Deposition and retention of meteoric 10Be in Holocene Taiwan river terraces

Deng, Kai; Wittmann, Hella; Hsieh, Meng-Long; Yang, Shouye; Blanckenburg, Friedhelm von

doi:10.1016/j.quascirev.2021.107048

Cited by 6 publications

(1 citation statement)

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“…10.1029/2021JF006221 5 of 18 You et al, 1988). Here we use an up-to-date, site-specific flux of 0.77 ± 0.11 × 10 6 at/cm 2 /yr constrained by meteoric 10 Be profiles of Holocene river terraces in Taiwan (Deng et al, 2021). Other approaches for determination of 10 Be depositional fluxes, including general circulation models (GCMs) (Heikkilä & von Blanckenburg, 2015) and rainfall 10 Be-based fitting equation (Graly et al, 2011), are commonly applied over larger spatial scales and may overestimate 10 Be fluxes in our study area (Deng et al, 2021;.…”

Section: Sampling Detailsmentioning

confidence: 99%

The Upper Limit of Denudation Rate Measurement From Cosmogenic ¹⁰Be(Meteoric)/⁹Be Ratios in Taiwan

et al. 2021

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Tectonically active regions produce disproportionately high sediment (physical erosion) (Milliman & Syvitski, 1992) and dissolved (chemical weathering) (Gaillardet et al., 1999) fluxes to the oceans, and therefore play an important role in the global carbon cycle. As an active mountain belt, the Taiwan orogen alone bears eight of the world's 13 rivers with sediment yield >10 4 t/km 2 /yr (Milliman & Farnsworth, 2011) that results from active tectonics and frequent typhoon events. Rates of mineral weathering from silicates and sulfides (Blattmann et al., 2019;Bufe et al., 2021) and rates of organic carbon transport and oxidation (Hemingway et al., 2018;Hilton et al., 2012) in the Taiwan orogen are among the highest worldwide as these processes are driven by rapid denudation. Hence, knowledge of denudation rates that integrate over time scales

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Section: Sampling Detailsmentioning

confidence: 99%

The Upper Limit of Denudation Rate Measurement From Cosmogenic ¹⁰Be(Meteoric)/⁹Be Ratios in Taiwan

et al. 2021

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Quantifying denudation rates and sediment recycling of low-relief, high-elevation landscapes using in-situ and meteoric cosmogenic nuclides

Yang,

Zhang,

Zhang

et al. 2024

Geochimica et Cosmochimica Acta

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Climate variability in a 3.8 Ma old sedimentary record from the hyperarid Atacama Desert

Arens,

Feige,

Airo

et al. 2024

Global and Planetary Change

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Deposition and retention of meteoric 10Be in Holocene Taiwan river terraces

Cited by 6 publications

References 62 publications

The Upper Limit of Denudation Rate Measurement From Cosmogenic ¹⁰Be(Meteoric)/⁹Be Ratios in Taiwan

The Upper Limit of Denudation Rate Measurement From Cosmogenic ¹⁰Be(Meteoric)/⁹Be Ratios in Taiwan

Quantifying denudation rates and sediment recycling of low-relief, high-elevation landscapes using in-situ and meteoric cosmogenic nuclides

Climate variability in a 3.8 Ma old sedimentary record from the hyperarid Atacama Desert

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Deposition and retention of meteoric 10Be in Holocene Taiwan river terraces

Cited by 6 publications

References 62 publications

The Upper Limit of Denudation Rate Measurement From Cosmogenic 10Be(Meteoric)/9Be Ratios in Taiwan

The Upper Limit of Denudation Rate Measurement From Cosmogenic 10Be(Meteoric)/9Be Ratios in Taiwan

Quantifying denudation rates and sediment recycling of low-relief, high-elevation landscapes using in-situ and meteoric cosmogenic nuclides

Climate variability in a 3.8 Ma old sedimentary record from the hyperarid Atacama Desert

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The Upper Limit of Denudation Rate Measurement From Cosmogenic ¹⁰Be(Meteoric)/⁹Be Ratios in Taiwan

The Upper Limit of Denudation Rate Measurement From Cosmogenic ¹⁰Be(Meteoric)/⁹Be Ratios in Taiwan

Climate variability in a 3.8 Ma old sedimentary record from the hyperarid Atacama Desert