RADIOCARBON WIGGLE-MATCHING OF JAPANESE HISTORICAL MATERIALS WITH A POSSIBLE SYSTEMATIC AGE OFFSET
Identifieur interne :
000058 ( Main/Corpus );
précédent :
000057;
suivant :
000059
RADIOCARBON WIGGLE-MATCHING OF JAPANESE HISTORICAL MATERIALS WITH A POSSIBLE SYSTEMATIC AGE OFFSET
Auteurs : Mineo Imamura ;
Hiromasa Ozaki ;
Takumi Mitsutani ;
Etsuko Niu ;
Shigeru ItohSource :
RBID : Francis:08-0357951
Descripteurs français
- Pascal (Inist)
- Datation,
Matériau,
Méthode,
Spectrométrie de masse,
Technique,
Dendrochronologie,
Bois,
Japon,
Calibration,
Radiocarbone,
Wiggle-matching.
English descriptors
Abstract
Progress in radiocarbon accelerator mass spectrometry (AMS) techniques enables much more access to wiggle-matching techniques for high-precision 14C dating with relatively low costs than before. Recently, we have applied wiggle-matching for a number of wood samples where dendrochronology is difficult because of various limitations imposed for dendro-dating. In most cases, wiggle-matching gave rather unambiguous calendar ages, but we found that in some cases the calibrated date was very sensitive to a systematic error of the 14C date. Here, we present a wooden artifact from the Ujishigai archaeological site as a case where the highest wiggle-matched date did not agree with the date given by dendrochronology. An age with lower probability agreed with the tree-ring age of AD 389, which marked the beginning of the production of Sue ware (unglazed stoneware) in Japan. We show that systematic errors must be carefully taken into account while interpreting 14C wiggle-matching results, whether they are due to instrumental errors (statistical) or due to a regional offset from the IntCal04 (Reimer et al. 2004) calibration curve.
Notice en format standard (ISO 2709)
Pour connaître la documentation sur le format Inist Standard.
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| A06 | | | | @2 2 |
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| A08 | 01 | 1 | ENG | @1 RADIOCARBON WIGGLE-MATCHING OF JAPANESE HISTORICAL MATERIALS WITH A POSSIBLE SYSTEMATIC AGE OFFSET |
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| A09 | 01 | 1 | ENG | @1 19th International Radiocarbon Conference, Keble College, Oxford, England. 3-7 April 2006 |
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| A11 | 01 | 1 | | @1 IMAMURA (Mineo) |
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| A11 | 02 | 1 | | @1 OZAKI (Hiromasa) |
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| A11 | 03 | 1 | | @1 MITSUTANI (Takumi) |
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| A11 | 04 | 1 | | @1 NIU (Etsuko) |
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| A11 | 05 | 1 | | @1 ITOH (Shigeru) |
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| A12 | 01 | 1 | | @1 RAMSEY (Christopher Bronk) @9 ed. |
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| A12 | 02 | 1 | | @1 HIGHAM (Thomas F. G.) @9 ed. |
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| A14 | 01 | | | @1 National Museum of Japanese History, The National Institute for Humanities, 117 Jonai-cho @2 Sakura-shi, Chiba 285-8502 @3 JPN @Z 1 aut. @Z 2 aut. |
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| A14 | 02 | | | @1 National Research Institute for Cultural Properties, Nara, 2-9-1 Nijo-cho @2 Nara-shi, Nara 630-8577 @3 JPN @Z 3 aut. |
|---|
| A14 | 03 | | | @1 Paleo-Labo Co. Ltd., 1900-65 Shimotazawa, Kurohone-cho @2 Kiryu-shi, Gunma 376-0144 @3 JPN @Z 4 aut. @Z 5 aut. |
|---|
| A15 | 01 | | | @1 Oxford Radiocarbon Accelerator Unit, Research Laboratory for Archaeology and the History of Art, Dyson Perrins Building, University of Oxford @2 Oxford OX1 3QY @3 GBR @Z 1 aut. |
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| A47 | 01 | 1 | | @0 08-0357951 |
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| A66 | 01 | | | @0 USA |
