气候变化领域集成服务门户(CCPortal): Corrigendum to “Ecohydrological evolution of Lake Naivasha (central Rift Valley; Kenya) during the past 1650 years; as recorded by ostracod assemblages and stable-isotope geochemistry” [Quat. Sci. Rev. 223 (2019) 105906] (Quaternary Science Reviews (2019) 223; (S0277379119303920); (10.1016/j.quascirev.2019.105906))

CCPortal

DOI	10.1016/j.quascirev.2020.106439
	Corrigendum to “Ecohydrological evolution of Lake Naivasha (central Rift Valley; Kenya) during the past 1650 years; as recorded by ostracod assemblages and stable-isotope geochemistry” [Quat. Sci. Rev. 223 (2019) 105906] (Quaternary Science Reviews (2019) 223; (S0277379119303920); (10.1016/j.quascirev.2019.105906))
	Van der Meeren T.; Ito E.; Laird K.R.; Cumming B.F.; Verschuren D.
发表日期	2020
ISSN	0277-3791
卷号	242
英文摘要	In the published article, the upper panel of Figure 6 was erroneously based on an earlier version of the age model. The updated figure, including the final and corrected age model, is printed below: [Figure presented] Fig. 6. Ecohydrological history of Lake Naivasha during the past 1650 years. Overview of ostracod-based reconstructions (CeF) in relation to the fluctuations in lake depth and salinity derived from other proxies (AeB). Yellow-shaded areas highlight the episodes when CIC was hydrologically closed; red vertical lines are the ostracod zonation boundaries, as in Fig. 4 (A) Lake-level reconstruction, revised from Verschuren (2001). Water depth at the deepest point of the CIC basin is plotted in relation to the estimated minimum elevation halting sediment focusing into CIC (dashed line 1); the sill elevation between CIC and the main basin of Lake Naivasha (dashed line 2); and the estimated maximum elevation for hydrological closure of CIC (dashed line 3); all three dashed lines are slanted, to reflect the overall reduction in water depth over time due to sediment infill. (B) Reconstruction of diatom-inferred conductivity, as in Verschuren et al. (2000a) but extended beyond 770 CE to the base of the record. (C) PCA scores summarizing the stratigraphic turnover in fossil ostracod assemblages. (D) Additional ostracod proxy information: i) depth interval with highest taxon richness (asterisk; cf. Fig. 4), indicating the onset of more permanent Malewa River inflow; ii) depth intervals with elevated proportion of non-calcified Z. costata valves (stippled line), reflecting reduced lake-water alkalinity and residence time; and iii) intervals containing large (>1000 mm) ostracod species (grey line sections), reflecting limited fish predation. (EeF) LOESS-smoothed time series of ostracod d18O and d13C, vertical bars represent the range in measured data at a given depth. All panels are plotted on a linear time axis according to the updated age model, with a non-linear depth axis for reference. (For interpretation of the references to colour in this figure legend, the reader is referred to the Web version of this article.) © 2020 Elsevier Ltd
语种	英语
scopus关键词	Bacillariophyta; Ostracoda
来源期刊	Quaternary Science Reviews
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/151398
作者单位	Department of Biology, Ghent University, K. L. Ledeganckstraat 35, Gent, 9000, Belgium; Department of Earth Sciences and Limnological Research Center, University of Minnesota, 310 Pillsbury Drive SE, Minneapolis, MN 55455, United States; Department of Biology, Queen's University, 116 Barrie St., Kingston, ON K7L 3N6, Canada
推荐引用方式 GB/T 7714	Van der Meeren T.,Ito E.,Laird K.R.,等. Corrigendum to “Ecohydrological evolution of Lake Naivasha (central Rift Valley; Kenya) during the past 1650 years; as recorded by ostracod assemblages and stable-isotope geochemistry” [Quat. Sci. Rev. 223 (2019) 105906] (Quaternary Science Reviews (2019) 223; (S0277379119303920); (10.1016/j.quascirev.2019.105906))[J],2020,242.
APA	Van der Meeren T.,Ito E.,Laird K.R.,Cumming B.F.,&Verschuren D..(2020).Corrigendum to “Ecohydrological evolution of Lake Naivasha (central Rift Valley; Kenya) during the past 1650 years; as recorded by ostracod assemblages and stable-isotope geochemistry” [Quat. Sci. Rev. 223 (2019) 105906] (Quaternary Science Reviews (2019) 223; (S0277379119303920); (10.1016/j.quascirev.2019.105906)).Quaternary Science Reviews,242.
MLA	Van der Meeren T.,et al."Corrigendum to “Ecohydrological evolution of Lake Naivasha (central Rift Valley; Kenya) during the past 1650 years; as recorded by ostracod assemblages and stable-isotope geochemistry” [Quat. Sci. Rev. 223 (2019) 105906] (Quaternary Science Reviews (2019) 223; (S0277379119303920); (10.1016/j.quascirev.2019.105906))".Quaternary Science Reviews 242(2020).