and N-S normal faulting. In this way, staircased marine terraces were 

 generated following the gentle, progressive, uplifting of these reliefs. 

 (Authors) 



117 GOY, J. L. , and ZAZO, C. 1986. "Western Almeria (Spain) Coastline 

 Changes Since the Last Interglacial , " Journal of Coastal Research . Special 

 Issue No. 1, pp 89-93. 



We have identified four marine terraces which contain S. bubonius 

 (Tyearrhenian) on the coast of Almeria in southeastern Spain where all marine 

 terraces are affected by normal and strike-slip faulting, manifesting tectonic 

 activity throughout the Quaternary. Two areas were studied for this paper. 

 The following sequence of processes were found in the Adra region: the 

 Tyearrhenian transgression; the Wurm regression with development of alluvial 

 fans; the Holocene transgression and its related eolian deposits; the forma- 

 tion of the Adra delta in the Eighteenth Century as a result of human activ- 

 ity; and the formation of the present Adra delta (19th Century) , its 

 progradation, and the formation of spit bars creating lagoons. In the 

 Guardias Viejas-Roquetas coastal area, the following sequence took place: 

 northward tilting of the Camp de Dallas at the beginning of the middle 

 Pleistocene; the formation of three raised stairstepped beaches with S. 

 bubonius . The most recent has been dated at about 104,000+6,000 years (Th/U) 

 or 109,000+16,00012,000 years (Pa/U) ; the Wurm regression with several 

 oscillations, one of which was very near the present sea- level; the Holocene 

 transgression, with a somewhat higher sea-level than that of today, as evi- 

 denced by an Ostrea beach; and the formation of four beach ridge systems, the 

 third of which began to form at about 1,870+35 BP(C"') . (Authors). 



118 GRANT, D. R. 1985. "Coral Reefs and Sea-Levels," Episodes . Vol 8, 

 No. 3, pp 193-194. 



This article is a conference report on coral reefs and sea- levels. The 

 conference was held in Tahiti, 27 May- 9 June 1985 and sponsored by 

 International Association of Biological Oceanography. The meeting consisted 

 of 2 days of paper sessions and a field trip to reef, atoll, and volcanic 

 island settings. (Gorman). 



119 GREENLEE, S. M. , and MOORE, T. C 1988. "Recognition and 

 Interpretation of Depositional Sequences and Calculation of Sea-level Changes 

 from Stratigraphic Data-Offshore New Jersey and Alabama Tertiary," Wilgus, 

 C. K. , Hastings, B. S., Kendall, C. G., Posamentier, H. W. , Ross, C. A., and 

 Van Wagoner, J. C, eds . , Sea- level Changes: An Integrated Approach . Special 

 Publication No. 42, Society of Economic Paleontologists and Mineralogists, 

 Tulsa, OK, pp 329-356. 



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