Santander, February 19th-22nd 2008 - Aranzadi
Santander, February 19th-22nd 2008 - Aranzadi
Santander, February 19th-22nd 2008 - Aranzadi
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122<br />
ZHANNA ANTIPUSHINA<br />
We reconstruct palaeoenvironmental conditions,<br />
based on analysis of shell remains from<br />
archaeological sites at Adak Island, Aleutian<br />
Islands. They were excavated by members of the<br />
Western Aleutian Archaeological and<br />
Palaeobiological Project (WAAPP), lead by D.L.<br />
West (University of Kansas).<br />
We investigated two shell middens. One shell<br />
midden ADK-171 is situated on the eastern coast<br />
of the Clam lagoon (51°55’32’’ N, 176°33’37’’ E),<br />
the second shell midden ADK-009 – on the south<br />
coast of the Sweeper Cove (51°51’10’’ N,<br />
176°38’18’’ E) (Fig. 1).<br />
2. MATERIALS AND METHODS<br />
The excavation areas in both sites were 1m 2<br />
and were excavated according to recognizable<br />
stratigraphic layers no thicker than 10 cm<br />
(Dinesman et al. 1999, Causey et al. 2005). Material<br />
was screened or sorted by hand. We used radiocarbon<br />
dating of fish bone collagen calibrated with<br />
OxCal 3.10. The dates obtained from the marine<br />
animal remains turned out to be a hundred years<br />
earlier because of the reservoir effect, so we used<br />
the calibration curve Marine04 (Reimer and Reimer<br />
2001, Hughen et al. 2004) and the regional correction<br />
ΔR for the southern part of the Bering sea<br />
(Stuiver and Braziunas 1993).<br />
We used the number of identified specimens<br />
(NISP) for quantification of chitons. For bivalves the<br />
number of umbo was counted (MNI). For gastropods,<br />
MNI was determined by the presence of<br />
>50% of the shell (Grayson 1984, Mason et al.<br />
1998, Claassen 2000, Glassow 2000, Mason et al.<br />
2000, Bird et al. 2002, Dinesman and Savinetsky<br />
2003, Antipushina <strong>2008</strong>).<br />
The samples were identified to the lowest taxonomical<br />
level possible using the reference collections<br />
housed at the Zoological Museum MSU,<br />
Institute of Ecology and Evolution RAS and<br />
Zoological Institute RAS.<br />
3. RESULTS AND DISCUSSIONS<br />
The ADK-171 profile included a cultural layer<br />
and several natural layers. The total depth of this<br />
profile was 2.7 m, and the cultural layer in this<br />
profile was 100 to 140 cm deep. Three radiocarbon<br />
dates show that the cultural layers were formed<br />
at the end of the 6 th millennium cal BC<br />
(6141±123 yr BP, IEMAE-1281; 6172±192 yr BP,<br />
Figure 1. Map of investigation area.<br />
MUNIBE Suplemento - Gehigarria 31, 2010<br />
S.C. <strong>Aranzadi</strong>. Z.E. Donostia/San Sebastián