascular cambium 360:cut through the 342:secondary growth 274: 233:Quercus stellata 128: 127: 120: 112: 111: 104: 98: 97: 90: 71:tree-ring dating 67:Dendrochronology 60:British Columbia 21: 5563: 5562: 5558: 5557: 5556: 5554: 5553: 5552: 5508: 5507: 5506: 5501: 5450: 5434: 5430:Molecular clock 5423:Genetic methods 5414: 5395:Nitrogen dating 5382:Relative dating 5376: 5345:Potassium–argon 5292:Absolute dating 5282: 5271: 5230: 5209: 5174: 5150:Cosmic Calendar 5142:Astronomic time 5132: 5074: 5029: 4993: 4979:Original Julian 4949: 4916: 4878: 4777:Ab urbe condita 4755: 4732: 4684: 4679: 4649: 4644: 4611: 4597: 4583: 4571: 4569: 4557: 4555: 4543: 4541: 4520: 4397: 4374:spruce-pine-fir 4347:Christmas trees 4229: 4145:Illegal logging 4077: 4071: 3786:Controlled burn 3771: 3762: 3743:Social forestry 3723:Energy forestry 3703:Bamboo forestry 3698:Analog forestry 3672: 3615: 3610: 3542: 3527:Wayback Machine 3468: 3467: 3466: 3451: 3447: 3442: 3437: 3385: 3384: 3380: 3334: 3333: 3329: 3322: 3318: 3308: 3306: 3302: 3295: 3290: 3289: 3285: 3278: 3274: 3265: 3264: 3260: 3250: 3248: 3235: 3234: 3230: 3220: 3218: 3209: 3208: 3204: 3197: 3184: 3183: 3179: 3169: 3168: 3164: 3145: 3119: 3118: 3111: 3094: 3093: 3089: 3072: 3071: 3067: 3056:Atomium Culture 3049: 3048: 3044: 3027: 3026: 3022: 3000: 2999: 2995: 2984: 2965: 2964: 2960: 2954:Wayback Machine 2942: 2938: 2916: 2915: 2911: 2906:Wayback Machine 2897: 2893: 2863: 2862: 2858: 2841: 2837: 2824: 2823: 2819: 2765: 2764: 2760: 2752: 2703: 2698: 2697: 2693: 2674: 2673: 2669: 2657: 2650: 2640: 2638: 2625: 2624: 2620: 2613: 2597: 2596: 2592: 2538: 2537: 2533: 2524: 2522: 2513: 2512: 2508: 2501: 2480: 2479: 2470: 2463: 2450: 2449: 2445: 2399: 2398: 2394: 2361:(2B): 969–979. 2346: 2344: 2343: 2342: 2341: 2337: 2336: 2332: 2321: 2304: 2303: 2299: 2291: 2252: 2247: 2246: 2242: 2233: 2231: 2221: 2215: 2211: 2204: 2191: 2190: 2186: 2173: 2169: 2152: 2148: 2143: 2139: 2124:Pinus austriaca 2118: 2114: 2097: 2093: 2088:Wayback Machine 2071: 2067: 2057:Wayback Machine 2043: 2039: 2032:Wayback Machine 2005: 2001: 1981:Wayback Machine 1963:Wayback Machine 1954:(Anon.) 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4948: 4947: 4942: 4937: 4932: 4926: 4924: 4918: 4917: 4915: 4914: 4909: 4907:Lists of kings 4904: 4899: 4897:Canon of Kings 4894: 4888: 4886: 4880: 4879: 4877: 4876: 4875: 4874: 4869: 4864: 4859: 4849: 4839: 4834: 4829: 4824: 4822:Before present 4819: 4814: 4809: 4804: 4799: 4794: 4789: 4780: 4773: 4767: 4765: 4756: 4754: 4753: 4748: 4743: 4737: 4734: 4733: 4731: 4730: 4725: 4720: 4719: 4718: 4708: 4703: 4698: 4692: 4690: 4686: 4685: 4680: 4678: 4677: 4670: 4663: 4655: 4646: 4645: 4643: 4642: 4632: 4622: 4608: 4594: 4580: 4566: 4552: 4538: 4525: 4522: 4521: 4519: 4518: 4513: 4508: 4506:Timber cruiser 4503: 4501:Shingle weaver 4498: 4493: 4488: 4483: 4478: 4473: 4468: 4463: 4462: 4461: 4456: 4451: 4446: 4436: 