Critica a la Teoría de la Función Económica Social

(PINEY ISLAND MIDDENI 8N®00255 MDSH FLOODPLAIN TERRA CEIA M UCK P P PINEY ISLAND 8MR00848 BURP FLOODPLAIN TERRA CELA M UCK P P

OLD SITE EATON CREEK 8M R000I4 M DSH FLOODPLAIN TERRA CELA MUCK-ASTATULA SAND,

DARK SU RI'ACE 8-17% \T P 315 RIDGE 8MR01867 SCNO FLOODPLAIN TERRA CEIA M UCK-HOLOPAW SAND P P

NN 8MR00044 M DSH FLOODPLAIN TERRA CEIA M UCK P PA GORES LANDING MIDDEN 8MRW030 MIDD FLOODPLAIN TERRA CEIA M UCK P UN GORES LANDING MOUND 8MR0003I MOUN FLOODPLAIN TERRA CEIA MUCK P UN DELKS LANDING M OUND 8MR00032 MOUN FLOODPIAXN TERRA CEIÀ-1BERIA CLAY VP UN

F l a u r # 4 . I S O k i a w a h a s t u d y a r e a a l i a s i n t a r r a c a i a m u c k k n o w s p r i o r t o t h a O R 8 p r o j a c t 1 9 9 1 .

During the ORS, six additional sites were recorded in the muck (See figure 4*11). Figure 4*13. illustrates site distribution within the terra ceia muck deposit by cultural affiliation both before and after the Okiawaha River Survey. Sixty per cent more sites were identified in the terra ceia muck as a result of the river's survey. By cultural affiliation, one-half of the newly recorded sites are prehistoric and the other 50 per cent are multi-component sites.

Straight comparison between the MSF's 54 known sites and the 11 newly recorded sites is problematical. Recalling the study area description given at the beginning of this chapter, the MSF data includes all sites along a 19 mile corridor whereas the ORS investigated only nine miles of the same corridor. The river survey's -distance falls short of the study area's length by a factor of two. The bias can be corrected by assuming that survey

of the study area's remaining ten miles would have yielded a similar number of sites. By doubling the number of sites found during the survey a better estimate for the impact of underwater -survey on site distribution is attained." Therefore, the.following figures include a column weighted for the significant length differentiation noted. Likewise, Figure 4.13 illustrates that rather than 60 per cent, the ORS could have recorded 120 per cent more sites in terra ceia muck than had been known previously within

the study area.

Comparison of sites in Terra Ceia Muck by Cultural Affiliation Cultural Affiliation Sites in TC Muck

known before ORS Sites recordedduring ORS 0R S x2 % A % A X 2 P 6 3 6 50 100 PA I 0 - - - H I 0 - - - HA 0 0 - - - M 0 3 6 (x3) (x6) UN 2 0 - - - TOTAL 10 60 120 F i g u r e 4 . 1 8 C e a p e s i t i e n o f s i t e s i n t e r r a c e i a m u c k , b y c u l t u r a l a f f i l i a t i o n , b a t h b e f o r e a n d a f t e r 0 R 8 p r o j e c t 1 8 9 1 .

Another useful method of determining the effect of underwater survey on, -site distribution patterns is grouping by cultural affiliation. Figures 4.14 through 4.18 list the known site data with respect to their gross cultural assignments; prehistoric (P) , prehistoric with historic aboriginal component (PA), historic Euroamerican (H), multi-component (M) and indeterminant (UN)

"This is a marginally acceptable means of sampling and full survey of the entire 19 mile length would have been best. However, funds to survey the entire study area were requested but only one-half the amount was received.

"since there were no historic/aboriginal (HA) sites identified in the Okiawaha study area, no table is provided.

SITEN iU IE SrrE_NU M BER SITETW E TOPOGRAPHA' SOILSERIE DR/UNAGEC CULTURE 8 PINEY ISLAND 8MRÜ0848 BURP FLOODPI..AIN TERRtA c el a M UCK P P /AMY'S DREAM 8MR00230 HABI LTL.AND LACUSTRINE DELKS S/AND-TERRA CEIA MUCK SP P USES OCA 90-14 8MR01969 HABI LIPLAND LACUSTRINE POMELLO SAND MW P SUNDAY BLUFF 8MR000I3 M DSH FLOODPLAIN ASTATLTA SAND, D/ARK SURFACE 8-17% E P USES 81-61 8MR00262 M DSH FLOODPLAIN ASTATULA SAND, D/ARK SURI'ACE 8-17% E P COIJaY LANDING SMR00057 M DSH FLOODPLAIN ASTATULA SAND (?) E P OKLAWAHA RIVER SH E IL M OUND It 8MR00224 M DSH LIPL/AND LACUS TRINE POMELLO SAND MW P DOUBLE BRIDGE M OUND B 8M R00I49 MDSH FLOODPLAIN SELLERS SAND \ T P TJ'S MIDDEN riTNEY ISLAND

