Author Correction: Penultimate deglacial warming across the Mediterranean Sea revealed by clumped isotopes in foraminifera

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) δ¹⁸O_C and (b,c) Δ₄₇-replicates (shadings correspond to the 95% CI of the 5,000 filtered simulations of the Δ₄₇-replicates). G. ruber Δ₄₇-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 δ¹⁸O_C and Δ₄₇-temperature late-Holocene values (purple star), respectively. Gaps in the final Δ₄₇-records correspond to intervals where the age uncertainties of the Δ₄₇-replicates do not overlap.

Figure 4.

TII temperature and δ¹⁸O_SW records across the Mediterranean Sea. (a) Northern Hemisphere insolation record at 65°N (black) overlain on the LC21 (purple) and ODP967 (orange) Δ₄₇-temperature, and LC21 ${\text{U}}_{37}^{{\text{K}}^{\prime }}$-temperature³² (using ref.⁶ age model) records from the eMed. (b) ODP975 G. bulloides Δ₄₇-temperature record (red) and ice-rafted debris (Lithics 90–150 μm, %) concentrations from the Iberian Margin (blue³⁹). (c) Freshwater fluxes into the North Atlantic (blue²) and ODP975 G. bulloides-δ¹⁸O_SW (red). (d) G. ruber δ¹⁸O_SW records from LC21 (purple) and ODP967 (orange). Dots, thick lines, and shadings as in Fig. 2c. LC21 Δ₄₇ late-Holocene temperature (purple star). Gaps in the final Δ₄₇-records correspond to intervals where the age uncertainties of the Δ₄₇-replicates do not overlap. Blue box highlights the HS11.