4431: 4426: 4421: 4416: 4411: 4405: 4403: 4399: 4398: 4396: 4395: 4394: 4393: 4383: 4382: 4381: 4376: 4371: 4366: 4361: 4351: 4350: 4349: 4339: 4337:Rail transport 4334: 4333: 4332: 4327: 4322: 4317: 4312: 4307: 4302: 4297: 4287: 4286: 4285: 4280: 4278:pulp and paper 4275: 4270: 4260: 4255: 4250: 4248:Forest farming 4245: 4239: 4237: 4231: 4230: 4228: 4227: 4222: 4217: 4212: 4207: 4206: 4205: 4198: 4196:slash-and-char 4193: 4191:slash-and-burn 4188: 4176: 4171: 4166: 4165: 4164: 4154: 4153: 4152: 4142: 4137: 4132: 4127: 4122: 4117: 4115:Forest dieback 4112: 4107: 4102: 4097: 4092: 4087: 4081: 4079: 4073: 4072: 4070: 4069: 4068: 4067: 4062: 4057: 4052: 4042: 4041: 4040: 4035: 4025: 4020: 4015: 4014: 4013: 4003: 4002: 4001: 3991: 3986: 3981: 3980: 3979: 3974: 3964: 3963: 3962: 3957: 3952: 3947: 3942: 3937: 3932: 3922: 3921: 3920: 3915: 3910: 3905: 3900: 3895: 3890: 3885: 3880: 3875: 3870: 3865: 3860: 3855: 3850: 3840: 3835: 3830: 3825: 3820: 3819: 3818: 3813: 3808: 3803: 3798: 3788: 3783: 3777: 3775: 3764: 3763: 3761: 3760: 3758:Urban forestry 3755: 3750: 3745: 3740: 3735: 3730: 3725: 3720: 3715: 3710: 3705: 3700: 3695: 3694: 3693: 3680: 3678: 3674: 3673: 3671: 3670: 3663: 3656: 3649: 3642: 3635: 3628: 3620: 3617: 3616: 3611: 3609: 3608: 3601: 3594: 3586: 3580: 3579: 3540: 3534: 3529: 3517: 3512: 3507: 3502: 3497: 3492: 3487: 3479: 3474: 3452: 3445: 3444: 3443: 3441: 3440:External links 3438: 3436: 3435: 3378: 3347:(4): S79–S83. 3327: 3316: 3283: 3280:TRiDaS website 3272: 3258: 3247:on 6 July 2015 3228: 3202: 3195: 3177: 3162: 3143: 3125:Sawyer, Birgit 3109: 3087: 3065: 3062:on 2013-10-18. 3042: 3020: 2993: 2982: 2958: 2936: 2909: 2891: 2878:10.1002/wcc.42 2872:(3): 343–352. 2856: 2835: 2817: 2758: 2691: 2667: 2648: 2618: 2611: 2590: 2551:(4): 725–757. 2531: 2506: 2499: 2468: 2461: 2443: 2412:(2): 287–288. 2392: 2345: 2330: 2319: 2297: 2240: 2209: 2202: 2184: 2167: 2165: 2164: 2161: 2146: 2137: 2135: 2134: 2131: 2112: 2110: : 70–93. 2091: 2065: 2037: 2035: 2034: 2017: 2010:Jacob Kuechler 1999: 1997: 1996: 1970: 1969:, pp. 116–117. 1944: 1914: 1886: 1856: 1854: 1853: 1836:Sarton, George 1833: 1810: 1808: 1807: 1800: 1774:(3): 245–365. 1763: 1696: 1670: 1652: 1631:(6): 475–490. 1608: 1557: 1526: 1509:(1867–1962). 1497: 1495: 1492: 1491: 1490: 1485: 1480: 1475: 1469: 1468: 1452: 1449: 1424:Some columnar 1384:Herbchronology 1379: 1378: 1329: 1327: 1320: 1314: 1311: 1305: 1302: 1296: 1293: 1292: 1291: 1285: 1278: 1260: 1250: 1211:Main article: 1208: 1205: 1172:A portrait of 1115: 1112: 1089:Main article: 1086: 1083: 1079: 8500 BC 1072: 6700 BC 1056: 1053: 1051: 1048: 1038:and traumatic 1031: 1028: 995: 992: 979: 976: 951: 948: 928: 921: 914: 907: 900: 877: 874: 868: 862: 857: 853: 849: 845: 839: 835: 831: 826: 821: 817: 813: 809: 803: 799: 795: 790: 786: 781: 773: 770: 765: 759: 755: 751: 744: 739: 735: 731: 727: 721: 717: 713: 708: 703: 699: 695: 691: 