We would like to thank Michael Haslam (Haslam et al., 2013) for his interest in our recent contribution on the dating of the Young Toba Tuff/Tephra (YTT) (Mark et al., 2013). However, we point out errors made by Haslam, using this opportunity to clarify and expand on our discussion while also re-emphasising the important points from our study that have been overlooked
Thermochronometry provides one of few methods to quantify rock exhumation rate and history, includin...
International audienceSauvet et al. (in press) present a partial description of the Uranium-series o...
Radiocarbon dates on samples aimed to date the settlement of Iceland are given together with comment...
We would like to thank Michael Haslam (Haslam et al., 2013) for his interest in our recent contribut...
We would like to thank Michael Haslam (Haslam et al., 2013) for his interest in our recent contribut...
Haslam and Petraglia raise three broad questions concerning our paper ‘Environmental impact of the 7...
Baksi (2012) claims that a number of radiometric ages presented in Barry et al. (2010) are statistic...
The potential impact of the ~73 ka Toba super-eruption upon global and regional climate, terrestrial...
peer reviewedWhen this paper was originally published, there was an error in Fig. 7g. Indeed the cur...
An IRSL age of 17.0 ± 2.2 ka (and a “mean age” of ca. 19 ka) reported by Grapes et al. [Grapes, R., ...
Climatic consequences of the Young Toba Tuff (YTT) eruption about 73 ka are a crucial argument in th...
Letter to the editorBanerjee, D. [2009. Thermoluminescence and optically stimulated luminescence sig...
<jats:p>Joachimski et al. carried out geochemical investigations to study seawater temperature...
late Paleocene thermal maximum (LPTM) has an age between 57.5 and 60.54 Ma (vs. 54.98 Ma in the curr...
International audienceWhen this paper was originally published there was an error in Table 1. The ag...
Thermochronometry provides one of few methods to quantify rock exhumation rate and history, includin...
International audienceSauvet et al. (in press) present a partial description of the Uranium-series o...
Radiocarbon dates on samples aimed to date the settlement of Iceland are given together with comment...
We would like to thank Michael Haslam (Haslam et al., 2013) for his interest in our recent contribut...
We would like to thank Michael Haslam (Haslam et al., 2013) for his interest in our recent contribut...
Haslam and Petraglia raise three broad questions concerning our paper ‘Environmental impact of the 7...
Baksi (2012) claims that a number of radiometric ages presented in Barry et al. (2010) are statistic...
The potential impact of the ~73 ka Toba super-eruption upon global and regional climate, terrestrial...
peer reviewedWhen this paper was originally published, there was an error in Fig. 7g. Indeed the cur...
An IRSL age of 17.0 ± 2.2 ka (and a “mean age” of ca. 19 ka) reported by Grapes et al. [Grapes, R., ...
Climatic consequences of the Young Toba Tuff (YTT) eruption about 73 ka are a crucial argument in th...
Letter to the editorBanerjee, D. [2009. Thermoluminescence and optically stimulated luminescence sig...
<jats:p>Joachimski et al. carried out geochemical investigations to study seawater temperature...
late Paleocene thermal maximum (LPTM) has an age between 57.5 and 60.54 Ma (vs. 54.98 Ma in the curr...
International audienceWhen this paper was originally published there was an error in Table 1. The ag...
Thermochronometry provides one of few methods to quantify rock exhumation rate and history, includin...
International audienceSauvet et al. (in press) present a partial description of the Uranium-series o...
Radiocarbon dates on samples aimed to date the settlement of Iceland are given together with comment...