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| C01 | 01 | | ENG | @0 Progress in radiocarbon accelerator mass spectrometry (AMS) techniques enables much more access to wiggle-matching techniques for high-precision 14C dating with relatively low costs than before. Recently, we have applied wiggle-matching for a number of wood samples where dendrochronology is difficult because of various limitations imposed for dendro-dating. In most cases, wiggle-matching gave rather unambiguous calendar ages, but we found that in some cases the calibrated date was very sensitive to a systematic error of the 14C date. Here, we present a wooden artifact from the Ujishigai archaeological site as a case where the highest wiggle-matched date did not agree with the date given by dendrochronology. An age with lower probability agreed with the tree-ring age of AD 389, which marked the beginning of the production of Sue ware (unglazed stoneware) in Japan. We show that systematic errors must be carefully taken into account while interpreting 14C wiggle-matching results, whether they are due to instrumental errors (statistical) or due to a regional offset from the IntCal04 (Reimer et al. 2004) calibration curve. |
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| C03 | 02 | H | FRE | @0 Matériau @5 02 |
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| C03 | 02 | H | ENG | @0 Materials @5 02 |
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| C03 | 03 | H | FRE | @0 Méthode @5 03 |
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| C03 | 03 | H | ENG | @0 Method @5 03 |
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| C03 | 04 | H | FRE | @0 Spectrométrie de masse @5 04 |
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| C03 | 04 | H | ENG | @0 Mass spectrometry @5 04 |
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| C03 | 10 | A | ENG | @0 Radiocarbon @2 NI @2 FM @5 18 |
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| pR |
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Format Inist (serveur)
| NO : | FRANCIS 08-0357951 INIST |
|---|
| ET : | RADIOCARBON WIGGLE-MATCHING OF JAPANESE HISTORICAL MATERIALS WITH A POSSIBLE SYSTEMATIC AGE OFFSET |
|---|
| AU : | IMAMURA (Mineo); OZAKI (Hiromasa); MITSUTANI (Takumi); NIU (Etsuko); ITOH (Shigeru); RAMSEY (Christopher Bronk); HIGHAM (Thomas F. G.) |
|---|
| AF : | National Museum of Japanese History, The National Institute for Humanities, 117 Jonai-cho/Sakura-shi, Chiba 285-8502/Japon (1 aut., 2 aut.); National Research Institute for Cultural Properties, Nara, 2-9-1 Nijo-cho/Nara-shi, Nara 630-8577/Japon (3 aut.); Paleo-Labo Co. Ltd., 1900-65 Shimotazawa, Kurohone-cho/Kiryu-shi, Gunma 376-0144/Japon (4 aut., 5 aut.); Oxford Radiocarbon Accelerator Unit, Research Laboratory for Archaeology and the History of Art, Dyson Perrins Building, University of Oxford/Oxford OX1 3QY/Royaume-Uni (1 aut.) |
|---|
| DT : | Publication en série; Congrès; Niveau analytique |
|---|
| SO : | Radiocarbon; ISSN 0033-8222; Etats-Unis; Da. 2007; Vol. 49; No. 2; Pp. 331-337; Bibl. 1/2 p. |
|---|
| LA : | Anglais |
|---|
| EA : | Progress in radiocarbon accelerator mass spectrometry (AMS) techniques enables much more access to wiggle-matching techniques for high-precision 14C dating with relatively low costs than before. Recently, we have applied wiggle-matching for a number of wood samples where dendrochronology is difficult because of various limitations imposed for dendro-dating. In most cases, wiggle-matching gave rather unambiguous calendar ages, but we found that in some cases the calibrated date was very sensitive to a systematic error of the 14C date. Here, we present a wooden artifact from the Ujishigai archaeological site as a case where the highest wiggle-matched date did not agree with the date given by dendrochronology. An age with lower probability agreed with the tree-ring age of AD 389, which marked the beginning of the production of Sue ware (unglazed stoneware) in Japan. We show that systematic errors must be carefully taken into account while interpreting 14C wiggle-matching results, whether they are due to instrumental errors (statistical) or due to a regional offset from the IntCal04 (Reimer et al. 2004) calibration curve. |
