Corrigendum to “Evidence for solar influence in a Holocene speleothem record (Père Nöel cave, SE Belgium)” (Quaternary Science Reviews (2018) 192 (249–262), (S0277379118302038) (10.1016/j.quascirev.2018.05.039))

• Published in: Quaternary Science Reviews
• Main Authors: Allan, Mohammed, Deliège, Alain, Verheyden, S., Nicolay, Samuel, Quinif, Y., Fagel, Nathalie
• Format: Article in Journal/Newspaper
• Language: English
• Published: Elsevier Ltd 2019
• Subjects: Physical; chemical; mathematical & earth Sciences; Earth sciences & physical geography; Physique; chimie; mathématiques & sciences de la terre; Sciences de la terre & géographie physique; North Atlantic
• Online Access: https://orbi.uliege.be/handle/2268/238466; https://orbi.uliege.be/bitstream/2268/238466/1/Corrigendum%20to%20Evidence%20for%20solar%20influence%20in%20a%20Holocene%20speleothem%20record%20%28P%c3%a8re%20No%c3%abl%20cave%20SE%20Belgium%29_.docx; https://doi.org/10.1016/j.quascirev.2019.02.024

peer reviewed When this paper was originally published, there was an error in Fig. 7g. Indeed the curve of percentage of hematite-stained grains measured on North Atlantic MC52-VM29-191 core, published by Bond et al. (2001), was inverted. Please find the correct Fig. 7 below: [Figure presented] Fig. 7 corrected: (a), (b) and (c) PN trace elements contents (Sr = red line; Ba = green line; and Mg = black line) in comparison to (d) PN Stalagmite δ 18 O (blue line), (e) δ 18 O record from Bunker Cave-W Germany (Fohlmeister et al., 2012), (f) δ 18 O record from lake Ammersee- Germany (von Grafenstein et al., 1999), (g) hematite-stained grains from the North Atlantic (Bond et al., 2001), (h) frequency of wet/dry events in the Northern Hemisphere as defined by Wanner et al. (2014). The blue horizontal bars mark cold events. In the paper, Fig. 7 allows us to compare the trace elements Ba, Sr, Mg and δ 18 O isotopes results of Père Noël (PN) stalagmite with other continental and marine records. In the figure, the blue lines underline the 6 geochemical events measured in our speleothem PN record that we attribute to cold events. As a first point, we note that most of the PN events are consistent with some of the dry events (Fig. 7h) defined by Wanner et al. (2014) for the Northern Hemisphere. The correspondence is clear for 5 intervals corresponding to the 2.6–2.8, 4.6–4.8, 6.2–6.4, 8.1–8.3 and 9.3–9.5 Wanner events (no data for the oldest event at 10.3–10.7). Second, we compare the PN record with the abundance of hematite-stained grains in core VM29-191 (Bond et al., 2001). This curve, that was used as one of the drift ice indices, represents the North Atlantic cold events. (Note the comparison with the stacked curve would lead to the same conclusion). At least the 3 PN events at 4.6–4.8, 6.2–6.4 and 9.3–9.5 ka BP occur in a time interval consistent with the Bond events 3, 4 and 6, respectively. In the manuscript, the text must be corrected (see lines 416–418):“During these three intervals (i.e., around 10.5, between ...