Exact(3)
a LR04 benthic isotope stack.
Intervals of laminated sediment at Site U1427 are shown at the base of the lower panel Fig. 10 a LR04 oxygen isotope stack.
In the LR04 δ 18O global isotope stack (Lisiecki and Raymo 2005), values are higher during this time compared to values during MIS 47, 43, 31, 11, 9, 5, and 1 (Fig. 4).
Similar(5)
The generated δ18O curve was then correlated to the LR04 stack isotope reference curve (Lisiecki and Raymo 2005) and the dataset of Bassinot et al. (1994).
isotope ratio mass spectrometry.
isotope dilution mass spectrometry.
The 14C dates and tephrochronology were used to establish an initial age depth model in order to express the δ18O curve of C0018A as a function of time and to compare the isotope data with the LR04 stack reference curve of Lisiecki and Raymo (2005) and the stack isotope curve of Bassinot et al. (1994).
The ages in core Z14-6 were determined using the correlation between the cores' oxygen isotope curve and the δ18O stack curve (Zhou et al. 2007).
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