摘要:Correction to:
Scientific Reports 10.1038/s41598-017-16528-6, published online 29 November 2017
This Article contains errors in Figures 3 and 4.
In Figures 3a (orange), 3e and 4c-d (red and orange) the filled circles were incorrectly plotted.
The correct Figures
3 and
4 and accompanying legends appear below.
Figure 3
Eastern Mediterranean temperature records across TII. LC21 (purple) and ODP967 (orange)
G.
ruber (
a)
δ
18O
C and (
b,
c)
Δ
47-replicates (shadings correspond to the 95% CI of the 5,000 filtered simulations of the
Δ
47-replicates).
G.
ruber Δ
47-temperature records from (
d) LC21 and (
e) ODP967. Dots, thick lines, and shadings in (
d,
e) as in Fig. 2c. We also show in (
a,
d) the LC21
δ
18O
C and
Δ
47-temperature late-Holocene values (purple star), respectively. Gaps in the final
Δ
47-records correspond to intervals where the age uncertainties of the
Δ
47-replicates do not overlap.
Figure 4
TII temperature and
δ
18O
SW records across the Mediterranean Sea
. (
a) Northern Hemisphere insolation record at 65°N (black) overlain on the LC21 (purple) and ODP967 (orange)
Δ
47-temperature, and LC21
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