685: 681: 674: 671: 668: 665: 662: 659: 656: 630: 602: 596: 593: 587: 583: 580: 577: 571: 568: 563: 558: 554: 541: 538: 533: 526: 522: 517: 512: 509: 506: 503: 500: 497: 467: 464: 358:cross sections 320: 317: 307: 304: 296:solar activity 280:A. E. Douglass 224:Jacob Kuechler 182: 179: 151:New growth in 26: 24: 14: 13: 10: 9: 6: 4: 3: 2: 5560: 5549: 5546: 5544: 5541: 5539: 5536: 5534: 5531: 5529: 5526: 5524: 5521: 5519: 5516: 5515: 5513: 5498: 5495: 5493: 5490: 5488: 5485: 5483: 5480: 5478: 5475: 5473: 5470: 5468: 5465: 5463: 5460: 5459: 5457: 5453: 5447: 5444: 5443: 5441: 5437: 5431: 5428: 5427: 5425: 5421: 5411: 5408: 5406: 5403: 5401: 5398: 5396: 5393: 5391: 5388: 5387: 5385: 5383: 5379: 5373: 5370: 5368: 5365: 5363: 5360: 5356: 5353: 5351: 5348: 5346: 5343: 5341: 5338: 5337: 5336: 5333: 5331: 5328: 5326: 5323: 5321: 5318: 5316: 5313: 5311: 5308: 5306: 5303: 5301: 5298: 5297: 5295: 5293: 5289: 5286: 5284: 5281:Chronological 5278: 5268: 5265: 5263: 5260: 5258: 5255: 5253: 5250: 5248: 5247:Geochronology 5245: 5243: 5240: 5239: 5237: 5233: 5227: 5224: 5222: 5219: 5218: 5216: 5212: 5206: 5203: 5201: 5198: 5196: 5193: 5192: 5190: 5186: 5183: 5181: 5180:Geologic time 5177: 5171: 5168: 5166: 5165:Metonic cycle 5163: 5161: 5160:Galactic year 5158: 5156: 5153: 5151: 5148: 5147: 5145: 5143: 5139: 5129: 5126: 5124: 5121: 5117: 5114: 5112: 5109: 5108: 5107: 5104: 5102: 5101:ISO week date 5099: 5097: 5094: 5092: 5089: 5087: 5084: 5083: 5081: 5077: 5071: 5068: 5065: 5061: 5058: 5056: 5053: 5050: 5046: 5042: 5039: 5038: 5036: 5032: 5026: 5023: 5021: 5018: 5016: 5013: 5011: 5008: 5006: 5003: 5002: 5000: 4996: 4990: 4987: 4985: 4982: 4980: 4977: 4975: 4972: 4971: 4969: 4965: 4962: 4960: 4956: 4946: 4943: 4941: 4938: 4936: 4933: 4931: 4928: 4927: 4925: 4923: 4919: 4913: 4910: 4908: 4905: 4903: 4900: 4898: 4895: 4893: 4890: 4889: 4887: 4885: 4881: 4873: 4870: 4868: 4865: 4863: 4860: 4858: 4855: 4854: 4853: 4850: 4847: 4843: 4840: 4838: 4835: 4833: 4830: 4828: 4825: 4823: 4820: 4818: 4815: 4813: 4810: 4808: 4807:Byzantine era 4805: 4803: 4800: 4798: 4795: 4793: 4790: 4788: 4784: 4781: 4779: 4778: 4774: 4772: 4769: 4768: 4766: 4764: 4763:Calendar eras 4760: 4757: 4752: 4749: 4747: 4744: 4742: 4739: 4738: 4735: 4729: 4726: 4724: 4721: 4717: 4714: 4713: 4712: 4709: 4707: 4704: 4702: 4699: 4697: 4694: 4693: 4691: 4687: 4683: 4676: 4671: 4669: 4664: 4662: 4657: 4656: 4653: 4641: 4633: 4631: 4623: 4621: 4620: 4615: 4609: 4607: 4606: 4601: 4595: 4593: 4592: 4587: 4581: 4579: 4578: 4567: 4565: 4564: 4553: 4551: 4550: 4539: 4537: 4536: 4527: 4526: 4523: 4517: 4514: 4512: 4509: 4507: 4504: 4502: 4499: 4497: 4496:Rubber tapper 4494: 4492: 4489: 4487: 4484: 4482: 4479: 4477: 4474: 4472: 4469: 4467: 4464: 4460: 4457: 4455: 4452: 4450: 4447: 4445: 4442: 4441: 4440: 4437: 4435: 4432: 4430: 4427: 4425: 4424:Choker setter 4422: 4420: 4417: 4415: 4412: 4410: 4407: 4406: 4404: 4400: 