气候变化领域集成服务门户(CCPortal): Corrigendum to “Millennial scale climate oscillations recorded in the Lower Danube loess over the last glacial period” [Palaeogeogr. Palaeoclimatol. Palaeoecol. 509; 15 November 2018 164–181](S0031018216309051)(10.1016/j.palaeo.2016.12.029)

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DOI	10.1016/j.palaeo.2019.01.026
	Corrigendum to “Millennial scale climate oscillations recorded in the Lower Danube loess over the last glacial period” [Palaeogeogr. Palaeoclimatol. Palaeoecol. 509; 15 November 2018 164–181](S0031018216309051)(10.1016/j.palaeo.2016.12.029)
	Zeeden C.; Hambach U.; Veres D.; Fitzsimmons K.; Obreht I.; Bösken J.; Lehmkuhl F.
发表日期	2019
ISSN	0031-0182
起始页码	116
结束页码	117
卷号	523
英文摘要	In the article ‘Millennial scale climate oscillations recorded in the Lower Danube loess over the last glacial period’ (Zeeden et al., 2018), we employed rock magnetic and grain size proxy data in combination with luminescence dating and correlation age models to examine millennial-scale climate variability at Rasova, Romania. The absolute values of mass-normalized magnetic susceptibility (MS) contain a systematic error due to incorrect conversion of instrument readings into SI units. The instrument assumes a volume of 10 cm 3 , and we in fact measured samples of 6.4 cm 3 volume. Therefore, the previously reported MS values were too low by a factor of 1.56×. The authors apologize for this error. This error does not affect the main conclusions of our study, whose focus is on relative variations of MS, but it influences absolute MS values and their comparison to other reference datasets (Section 6.3). Here, we provide a corrected version of Fig. 5 to show the relationship between MS at Rasova and in other reference datasets. Most significantly, the χ B at Rasova is actually ~2.30 × 10 −7 m 3 kg −1 . This is slightly elevated compared to average values of 1.7 × 10 −7 ± 0.2 m 3 kg −1 determined by Forster et al. (1994) and (Buggle et al., 2014) for Eurasian loess. These elevated values are interpreted as due to input of sediments with a higher MS from local sources. However, the applied fit does not allow for a precise determination of the χ B .[Figure presented] Corrected Fig. 5: χ lf (ordinate) vs. χ Δ (abscissa), and the “true loess line” for Europe as suggested by Zeeden et al. (2016), based on Forster et al. (1994). Besides pedogenic magnetic enhancement (χ lf ↑, χ Δ ↑), trends of the wind vigour effect (χ lf ↑, χ Δ ↓) and of magnetic depletion are shown (χ lf ↓, χ Δ ↑). Note that only the interval above ca. 1.5 m shows pedogenically enhanced χ. In the interval below (until 3.2 m), numerous samples deviate from the trend marked by the “true loess line”, indicating the contribution of sediment particles with a coarser magnetic fraction and not affected by magnetic enhancement. Thin black lines mark the confidence limit of the fit. The grey arrow indicates the difference between χ B at Rasova and the reference data of Forster et al. (1994). © 2017 Elsevier B.V.
语种	英语
来源期刊	Palaeogeography, Palaeoclimatology, Palaeoecology
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/150993
作者单位	Department of Geography, RWTH Aachen University, Germany; LIAG, Leibniz Institute for Applied Geophysics, Stilleweg 2, Hannover, 30655, Germany; BayCEER & Chair of Geomorphology, University of Bayreuth, Germany; Laboratory for Palaeoecological Reconstruction, Faculty of Sciences, University of Novi Sad, Serbia; Institute of Speleology, Romanian Academy, Cluj-Napoca, Romania; Interdisciplinary Research Institute on Bio-Nano-Science of Babes-Bolyai University, Cluj-Napoca, Romania; Department of Human Evolution, Max Planck Institute for Evolutionary Anthropology, Germany; Max Planck Research Group for Terrestrial Palaeoenvironments, Max Planck Institute for Chemistry, Germany
推荐引用方式 GB/T 7714	Zeeden C.,Hambach U.,Veres D.,等. Corrigendum to “Millennial scale climate oscillations recorded in the Lower Danube loess over the last glacial period” [Palaeogeogr. Palaeoclimatol. Palaeoecol. 509; 15 November 2018 164–181](S0031018216309051)(10.1016/j.palaeo.2016.12.029)[J],2019,523.
APA	Zeeden C..,Hambach U..,Veres D..,Fitzsimmons K..,Obreht I..,...&Lehmkuhl F..(2019).Corrigendum to “Millennial scale climate oscillations recorded in the Lower Danube loess over the last glacial period” [Palaeogeogr. Palaeoclimatol. Palaeoecol. 509; 15 November 2018 164–181](S0031018216309051)(10.1016/j.palaeo.2016.12.029).Palaeogeography, Palaeoclimatology, Palaeoecology,523.
MLA	Zeeden C.,et al."Corrigendum to “Millennial scale climate oscillations recorded in the Lower Danube loess over the last glacial period” [Palaeogeogr. Palaeoclimatol. Palaeoecol. 509; 15 November 2018 164–181](S0031018216309051)(10.1016/j.palaeo.2016.12.029)".Palaeogeography, Palaeoclimatology, Palaeoecology 523(2019).