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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

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