4392: 4389: 4388: 4387: 4384: 4380: 4377: 4375: 4372: 4370: 4367: 4365: 4362: 4360: 4357: 4356: 4355: 4352: 4348: 4345: 4344: 4343: 4340: 4338: 4335: 4331: 4328: 4326: 4323: 4321: 4318: 4316: 4313: 4311: 4308: 4306: 4303: 4301: 4298: 4296: 4293: 4292: 4291: 4288: 4284: 4281: 4279: 4276: 4274: 4271: 4269: 4266: 4265: 4264: 4263:Manufacturing 4261: 4259: 4256: 4254: 4251: 4249: 4246: 4244: 4241: 4240: 4238: 4236: 4232: 4226: 4223: 4221: 4218: 4216: 4213: 4211: 4208: 4204: 4203: 4199: 4197: 4194: 4192: 4189: 4187: 4186: 4182: 4181: 4180: 4177: 4175: 4172: 4170: 4167: 4163: 4160: 4159: 4158: 4155: 4151: 4148: 4147: 4146: 4143: 4141: 4138: 4136: 4133: 4131: 4128: 4126: 4123: 4121: 4118: 4116: 4113: 4111: 4108: 4106: 4103: 4101: 4100:Deforestation 4098: 4096: 4093: 4091: 4088: 4086: 4083: 4082: 4080: 4076:Environmental 4074: 4066: 4063: 4061: 4058: 4056: 4053: 4051: 4048: 4047: 4046: 4043: 4039: 4036: 4034: 4031: 4030: 4029: 4026: 4024: 4021: 4019: 4016: 4012: 4009: 4008: 4007: 4004: 4000: 3997: 3996: 3995: 3992: 3990: 3987: 3985: 3982: 3978: 3977:reforestation 3975: 3973: 3972:afforestation 3970: 3969: 3968: 3965: 3961: 3958: 3956: 3953: 3951: 3948: 3946: 3943: 3941: 3938: 3936: 3933: 3931: 3928: 3927: 3926: 3923: 3919: 3916: 3914: 3911: 3909: 3906: 3904: 3901: 3899: 3896: 3894: 3891: 3889: 3886: 3884: 3881: 3879: 3876: 3874: 3871: 3869: 3866: 3864: 3861: 3859: 3856: 3854: 3851: 3849: 3846: 3845: 3844: 3841: 3839: 3836: 3834: 3831: 3829: 3826: 3824: 3821: 3817: 3814: 3812: 3809: 3807: 3804: 3802: 3799: 3797: 3794: 3793: 3792: 3789: 3787: 3784: 3782: 3781:Arboriculture 3779: 3778: 3776: 3774: 3769: 3765: 3759: 3756: 3754: 3751: 3749: 3746: 3744: 3741: 3739: 3736: 3734: 3733:Permaforestry 3731: 3729: 3726: 3724: 3721: 3719: 3716: 3714: 3711: 3709: 3706: 3704: 3701: 3699: 3696: 3692: 3691: 3687: 3686: 3685: 3682: 3681: 3679: 3675: 3669: 3668: 3664: 3662: 3661: 3657: 3655: 3654: 3650: 3648: 3647: 3643: 3641: 3640: 3636: 3634: 3633: 3629: 3627: 3626: 3622: 3621: 3618: 3614: 3607: 3602: 3600: 3595: 3593: 3588: 3587: 3584: 3576: 3572: 3567: 3562: 3558: 3554: 3550: 3546: 3541: 3538: 3535: 3533: 3530: 3528: 3524: 3521: 3518: 3516: 3513: 3511: 3508: 3506: 3503: 3501: 3498: 3496: 3493: 3491: 3488: 3486: 3484: 3480: 3478: 3475: 3473: 3470: 3469: 3464: 3463: 3455: 3439: 3431: 3427: 3422: 3417: 3413: 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2678: 2671: 2668: 2665: 2661: 2655: 2653: 2649: 2636: 2632: 2628: 2622: 2619: 2614: 2608: 2604: 2600: 2594: 2591: 2586: 2582: 2577: 2572: 2567: 2562: 2558: 2554: 2550: 2546: 2542: 2535: 2532: 2521:on 2010-08-04 2520: 2516: 2510: 2507: 2502: 2496: 2492: 2487: 2486: 2477: 2475: 2473: 2469: 2464: 2458: 2454: 2447: 2444: 2438: 2433: 2428: 2423: 2419: 2415: 2411: 2407: 2403: 2396: 2393: 2387: 2382: 2377: 2372: 2368: 2364: 2360: 2356: 2352: 2334: 2331: 2326: 2322: 2320:9781118700099 2316: 2312: 2308: 2301: 2298: 2290: 