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7,000<br />

25,000<br />

6,000<br />

5,000<br />

?<br />

4,000<br />

cal yr BP<br />

3,000<br />

Gulf <strong>of</strong> Mexico (Balsillie <strong>and</strong> Donoghue, 2004)<br />

Red Sea (Siddall et al. 2003)<br />

20,000<br />

15,000<br />

Cal Yr BP<br />

10,000<br />

Figure 1.5. Composite sea-level curves for <strong>the</strong> nor<strong>the</strong>rn Gulf <strong>of</strong> Mexico. The solid line<br />

adapted from Balsillie <strong>and</strong> Donoghue (2004) is a comprehensive compilation <strong>of</strong> radiocarbon<br />

dated sea-level indicators for <strong>the</strong> nor<strong>the</strong>rn Gulf <strong>of</strong> Mexico. The dashed curve is <strong>the</strong> global<br />

“eustatic” sea-level history from Red Sea benthic foraminifera data <strong>of</strong> Siddall et al. (2003).<br />

19<br />

Gulf <strong>of</strong> Mexico Younger Data Set<br />

2,000<br />

5,000<br />

1,000<br />

0<br />

0<br />

10<br />

0<br />

-10<br />

-20<br />

-30<br />

-40<br />

-50<br />

-60<br />

-70<br />

-80<br />

-90<br />

6<br />

4<br />

2<br />

0<br />

-2<br />

-4<br />

-6<br />

-8<br />

-100<br />

-110<br />

-120<br />

-130<br />

-10<br />

-12<br />

Meters MSL<br />

Sea Level (m)

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