|---|
| CC : | 52618; 526 |
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| FD : | Datation; Matériau; Méthode; Spectrométrie de masse; Technique; Dendrochronologie; Bois; Japon; Calibration; Radiocarbone; Wiggle-matching |
|---|
| FG : | Asie |
|---|
| ED : | Dating; Materials; Method; Mass spectrometry; Technique; Dendrochronology; Wood; Japan; Calibration; Radiocarbon |
|---|
| EG : | Asia |
|---|
| LO : | INIST-502B.354000174300270170 |
|---|
| ID : | 08-0357951 |
|---|
Links to Exploration step
Francis:08-0357951
Le document en format XML
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<author><name sortKey="Imamura, Mineo" sort="Imamura, Mineo" uniqKey="Imamura M" first="Mineo" last="Imamura">Mineo Imamura</name>
<affiliation><inist:fA14 i1="01"><s1>National Museum of Japanese History, The National Institute for Humanities, 117 Jonai-cho</s1>
<s2>Sakura-shi, Chiba 285-8502</s2>
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<sZ>2 aut.</sZ>
</inist:fA14><author><name sortKey="Ozaki, Hiromasa" sort="Ozaki, Hiromasa" uniqKey="Ozaki H" first="Hiromasa" last="Ozaki">Hiromasa Ozaki</name>
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<s2>Sakura-shi, Chiba 285-8502</s2>
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<sZ>1 aut.</sZ>
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</inist:fA14><author><name sortKey="Mitsutani, Takumi" sort="Mitsutani, Takumi" uniqKey="Mitsutani T" first="Takumi" last="Mitsutani">Takumi Mitsutani</name>
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<sZ>3 aut.</sZ>
</inist:fA14><author><name sortKey="Niu, Etsuko" sort="Niu, Etsuko" uniqKey="Niu E" first="Etsuko" last="Niu">Etsuko Niu</name>
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<s2>Kiryu-shi, Gunma 376-0144</s2>
<s3>JPN</s3>
<sZ>4 aut.</sZ>
<sZ>5 aut.</sZ>
</inist:fA14><author><name sortKey="Itoh, Shigeru" sort="Itoh, Shigeru" uniqKey="Itoh S" first="Shigeru" last="Itoh">Shigeru Itoh</name>
<affiliation><inist:fA14 i1="03"><s1>Paleo-Labo Co. Ltd., 1900-65 Shimotazawa, Kurohone-cho</s1>
<s2>Kiryu-shi, Gunma 376-0144</s2>
<s3>JPN</s3>
<sZ>4 aut.</sZ>
<sZ>5 aut.</sZ>
</inist:fA14><series><title level="j" type="main">Radiocarbon</title>
<title level="j" type="abbreviated">Radiocarbon</title>
<idno type="ISSN">0033-8222</idno>
<imprint><date when="2007">2007</date>
</imprint><seriesStmt><title level="j" type="main">Radiocarbon</title>
<title level="j" type="abbreviated">Radiocarbon</title>
<idno type="ISSN">0033-8222</idno>
</seriesStmt><profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Calibration</term>
<term>Dating</term>
<term>Dendrochronology</term>
<term>Japan</term>
<term>Mass spectrometry</term>
<term>Materials</term>
<term>Method</term>
<term>Radiocarbon</term>
<term>Technique</term>
<term>Wood</term>
</keywords><keywords scheme="Pascal" xml:lang="fr"><term>Datation</term>
<term>Matériau</term>
<term>Méthode</term>
<term>Spectrométrie de masse</term>
<term>Technique</term>
<term>Dendrochronologie</term>
<term>Bois</term>
<term>Japon</term>
<term>Calibration</term>
<term>Radiocarbone</term>
<term>Wiggle-matching</term>
</keywords><front><div type="abstract" xml:lang="en">Progress in radiocarbon accelerator mass spectrometry (AMS) techniques enables much more access to wiggle-matching techniques for high-precision <sup>14</sup>
C dating with relatively low costs than before. Recently, we have applied wiggle-matching for a number of wood samples where dendrochronology is difficult because of various limitations imposed for dendro-dating. In most cases, wiggle-matching gave rather unambiguous calendar ages, but we found that in some cases the calibrated date was very sensitive to a systematic error of the <sup>14</sup>
