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DOI	10.1016/j.palaeo.2019.109492
	Erratum to “Growth pattern and oxygen isotopic systematics of modern freshwater mollusks along an elevation transect: Implications for paleoclimate reconstruction” (Palaeogeography; Palaeoclimatology; Palaeoecology (2019) 532; (S0031018219300331); (10.1016/j.palaeo.2019.109243))
	Roy R.; Wang Y.; Jiang S.
发表日期	2020
ISSN	0031-0182
卷号	538
英文摘要	The publisher regrets that the Figs. 1, 2, 4–10 were captioned wrongly in the published article. The captions were abridged in all the figures, except in Fig. 3. In addiiton, the captions did not match the texts for Figs. 5-8. Hence, please find below the corrected figure captions. Fig. 1 Location map (Google maps: Imagery © 2016 Landsat, Data SIO, NOAA, U.S. Navy, NGA, GEBCO, Map data © 2016 Google, ZENRIN) showing the lakes from where the samples were collected: Lake Manasarovar at the highest elevation of 4.6 km above sea level (m.a.s.l.), Fuxian Lake at an elevation of ~1.7 km m.a.s.l. and Liuxihe Reservoir at ~0.2 km m.a.s.l. (symbols not to scale). Fig. 2 Photos showing examples of serial sampled shells of Bellamya sp. and Radix sp. The Bellamya specimen shown here was 2.3 cm in length and the Radix was 1.0 cm in length. In the Radix shells the holes were drilled along the black dots. Diameter of the drill holes is ~0.3 mm. Sampling was started from the aperture (the youngest part of a shell) and ended at the apex (the oldest part of a shell). Fig. 4 Seasonal variations in the water temperature, and in the δ18OW of Fuxian Lake and δ18OW of precipitation in the area. The precipitation isotope data are from the nearby IAEA-GNIP station in Kunming located ~60 km North of Fuxian Lake (IAEA/WMO, 2018). Lake water δ18OW values were measured in this study. The long-term monthly average water temperature data are from Gu (2008). Fig. 5 Seasonal variations in the water temperature and in the δ18OW of Liuxihe Reservoir and δ18OW of precipitation in the area. The precipitation isotope data are from the nearby IAEA-GNIP station in Guangzhou (~80 km south of Liuxihe Reservoir) (IAEA/WMO, 2018). Lake water δ18OW values were measured in this study. Water temperature data are an average of the long-term temperature data from Peng et al. (2007) and measured water temperature in this study. Fig. 6 Seasonal variations in the water temperature in the region recorded at lake Ngangla Ring Cuo (~160 km northeast of Lake Manasarovar; Huntington et al., 2015) and the monthly average δ18OW of precipitation (1986–1992) in Lhasa (located ~940 km SE of the lake) (IAEA/WMO, 2018). Fig. 7 δ18OAr values of serial samples from individual shells and the calculated temperature (black smooth line) variation along the direction of shell growth during the life span of each snail analyzed from Fuxian Lake (A–F). Temperatures are calculated from the δ18OAr values of serial sampled shell and the annual average δ18OW (±1 Σ) of lake water using the aragonite–water isotope fractionation equation of Kim et al. (2007). Shaded area represents the range of calculated temperature.ing the life span of each snail analyzed from Fuxian Lake (A–F). Fig. 8 δ18OAr values of serial samples from individual shells and the calculated temperature (black smooth line) variation along the direction of shell growth during the life span of each snail analyzed from Liuxihe Reservoir (A–D). Temperatures are calculated from the δ18OAr values of serial sampled shell and the annual average δ18OW (±1 Σ) of lake water using the aragonite–water isotope fractionation equation of Kim et al. (2007). Shaded area represents the range of calculated temperature. Fig. 9 δ18OAr values of serial samples from individual Radix shells and the calculated temperature variation (black smooth line) along the direction of shell growth during the life span of each snail analyzed from Lake Manasarovar. Temperatures are calculated from the δ18OAr of serial sampled shell and the δ18OW values of lake water (including values obtained in this study and from Yao et al. (2009), and from the average of the available lake water δ18OW values) using the aragonite–water aragonite–water isotope fractionation equation of Kim et al. (2007). Shaded area represents the range of calculated temperature. Fig. 10 Comparisons of average δ18OArvalues of individual shells, and average δ18OW values of lake water and precipitation (A); annual range of average monthly average air temperatures and magnitude of intra-shell temperature variation (B); and average growth temperatures of individual shells, MAWT, and MAAT (C) among study sites. The average δ18OAr value and the average growth temperature of an individual shell were calculated by averaging values of all serial samples from that shell. The precipitation δ18OW value for each lake is the weighed annual mean value recorded at the IAEA-GNIP station near the lake except for Lake Manasarovar where the precipitation δ18OW value represents the value of one rain sample collected in August of 2010 (see text for more information). The error bars indicate ±1 standard deviation from the means. The publisher would like to apologise for any inconvenience caused. © 2019 Elsevier B.V.
语种	英语
scopus关键词	Gastropoda; Mollusca
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/150657
作者单位	Department of Earth, Ocean, and Atmospheric Science, Florida State University, Tallahassee, FL 32306, United States; National High Magnetic Field Laboratory, Tallahassee, FL 32310, United States; Department of Estuarine and Ocean Sciences, School for Marine Science and Technology, University of Massachusetts Dartmouth, New Bedford, MA 02744, United States; Institute of Groundwater and Earth Science, Jinan University, Guangzhou, 510632, China
推荐引用方式 GB/T 7714	Roy R.,Wang Y.,Jiang S.. Erratum to “Growth pattern and oxygen isotopic systematics of modern freshwater mollusks along an elevation transect: Implications for paleoclimate reconstruction” (Palaeogeography; Palaeoclimatology; Palaeoecology (2019) 532; (S0031018219300331); (10.1016/j.palaeo.2019.109243))[J],2020,538.
APA	Roy R.,Wang Y.,&Jiang S..(2020).Erratum to “Growth pattern and oxygen isotopic systematics of modern freshwater mollusks along an elevation transect: Implications for paleoclimate reconstruction” (Palaeogeography; Palaeoclimatology; Palaeoecology (2019) 532; (S0031018219300331); (10.1016/j.palaeo.2019.109243)).Palaeogeography, Palaeoclimatology, Palaeoecology,538.
MLA	Roy R.,et al."Erratum to “Growth pattern and oxygen isotopic systematics of modern freshwater mollusks along an elevation transect: Implications for paleoclimate reconstruction” (Palaeogeography; Palaeoclimatology; Palaeoecology (2019) 532; (S0031018219300331); (10.1016/j.palaeo.2019.109243))".Palaeogeography, Palaeoclimatology, Palaeoecology 538(2020).