Fig. 3 | Nature Communications

Fig. 3

From: Coral carbon isotope sensitivity to growth rate and water depth with paleo-sea level implications

Fig. 3

South Pacific coral δ13C and skeletal extension rate: coral annual skeletal extensions rates (in blue) and annual average skeletal δ13C (black open dots) and δ13C data with the average atmospheric 13C Suess effect removed (solid black dots) in Porites lutea corals from: a Fiji core AB53, b Fiji core 1F52, c Tonga core TNI254, d Rarotonga core 2R51,52, and e American Samoa core Ta’u-155,56. Extension rate and δ13C significantly correlate to varying degrees (see R values in Table 1) up until the mid-20th century when coral δ13C abruptly shifts ~1.0‰ lower at all of these sites. The very low growth year in 2000 in Tonga core TNI2 is a confirmed bleaching event when growth was truncated to 7 mm in that year. Also note that Fiji cores 1F and AB were collected from Porites lutea colonies in Savusavu Bay at the same water depth approximately 100 m from each other. Source data are provided as a Source Data file in the Supplement

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