C date. Here, we present a wooden artifact from the Ujishigai archaeological site as a case where the highest wiggle-matched date did not agree with the date given by dendrochronology. An age with lower probability agreed with the tree-ring age of AD 389, which marked the beginning of the production of Sue ware (unglazed stoneware) in Japan. We show that systematic errors must be carefully taken into account while interpreting <sup>14</sup>
C wiggle-matching results, whether they are due to instrumental errors (statistical) or due to a regional offset from the IntCal04 (Reimer et al. 2004) calibration curve.</div><inist><standard h6="B"><pA><fA01 i1="01" i2="1"><s0>0033-8222</s0>
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</fA03><fA08 i1="01" i2="1" l="ENG"><s1>RADIOCARBON WIGGLE-MATCHING OF JAPANESE HISTORICAL MATERIALS WITH A POSSIBLE SYSTEMATIC AGE OFFSET</s1>
</fA08><fA09 i1="01" i2="1" l="ENG"><s1>19th International Radiocarbon Conference, Keble College, Oxford, England. 3-7 April 2006</s1>
</fA09><fA11 i1="01" i2="1"><s1>IMAMURA (Mineo)</s1>
</fA11><fA11 i1="02" i2="1"><s1>OZAKI (Hiromasa)</s1>
</fA11><fA11 i1="03" i2="1"><s1>MITSUTANI (Takumi)</s1>
</fA11><fA11 i1="04" i2="1"><s1>NIU (Etsuko)</s1>
</fA11><fA11 i1="05" i2="1"><s1>ITOH (Shigeru)</s1>
</fA11><fA12 i1="01" i2="1"><s1>RAMSEY (Christopher Bronk)</s1>
<s9>ed.</s9>
</fA12><fA12 i1="02" i2="1"><s1>HIGHAM (Thomas F. G.)</s1>
<s9>ed.</s9>
</fA12><fA14 i1="01"><s1>National Museum of Japanese History, The National Institute for Humanities, 117 Jonai-cho</s1>
<s2>Sakura-shi, Chiba 285-8502</s2>
<s3>JPN</s3>
<sZ>1 aut.</sZ>
<sZ>2 aut.</sZ>
</fA14><fA14 i1="02"><s1>National Research Institute for Cultural Properties, Nara, 2-9-1 Nijo-cho</s1>
<s2>Nara-shi, Nara 630-8577</s2>
<s3>JPN</s3>
<sZ>3 aut.</sZ>
</fA14><fA14 i1="03"><s1>Paleo-Labo Co. Ltd., 1900-65 Shimotazawa, Kurohone-cho</s1>
<s2>Kiryu-shi, Gunma 376-0144</s2>
<s3>JPN</s3>
<sZ>4 aut.</sZ>
<sZ>5 aut.</sZ>
</fA14><fA15 i1="01"><s1>Oxford Radiocarbon Accelerator Unit, Research Laboratory for Archaeology and the History of Art, Dyson Perrins Building, University of Oxford</s1>
<s2>Oxford OX1 3QY</s2>
<s3>GBR</s3>
<sZ>1 aut.</sZ>
</fA15><fA20><s1>331-337</s1>
</fA20><fA21><s1>2007</s1>
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</fA64><fA66 i1="01"><s0>USA</s0>
</fA66><fC01 i1="01" l="ENG"><s0>Progress in radiocarbon accelerator mass spectrometry (AMS) techniques enables much more access to wiggle-matching techniques for high-precision <sup>14</sup>
C dating with relatively low costs than before. Recently, we have applied wiggle-matching for a number of wood samples where dendrochronology is difficult because of various limitations imposed for dendro-dating. In most cases, wiggle-matching gave rather unambiguous calendar ages, but we found that in some cases the calibrated date was very sensitive to a systematic error of the <sup>14</sup>
C date. Here, we present a wooden artifact from the Ujishigai archaeological site as a case where the highest wiggle-matched date did not agree with the date given by dendrochronology. An age with lower probability agreed with the tree-ring age of AD 389, which marked the beginning of the production of Sue ware (unglazed stoneware) in Japan. We show that systematic errors must be carefully taken into account while interpreting <sup>14</sup>
C wiggle-matching results, whether they are due to instrumental errors (statistical) or due to a regional offset from the IntCal04 (Reimer et al. 2004) calibration curve.</s0><fC02 i1="01" i2="A"><s0>52618</s0>
<s1>I</s1>
</fC02><fC02 i1="02" i2="A"><s0>526</s0>
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<s5>03</s5>
</fC03><fC03 i1="03" i2="H" l="ENG"><s0>Method</s0>
<s5>03</s5>
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<s5>04</s5>
