Corrigendum to “A sub-millennial sediment record of ice-stream retreat and meltwater storage in the Baltic Ice Lake during the Bølling-Allerød interstadial” (Quaternary Science Reviews (2018) 198 (126–139), (S0277379118303500), (10.1016/j.quascirev.2018.08.018))

A. L. Kelly, Sandra Passchier

Research output: Contribution to journalComment/debateResearch

Abstract

When this article was first published there was a plotting error in Figure 7. The revised plot is presented below and it should replace the original Figure 7. The implication of the error is that there is only a slight enrichment of Th over upper crustal values, and that the Th/Sc ratios for the proximal (Unit IIIb) varves are not significantly different from those of the distal (Unit IIIa) varves in Hanö Bay. However, this change does not influence the conclusions of the study. The authors regret this error. Figure 7. Bi-plot of Th/Sc ratios vs. Zr/Sc ratios, showing enrichment of Th for the lower proximal Baltic Ice Lake varves at Site M0064 (Unit IIIb). Diamictites of Unit IV and distal varves of Unit IIIa both have compositions near upper crustal values (McLennan, 2001) with Zr enrichment in the diamicton. The black line represents the typical compositional variability of fine-grained turbidites generated in active margin settings (from McLennan et al., 1993).

Original languageEnglish
Article number105940
JournalQuaternary Science Reviews
Volume223
DOIs
StatePublished - 1 Nov 2019

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Baltic Ice Lake
varve
ice stream
interstadial
snowmelt
meltwater
ice
lakes
sediments
science
sediment
diamicton
active margin
Values
Varves
Retreat
Sediment
Enrichment

Cite this

@article{32d6aec4e575400f97f5ed935d5af80c,
title = "Corrigendum to “A sub-millennial sediment record of ice-stream retreat and meltwater storage in the Baltic Ice Lake during the B{\o}lling-Aller{\o}d interstadial” (Quaternary Science Reviews (2018) 198 (126–139), (S0277379118303500), (10.1016/j.quascirev.2018.08.018))",
abstract = "When this article was first published there was a plotting error in Figure 7. The revised plot is presented below and it should replace the original Figure 7. The implication of the error is that there is only a slight enrichment of Th over upper crustal values, and that the Th/Sc ratios for the proximal (Unit IIIb) varves are not significantly different from those of the distal (Unit IIIa) varves in Han{\"o} Bay. However, this change does not influence the conclusions of the study. The authors regret this error. Figure 7. Bi-plot of Th/Sc ratios vs. Zr/Sc ratios, showing enrichment of Th for the lower proximal Baltic Ice Lake varves at Site M0064 (Unit IIIb). Diamictites of Unit IV and distal varves of Unit IIIa both have compositions near upper crustal values (McLennan, 2001) with Zr enrichment in the diamicton. The black line represents the typical compositional variability of fine-grained turbidites generated in active margin settings (from McLennan et al., 1993).",
author = "Kelly, {A. L.} and Sandra Passchier",
year = "2019",
month = "11",
day = "1",
doi = "10.1016/j.quascirev.2019.105940",
language = "English",
volume = "223",
journal = "Quaternary Science Reviews",
issn = "0277-3791",
publisher = "Elsevier Ltd",

}

TY - JOUR

T1 - Corrigendum to “A sub-millennial sediment record of ice-stream retreat and meltwater storage in the Baltic Ice Lake during the Bølling-Allerød interstadial” (Quaternary Science Reviews (2018) 198 (126–139), (S0277379118303500), (10.1016/j.quascirev.2018.08.018))

AU - Kelly, A. L.

AU - Passchier, Sandra

PY - 2019/11/1

Y1 - 2019/11/1

N2 - When this article was first published there was a plotting error in Figure 7. The revised plot is presented below and it should replace the original Figure 7. The implication of the error is that there is only a slight enrichment of Th over upper crustal values, and that the Th/Sc ratios for the proximal (Unit IIIb) varves are not significantly different from those of the distal (Unit IIIa) varves in Hanö Bay. However, this change does not influence the conclusions of the study. The authors regret this error. Figure 7. Bi-plot of Th/Sc ratios vs. Zr/Sc ratios, showing enrichment of Th for the lower proximal Baltic Ice Lake varves at Site M0064 (Unit IIIb). Diamictites of Unit IV and distal varves of Unit IIIa both have compositions near upper crustal values (McLennan, 2001) with Zr enrichment in the diamicton. The black line represents the typical compositional variability of fine-grained turbidites generated in active margin settings (from McLennan et al., 1993).

AB - When this article was first published there was a plotting error in Figure 7. The revised plot is presented below and it should replace the original Figure 7. The implication of the error is that there is only a slight enrichment of Th over upper crustal values, and that the Th/Sc ratios for the proximal (Unit IIIb) varves are not significantly different from those of the distal (Unit IIIa) varves in Hanö Bay. However, this change does not influence the conclusions of the study. The authors regret this error. Figure 7. Bi-plot of Th/Sc ratios vs. Zr/Sc ratios, showing enrichment of Th for the lower proximal Baltic Ice Lake varves at Site M0064 (Unit IIIb). Diamictites of Unit IV and distal varves of Unit IIIa both have compositions near upper crustal values (McLennan, 2001) with Zr enrichment in the diamicton. The black line represents the typical compositional variability of fine-grained turbidites generated in active margin settings (from McLennan et al., 1993).

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U2 - 10.1016/j.quascirev.2019.105940

DO - 10.1016/j.quascirev.2019.105940

M3 - Comment/debate

VL - 223

JO - Quaternary Science Reviews

JF - Quaternary Science Reviews

SN - 0277-3791

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