High-time resolution AMS 14C data sets for Lake Baikal and Lake Hovsgol sediment cores

Changes in radiocarbon age and sedimentation rates during the transition from the last glacial to the Holocene

Takahiro Watanabe, Toshio Nakamura, Fumiko Watanabe Nara, Takeshi Kakegawa, Kazuho Horiuchi, Ryoko Senda, Takefumi Oda, Mitsugu Nishimura, Genki Inoue Matsumoto, Takayoshi Kawai

研究成果: ジャーナルへの寄稿記事

43 引用 (Scopus)

抄録

High-time resolution 14C dating of Lake Baikal sediment cores indicates negative and positive anomalies of calculated linear sedimentation rate (LSR; 1.1 and 35.6 cm/ka, respectively) during the period of climate transition from the last glacial to Holocene. The timing of the Lake Baikal apparent LSR anomalies is consistent with that of the changes in the atmospheric radiocarbon concentration (Δ14C) during Younger Dryas rapid cooling event. 14C dating of lipids in the Lake Baikal surface sediments revealed that the sources of sedimentary lipids were different in each basin. In the Northern Basin of Lake Baikal, the 14C age of total lipids from the surface sediment (4.0 14C ka) was found to be older than that of TOC (1.6 14C ka). By contrast, the 14C age of total lipids in the Southern Basin was younger than that of the TOC by ca. 0.7-3.0 ka. In the Lake Hovsgol sediment cores, ages of the main lithologic boundaries during the last glacial-interglacial transition were estimated based on new 14C data sets. TOC concentration in the cores started to rapidly increase at 13.8 ± 0.3 14C ka at the base of the basinwide finely laminated layer deposited during Bølling/Allerød. The base of the layer diatomaceous mud corresponds to the end of Younger Dryas event (10.6 ± 0.1 14C ka).

元の言語英語
ページ(範囲)12-20
ページ数9
ジャーナルQuaternary International
205
発行部数1-2
DOI
出版物ステータス出版済み - 8 15 2009
外部発表Yes

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accelerator mass spectrometry
Last Glacial
sedimentation rate
sediment core
lacustrine deposit
lipid
Holocene
lake
Younger Dryas
basin
anomaly
Last Glacial-Interglacial
sediment
mud
cooling
climate
dating

All Science Journal Classification (ASJC) codes

  • Earth-Surface Processes

これを引用

High-time resolution AMS 14C data sets for Lake Baikal and Lake Hovsgol sediment cores : Changes in radiocarbon age and sedimentation rates during the transition from the last glacial to the Holocene. / Watanabe, Takahiro; Nakamura, Toshio; Nara, Fumiko Watanabe; Kakegawa, Takeshi; Horiuchi, Kazuho; Senda, Ryoko; Oda, Takefumi; Nishimura, Mitsugu; Matsumoto, Genki Inoue; Kawai, Takayoshi.

:: Quaternary International, 巻 205, 番号 1-2, 15.08.2009, p. 12-20.

研究成果: ジャーナルへの寄稿記事

Watanabe, Takahiro ; Nakamura, Toshio ; Nara, Fumiko Watanabe ; Kakegawa, Takeshi ; Horiuchi, Kazuho ; Senda, Ryoko ; Oda, Takefumi ; Nishimura, Mitsugu ; Matsumoto, Genki Inoue ; Kawai, Takayoshi. / High-time resolution AMS 14C data sets for Lake Baikal and Lake Hovsgol sediment cores : Changes in radiocarbon age and sedimentation rates during the transition from the last glacial to the Holocene. :: Quaternary International. 2009 ; 巻 205, 番号 1-2. pp. 12-20.
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abstract = "High-time resolution 14C dating of Lake Baikal sediment cores indicates negative and positive anomalies of calculated linear sedimentation rate (LSR; 1.1 and 35.6 cm/ka, respectively) during the period of climate transition from the last glacial to Holocene. The timing of the Lake Baikal apparent LSR anomalies is consistent with that of the changes in the atmospheric radiocarbon concentration (Δ14C) during Younger Dryas rapid cooling event. 14C dating of lipids in the Lake Baikal surface sediments revealed that the sources of sedimentary lipids were different in each basin. In the Northern Basin of Lake Baikal, the 14C age of total lipids from the surface sediment (4.0 14C ka) was found to be older than that of TOC (1.6 14C ka). By contrast, the 14C age of total lipids in the Southern Basin was younger than that of the TOC by ca. 0.7-3.0 ka. In the Lake Hovsgol sediment cores, ages of the main lithologic boundaries during the last glacial-interglacial transition were estimated based on new 14C data sets. TOC concentration in the cores started to rapidly increase at 13.8 ± 0.3 14C ka at the base of the basinwide finely laminated layer deposited during B{\o}lling/Aller{\o}d. The base of the layer diatomaceous mud corresponds to the end of Younger Dryas event (10.6 ± 0.1 14C ka).",
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AU - Watanabe, Takahiro

AU - Nakamura, Toshio

AU - Nara, Fumiko Watanabe

AU - Kakegawa, Takeshi

AU - Horiuchi, Kazuho

AU - Senda, Ryoko

AU - Oda, Takefumi

AU - Nishimura, Mitsugu

AU - Matsumoto, Genki Inoue

AU - Kawai, Takayoshi

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