</fC03><fC03 i1="04" i2="H" l="ENG"><s0>Mass spectrometry</s0>
<s5>04</s5>
</fC03><fC03 i1="05" i2="A" l="FRE"><s0>Technique</s0>
<s5>05</s5>
</fC03><fC03 i1="05" i2="A" l="ENG"><s0>Technique</s0>
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<s5>06</s5>
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<s5>07</s5>
</fC03><fC03 i1="07" i2="A" l="ENG"><s0>Wood</s0>
<s5>07</s5>
</fC03><fC03 i1="08" i2="A" l="FRE"><s0>Japon</s0>
<s2>NG</s2>
<s5>13</s5>
</fC03><fC03 i1="08" i2="A" l="ENG"><s0>Japan</s0>
<s2>NG</s2>
<s5>13</s5>
</fC03><fC03 i1="09" i2="A" l="FRE"><s0>Calibration</s0>
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<s2>FM</s2>
<s5>17</s5>
</fC03><fC03 i1="10" i2="A" l="FRE"><s0>Radiocarbone</s0>
<s2>NI</s2>
<s2>FM</s2>
<s5>18</s5>
</fC03><fC03 i1="10" i2="A" l="ENG"><s0>Radiocarbon</s0>
<s2>NI</s2>
<s2>FM</s2>
<s5>18</s5>
</fC03><fC03 i1="11" i2="A" l="FRE"><s0>Wiggle-matching</s0>
<s4>INC</s4>
<s5>31</s5>
</fC03><fC07 i1="01" i2="A" l="FRE"><s0>Asie</s0>
<s2>NG</s2>
<s5>21</s5>
</fC07><fC07 i1="01" i2="A" l="ENG"><s0>Asia</s0>
<s2>NG</s2>
<s5>21</s5>
</fC07><fN21><s1>224</s1>
</fN21><pR><fA30 i1="01" i2="1" l="ENG"><s1>International Radiocarbon Conference</s1>
<s2>19</s2>
<s3>Oxford GBR</s3>
<s4>2006-04-03</s4>
</fA30><server><NO>FRANCIS 08-0357951 INIST</NO>
<ET>RADIOCARBON WIGGLE-MATCHING OF JAPANESE HISTORICAL MATERIALS WITH A POSSIBLE SYSTEMATIC AGE OFFSET</ET>
<AU>IMAMURA (Mineo); OZAKI (Hiromasa); MITSUTANI (Takumi); NIU (Etsuko); ITOH (Shigeru); RAMSEY (Christopher Bronk); HIGHAM (Thomas F. G.)</AU>
<AF>National Museum of Japanese History, The National Institute for Humanities, 117 Jonai-cho/Sakura-shi, Chiba 285-8502/Japon (1 aut., 2 aut.); National Research Institute for Cultural Properties, Nara, 2-9-1 Nijo-cho/Nara-shi, Nara 630-8577/Japon (3 aut.); Paleo-Labo Co. Ltd., 1900-65 Shimotazawa, Kurohone-cho/Kiryu-shi, Gunma 376-0144/Japon (4 aut., 5 aut.); Oxford Radiocarbon Accelerator Unit, Research Laboratory for Archaeology and the History of Art, Dyson Perrins Building, University of Oxford/Oxford OX1 3QY/Royaume-Uni (1 aut.)</AF>
<DT>Publication en série; Congrès; Niveau analytique</DT>
<SO>Radiocarbon; ISSN 0033-8222; Etats-Unis; Da. 2007; Vol. 49; No. 2; Pp. 331-337; Bibl. 1/2 p.</SO>
<LA>Anglais</LA>
<EA>Progress in radiocarbon accelerator mass spectrometry (AMS) techniques enables much more access to wiggle-matching techniques for high-precision <sup>14</sup>
C dating with relatively low costs than before. Recently, we have applied wiggle-matching for a number of wood samples where dendrochronology is difficult because of various limitations imposed for dendro-dating. In most cases, wiggle-matching gave rather unambiguous calendar ages, but we found that in some cases the calibrated date was very sensitive to a systematic error of the <sup>14</sup>
C date. Here, we present a wooden artifact from the Ujishigai archaeological site as a case where the highest wiggle-matched date did not agree with the date given by dendrochronology. An age with lower probability agreed with the tree-ring age of AD 389, which marked the beginning of the production of Sue ware (unglazed stoneware) in Japan. We show that systematic errors must be carefully taken into account while interpreting <sup>14</sup>
C wiggle-matching results, whether they are due to instrumental errors (statistical) or due to a regional offset from the IntCal04 (Reimer et al. 2004) calibration curve.</EA><CC>52618; 526</CC>
<FD>Datation; Matériau; Méthode; Spectrométrie de masse; Technique; Dendrochronologie; Bois; Japon; Calibration; Radiocarbone; Wiggle-matching</FD>
<FG>Asie</FG>
<ED>Dating; Materials; Method; Mass spectrometry; Technique; Dendrochronology; Wood; Japan; Calibration; Radiocarbon</ED>
<EG>Asia</EG>
<LO>INIST-502B.354000174300270170</LO>
<ID>08-0357951</ID>
</server>
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