MIDDENI 8MR00255 M DSH FLOODPLAIN TERRA CEIA M UCK P P OLD SITE EATON CREEK 8MROOOI4 M DSH FLOODPLAIN TERRA CEIA M UCK-ASTATLLA SAND,

DARK SURFACE 8-17% VP P EATON CREEK 8MR00015 MIDD pLOODPLAlN ASTATULA SAND 0-8»ô-ASTATULA SAND,

D.ARK SURFACE 8-17 E P EATON CREEK MIDDEN 8MR0Ü0I6 MIDD FLOODPLAIN TERRA CEIA MUCK P P PETERSON'S M OUND 8MR00146 M OUN UPLAND LACUSTRINE ASTATULA SAND, D.ARK SURI'ACE 0-8% E P PALMETTO LANDING M OUND 6 8MR00024 M OUN UPLAND LACUSTRINE DELKS S.AND SP P SHINER POND M OUND 2 8MR00CU9 MOUN UPLAND LACUSTRINE DELKS SAND-POMELLO SAND SP P BUCK MACDONALD MOUND 8M R00I45 MOUN UPLAND LA CU SnU N K PAOLA SAND. MOD. DEEP W m 0-5% E P COFFEE PO T M OUND 8MR0O141 M OU N MARGIN POMELLO S/U4D MW P DOUBLE BRIDGE M OUND A 8MR00148 MOUN FLOODPLAIN SELLERS S,\N D VP P LAKE CILARUiS UNIT 5, NO 1 8MR0O819 SCAR UPLAND LACUSTRINE •ASTATULA SAND. M OD. DEEP WTR 0-8?^ F, P USFS 81-57 8MR00248 SCAR UPLAND DRY ASTATULA SAND 0-8% E P ÎI4-A 8M R0I876 SCAR UPLAND LACUSTRINE PAOLA SAND. MOD. DEEP % TR 0-5% E P LAKE CHARIJÎS UNIT 5. NO 3 8MR0Ü820 SCAR UPLAND LACUSTRINE POMELLO S/VND MW P LAKE CH/ARLES UNIT 5. NO 2 8MR00831 SCAR UPLAND LACUSTRINE POMELLO S /W D MW P USS «89-2 OC.ALA 8M R 0I9I6 SCAR UPLAND LACUSTRINE POMELLO SAND MW P USFS 81-60 8MR00247 S C U UPLAND DRY ASTATULA S.AND. D.ARK SURF.ACE 8-17% E P NN 8MR00232 S C U UPLAND LACUSTRINE DELKS SAND SP P USFS 81-52 8MR00243 S C U UPLAND LACUSTRINE DELKS SAND SP P USFS 81-63 8MR00263 SC U FLOODPLAIN DELKS SAND SP P USFS OCA 87-3,SHARPES FERRY 52

SCATTER 8MR00851 S C U UPLAND LACUSTRINE DELKS SAND SP P USFS 81-51 8MR0O242 S C U UPLAND LACUSTRINE DELKS S.AND-POMELLO S/3ND MW-SP P GORES LANDING BORROAV PIT SMRtXWSO SC U FLOODPLAIN HOLOPAW SAND-ANCLOTE SAND P P USFS 81-53 8MR00244 SC U UPLAND LACUSTRINE POMELLO SAND MW P USFS 81-54 8MR00245 SC U LtPLAND LACUSTRINE POMELLO s a n d MW P FORE LAKE U'EST 8MR00519 S C U UPLAND LACUSTRINE POMELLO SAND MW P USFS 81-35 8MR00254 SC U FLOODPLAIN TERR.A CELA ML'CK P P 315 RIDGE 8MR01867 SCNO FLOODPLAIN TERR.A CEIA MUCK-HOLOPAW SAND P P

F i g u r e 4 . 1 4 F r e h i e t o r i c e i t e # k n e w n i n O k i a w a h a s t u d y a r e a p r i o r t o O R S p r o j e c t