Christopher M. Wurster, Hamdi Rifai, Bin Zhou, Jordahna Haig, Michael I. Bird
In this Article, the references for Figure 2c, 2d, and 2e are incorrect. As a result, the legend for Figure 2: “Comparison of guano δ13C records to regional records of palaeoclimate from key regions in and around Sundaland. (a) Cave stalagmite δ18O records from Borneo23,45. (b) δ13C values from fatty acids from Lake Towuti, Sulawesi39. (c) Guano δ13C record from Palawan23. (d) Aereal extent of Sunda shelf exposure38. (e) Guano δ13C record from Peninsular Malaysia23. (f) Guano (blue) and n-alkane records from Saleh Cave (red, C27: closed, C29: open). Calibrated age ranges (2σ) from radiocarbon measurements are plotted. Highlighted area indicates the Last Glacial Maximum.” should read: “Comparison of guano δ13C records to regional records of palaeoclimate from key regions in and around Sundaland. (a) Cave stalagmite δ18O records from Borneo23,45. (b) δ13C values from fatty acids from Lake Towuti, Sulawesi39. (c) Guano δ13C record from Palawan24. (d) Aereal extent of Sunda shelf exposure39. (e) Guano δ13C record from Peninsular Malaysia24. (f) Guano (blue) and n-alkane records from Saleh Cave (red, C27: closed, C29: open). Calibrated age ranges (2σ) from radiocarbon measurements are plotted. Highlighted area indicates the Last Glacial Maximum.”. © 2020, The Author(s).
College of Science and Engineering, James Cook University, Cairns, 4870, QLD, Australia; ARC Centre of Excellence for Australian Biodiversity and Heritage, James Cook University, Cairns, 4870, QLD, Australia; Centre of Tropical Environmental and Sustainability Sciences, James Cook University, Cairns, 4870, QLD, Australia; Department of Physics Faculty of Mathematics and Natural Sciences, Universitas Negeri Padang, Padang, 25131, Indonesia; Key Laboratory of Surficial Geochemistry (Ministry of Education), School of Earth Sciences and Engineering, Nanjing University, Nanjing, China
