Deep-sea limestone block as a source of 14C-depleted dissolved inorganic carbon at the Palau Trench

Tsuboi, Tatsuya; Wada, Hideki; Nakamura, Toshio; Hang, Tran Thuy; Matsuzaki, Hiroyuki; Otsuji, Naho; Fujioka, Kantaro; Oguri, Kazuta; Kitazato, Hiroshi

doi:10.1016/j.chemgeo.2013.11.013

Cited by 2 publications

(1 citation statement)

References 25 publications

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“…The BG standard on the other hand was combusted in a sealed quartz tube with V 2 O 5 at 1000°C for 2 hours to produce CO 2 . The purification and graphitization of CO 2 , from the standards (NOX and BG), were the same processes as for sample (S) (Wada et al, 1984;Tsuboi et al, 2014). For these graphite samples, 12 C, 13 C, and 14 C abundances were synchronously measured using an accelerator mass spectrometer (AMS) of the Micro-Analysis Laboratory, University of Tokyo (MALT), Japan (Matsuzaki et al, 2007).…”

Section: Measurement and Calibrationmentioning

confidence: 99%

Radial growth rate through successive cambia in <i>Haloxylon ammodendron </i>(Chenopodiaceae) from the Gurbantünggüt Desert, Northwestern China, determined by a series of radiocarbon dating

Wada

Matsuzaki

2015

Geochem. J.

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marina (A. marina, a grey mangrove species) show a succession of dark colored xylem tissue bands and pale colored phloem tissue bands (Robert et al., 2011). It is difficult to clearly distinguish RISC layers from annual rings, because the RISC layers possess similar morphological features as compared to annual rings through megascopic cross sectional observations (Fig. 1). RISC layer cannot form a complete closed ring but several fragments in a growing season (Robert et al., 2011, 2014; Nazim et al., 2013). Previous studies have demonstrated that the dendrochronological methods cannot be applied to some successive cambia species (Schmitz et al., 2007; Nazim et al., 2013). Santini et al. (2013) used radiocarbon techniques combining with X-ray densitometry to develop a wood density chronology for A. marina in the Exmouth Gulf (from Western Australia), and confirmed that the actual growth rates (range from 4.08 ± 2.36 to 5.30 ± 3.33 mm/yr) were higher than the RISC layer width (range from 0.58 ± 0.08 to 0.97 ± 0.29 mm/layer) (Santini

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Section: Measurement and Calibrationmentioning

confidence: 99%

Radial growth rate through successive cambia in <i>Haloxylon ammodendron </i>(Chenopodiaceae) from the Gurbantünggüt Desert, Northwestern China, determined by a series of radiocarbon dating

Wada

Matsuzaki

2015

Geochem. J.

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Effects of decarbonation on elemental behaviors during subduction-zone metamorphism: Evidence from a titanite-rich contact between eclogite-facies marble and omphacitite

Xiao

Niu

Zhang

et al. 2017

Journal of Asian Earth Sciences

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. (2017) 'Eects of decarbonation on elemental behaviors during subduction-zone metamorphism : evidence from a titanite-rich contact between eclogite-facies marble and omphacitite.', Journal of Asian earth sciences., 135 . pp. 338-346. Further information on publisher's website: Use policyThe full-text may be used and/or reproduced, and given to third parties in any format or medium, without prior permission or charge, for personal research or study, educational, or not-for-prot purposes provided that:• a full bibliographic reference is made to the original source • a link is made to the metadata record in DRO • the full-text is not changed in any way The full-text must not be sold in any format or medium without the formal permission of the copyright holders.Please consult the full DRO policy for further details.

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Deep-sea limestone block as a source of 14C-depleted dissolved inorganic carbon at the Palau Trench

Cited by 2 publications

References 25 publications

Radial growth rate through successive cambia in <i>Haloxylon ammodendron </i>(Chenopodiaceae) from the Gurbantünggüt Desert, Northwestern China, determined by a series of radiocarbon dating

Radial growth rate through successive cambia in <i>Haloxylon ammodendron </i>(Chenopodiaceae) from the Gurbantünggüt Desert, Northwestern China, determined by a series of radiocarbon dating

Effects of decarbonation on elemental behaviors during subduction-zone metamorphism: Evidence from a titanite-rich contact between eclogite-facies marble and omphacitite

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