2286: 2282: 2278: 2274: 2270: 2266: 2262: 2258: 2251: 2244: 2241: 2229: 2225: 2219: 2213: 2210: 2205: 2199: 2195: 2188: 2185: 2181: 2180:Mediterranean 2177: 2171: 2168: 2162: 2159: 2155: 2154: 2150: 2147: 2141: 2138: 2132: 2129: 2125: 2121: 2120: 2116: 2113: 2109: 2105: 2101: 2095: 2092: 2089: 2085: 2082: 2078: 2074: 2069: 2066: 2062: 2058: 2054: 2051: 2047: 2041: 2038: 2033: 2029: 2026: 2022: 2018: 2015: 2011: 2008: 2007: 2003: 2000: 1994: 1990: 1986: 1982: 1978: 1975: 1971: 1968: 1964: 1960: 1957: 1953: 1952: 1948: 1945: 1941: 1937: 1936: 1931: 1927: 1924: 1918: 1915: 1911: 1907: 1903: 1899: 1896: 1890: 1887: 1883: 1879: 1875: 1871: 1868: 1867: 1860: 1857: 1851: 1847: 1843: 1842: 1837: 1834: 1831: 1828:From p. 396: 1827: 1823: 1819: 1818: 1814: 1811: 1805: 1801: 1797: 1793: 1789: 1785: 1781: 1777: 1773: 1769: 1764: 1760: 1756: 1752: 1748: 1744: 1740: 1737:(1/3): 1–72. 1736: 1732: 1723: 1718: 1714: 1710: 1705: 1704: 1700: 1697: 1692: 1688: 1684: 1680: 1674: 1671: 1666: 1659: 1657: 1653: 1647: 1642: 1638: 1634: 1630: 1626: 1619: 1612: 1609: 1603: 1598: 1593: 1588: 1584: 1580: 1576: 1572: 1568: 1561: 1558: 1546: 1542: 1541: 1533: 1531: 1527: 1520: 1516: 1515: 1508: 1502: 1499: 1493: 1489: 1486: 1484: 1481: 1479: 1476: 1474: 1471: 1470: 1466: 1460: 1455: 1450: 1448: 1446: 1442: 1437: 1435: 1431: 1427: 1422: 1420: 1416: 1412: 1408: 1404: 1400: 1397: 1393: 1389: 1385: 1375: 1372: 1364: 1361:November 2014 1354: 1350: 1346: 1340: 1339: 1335: 1330:This section 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487: 480: 472: 465: 463: 461: 457: 453: 448: 446: 442: 438: 432: 430: 426: 420: 413: 409: 405: 403: 398: 395: 391: 387: 383: 379: 375: 371: 367: 363: 359: 351: 347: 343: 338: 333: 326: 318: 312: 305: 303: 301: 297: 293: 289: 285: 281: 276: 272: 268: 264: 259: 255: 254:Robert Hartig 251: 247: 243: 239: 235: 234: 229: 225: 220: 218: 214: 210: 206: 202: 198: 194: 193: 188: 180: 178: 176: 172: 171:Miyake events 168: 167:Northern Alps 163: 159: 154: 149: 147: 143: 139: 135: 130: 126: 119: 118: 110: 103: 96: 89: 84: 80: 76: 72: 68: 61: 57: 53: 48: 41: 37: 32: 19: 5548:Paleoecology 5410:Stratigraphy 5355:Uranium–lead 5325:Lichenometry 5309: 5123:Winter count 5106:Mesoamerican 5034:Astronomical 4852:Mesoamerican 4837:Sothic cycle 4812:Seleucid era 4797:Bosporan era 4785: / 4775: 4723:Paleontology 4610: 4596: 4582: 4568: 4554: 4540: 4533: 4511:Tree planter 4491:Resin tapper 4471:Truck driver 4466:River driver 4215:Tree hugging 4200: 4183: 4150:timber mafia 4140:High grading 4125:Ghost forest 4095:Clearcutting 4018:Silviculture 3994:Horticulture 3838:Fire ecology 3753:Urban forest 3728:Mycoforestry 3688: 3684:Agroforestry 3665: 3658: 3651: 3644: 3637: 3632:Forest areas 3630: 3623: 3566:10150/262645 3551:(2): 51–65. 3548: 3544: 3482: 3458: 3395: 3391: 3381: 3372:10150/630521 3344: 3340: 3330: 3319: 3307:. 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