migration times are caused by a delay in the arrival of the shrimp at a size large 
enough for the trawls to capture. When an appropriate time lag is used the correlation 
is improved between the relative abundance of emigrating juveniles and the catch per 
unit of effort of small shrimp on the Tortugas grounds. Based on this relationship a 
forecast of increased abundance of small shrimp on the fishing grounds can be made 
before they are available to the fishery. Using commercial landing data an apparent 
movement through the Tortugas can be seen. This appears reliable enough so that a 
forecast of up to 4 months can be made of increased abundance of 41 - 50 count shrimp. 
1964 
Costello, T. J., and D. M. Allen (1965) Pink shrimp life history. Fishery research for the 
year ending June 30 1964. Circ. No. 230. Bureau of Commercial Fisheries, US Fish and 
Wildlife Service, Galveston, TX. 22-4. 
This citation describes pink shrimp life history. 
1964 0 
Craighead, F. C. (1964) Land, mangroves and hurricanes. Fairchild Trop. Gard. Bull. . 
1 9(4): 1-28. 
(DATE OF SAMPLING UNKNOWN OR NOT APPLICABLE.] This citation reviews the role of 
mangroves in building new land in South Florida and the effects of the deposits of silt 
and shell by hurricanes in this process. The effects of hurricane Donna in South Florida 
are discussed. 
1964 
Holden, M. W. (1964) Sea turtle nesting survey on Cape Sable beach, Everglades National 
Park, Florida, 1964 season. Open File Rep. N4415. South Florida Research Center, 
Everglades National Park, Homestead, FL. 
[NO COPY OF PAPER AVAILABLE. ABSTRACT FROM SCHMIDT (1991).] This paper 
presents the earliest known National Park Service report of sea turtle nesting on Cape 
Sable. It is the traditional nesting ground for the loggerhead turtle, Caretta caretta, and 
once was used by the green turtle, Chelonia mydas. Five miles of beach was surveyed, 
from East Cape to SE of Middle Cape. Data is provided on the marking and counting of 
turtle crawls, destroyed nests, and hatching with additional notes on racoon 
observations in the survey area. 
1964 0 
Price, W. A. (1964) Cyclic cuspate sand spits and sediment transport efficiency. J. GeoL 
72(6):876-80. 
[NO COPY OF PAPER AVAILABLE. ABSTRACT FROM SCHMIDT (1991).] Contrasts in the 
occurrence of cyclic cuspate spits are found between: (1) a smooth, sandy oceanic 
barrier shoreline and spit-decorated shorelines of the associated narrow barrier 
lagoon; (2) In spit development varying from none on a straight sandy shoreline to 
progressively prominent development with increasing convexity along an adjoining 
sandy headland. Critical factors in this selectivity seem to be wave fetch and shoreline 
curvature. An example of sandy cuspate foreland and small sandy foreland is Cape 
Sable. 
1964 0 
Scholl, D. W. (1964) Recent sedimentary record in mangrove swamps and rise in sea level 
over the southwest coast of Florida. Part 1. Mar. GeoL 1:344-66. 
[DATE OF SAMPLING UNKNOWN OR NOT APPLICABLE.] Beneath the shallowly submerged 
coastal mangrove forest (paralic mangrove swamps) of southwestern Florida, marine 
and brackish-water sediments of Recent age overlie freshwater calcitic mud that was 
168 
