BD missing, & column AW: is the included data series before or after filtering?  LCB: AFTER

LCB(29/03/2019): the first tab in lipdverse should be the primary series (no hiatuses). Don't know which one it is

observed seasonal changes of d18O of rainfall

changes of d18O in speleothems reflect changes of the average d18O of rainfall in the region related to rainfall seasonality

age model constructed by linear interpolation

observed present day correlation between rainfall seasonality and d18O at a nearby station of the Global Network for Isotopes in precipitation

Changes in the strength of the Bermuda high cause variations of the amount of summer rain at the site; higher summer rain leads to more positive d18O in rainfall

Hardt, B., Rowe, H. D., Springer, G. S., Cheng, H. and Edwards, R. L.: The seasonality of east central North American precipitation based on three coeval Holocene speleothems from southern West Virginia, Earth and Planetary Science Letters, 295(3-4), 342–348, doi:10.1016/j.epsl.2010.04.002, 2010.

d18O (SP10HAUS01A): interpretation3_scope: '' has been replaced by 'isotope'
d18O (SP10HAUS01A): interpretation4_scope: '' has been replaced by 'isotope'
d18O (SP10HAUS02A): interpretation3_scope: '' has been replaced by 'isotope'
d18O (SP10HAUS02A): interpretation4_scope: '' has been replaced by 'isotope'
d18O (SP10HAUS03A): interpretation3_scope: '' has been replaced by 'isotope'
d18O (SP10HAUS03A): interpretation4_scope: '' has been replaced by 'isotope'

characteristics and physical conditions of Tzabnah cave, a Hendy test and isotopic equilibrium calculations (Sharp, 2007)

A calibration between Chaac ?18O and the instrumental record of precipitation from a meteorological station in Mi¿½rida indicates a significant correlation between the two signals (r=?0.62, P=0.023) with a slope of ?176 mm??1 increase in Chaac ?18O (Fig. 4). The strength of the relationship between Chaac ?18O and rainfall amount is similar to that observed between rainfall amount data from adjacent meteorological stations (0.2brb0.7, Pb0.01).