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. 2020 Mar 3;10:4267. doi: 10.1038/s41598-020-60958-8

Author Correction: Savanna in equatorial Borneo during the late Pleistocene

Christopher M Wurster 1,2,3,✉, Hamdi Rifai 4, Bin Zhou 5, Jordahna Haig 1,2,3, Michael I Bird 1,2,3
PMCID: PMC7051967  PMID: 32123272

Correction to: Scientific Reports 10.1038/s41598-019-42670-4, published online 25 April 2019

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.”


Articles from Scientific Reports are provided here courtesy of Nature Publishing Group

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