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Santander, February 19th-22nd 2008 - Aranzadi

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Analysis of malacofauna remains from archaeological sites on Adak Island (Aleutian Islands, USA)<br />

123<br />

Profile ADK-171<br />

0 - 5 cm Present-day sod<br />

Peaty sod, grayish chestnut, friable, unstructured, pierced by roots; transition to the underlying horizon is distinct and even.<br />

6 - 10 cm 40-year-old ash<br />

Between tussocks – light brown to grayish olive-brown, loamy, ductile, adhesive, unstructured; pierced by roots; transition to the underlying horizon<br />

is gradual, the boundary uneven.<br />

10 – 50 cm Peaty soil<br />

10 – 18 cm Under tussocks – dark grey to chestnut getting lighter, loamy, ductile, adhesive, unstructured; pierced by roots; transition to the underlying horizon is gradual.<br />

18 - 50 cm Peaty, dark chestnut, homogeneous, compacted, ductile, adhesive; densely pierced by roots; plant remains are well decomposed; transition to the<br />

underlying horizon is abrupt and even.<br />

50 - 61 cm Sandwich Volcanic ash<br />

Heterogeneous tephra layers. Coarse-grained clastic ash (50-54 cm) is replaced by inequigranular sandy volcanic ash with coarse clastic concretions<br />

(54-57 cm) still lower (57-60 cm) is presented by fine- grained volcanic ash olive color; the boundary is abrupt and even.<br />

61 - 100 cm Stratified mineral stratum<br />

Heterogeneous stratified tephra thickness. Interchanging volcanic ash layers, from brown chestnut to light olive tinted with grayish black; ash layers<br />

is fine- grained, ductile, adhesive; many fine roots; low boundary is abrupt and even.<br />

100 - 140 cm Cultural layer<br />

100 - 125 cm Layer of densely large clam shells packed, almost without fine-grained mineral material, bones. During the excavation we divided this layer into<br />

two – layer 2 and layer 3.<br />

125 - 129 cm Layer of re-deposited volcanic ash, grayish-pink, fine-grained to loamy, adhesive.<br />

129 - 141 cm Layer of small mussel shells. Shells is mixed with tiny fragments of the charcoal. In the left part of side and along slopes the layer flattens and<br />

consists only of broken shells. Crumbs of shells prevail at the contact with lower horizon, material gets sooty. We called this horizon – layer 4.<br />

140 -150 cm Volcanic ash? Sandy loam, brown-pink to grayish brown, compacted, ductile, adhesive, friable upon drying, possible volcanic ash; impregnated<br />

with well decomposed organic matter; the boundary is abrupt and even.<br />

150 - 166 cm Intermediate Volcanic ash<br />

Heterogeneous stratified tephra stratum; the streaks alternate with the lenses of mineral material from volcanic ash; inequigranular to well<br />

sorted, saturated with coarse clastic ash; variegated- light olive to light brown; ductile, adhesive; the boundary is abrupt and even.<br />

166 cm and lower Dune sand<br />

Homogenous sand, unstructured, middle- grained, whitish grey; indistinct ferruginous streaks and spots on depth 166 - 170 cm and 222 - 230 cm;<br />

streaks of black-colored minerals; the boundary is abrupt and even.<br />

IEMAE-1248; 6,525±94 yr BP, IEMAE-1296).<br />

These data confirm that ADK-171 is the oldest<br />

archaeological site found on the Adak Island<br />

(Luttrell and Corbett 2000).<br />

The total depth of the ADK-009 profile was<br />

170 cm, and the cultural layer in this profile was<br />

22 to 166 cm deep. Four radiocarbon dates from<br />

fish bone collagen, show that the cultural layer<br />

was formed from the beginning of 8 th to the beginning<br />

of 19 th centuries cal AD (Table 1).<br />

Depth of Laboratory Material dated Radiocarbon Calibrated dates,<br />

horizon (cm) number IEMAE- age, years BP years AD (2σ<br />

23 – 38 1264 fish bone collagen 755±72 1627 – 1890<br />

45 – 79 1242 fish bone collagen 1126±103 1260 – 1660<br />

115 – 127 1288 fish bone collagen 1360±74 1060 – 1410<br />

150 – 160 1265 fish bone collagen 1888±50 590 – 900<br />

Table 1. Radiocarbon dating of ADK-009<br />

Profile ADK-009<br />

1 – 13 cm Re-deposited culture layer<br />

Dark-gray to black sward culture layer pierced by roots, saturated with crashed shells and bones.<br />

13 – 18 cm Buried sod<br />

Dark-brown to brown buried motley sod with inclusions of light-brown presumably ash spots.<br />

18 – 20 cm 40-year-old ash<br />

Light-brown fine-sorted compressed ash layer of uneven thickness<br />

20 – 22 cm Humus streak<br />

Light-brown to brown smeared humus streak<br />

22 – 166 cm Culture layer<br />

22 – 56 cm Layer I<br />

22 – 35 cm Dark-gray to black fine-grained mineral material saturated with crashed shells, pierced by roots, with inclusions of sparse bones.<br />

Lens of sea urchin plates in the bottom left corner.<br />

35 – 37 cm Streak of fine-grained material: dark-brown to brown with black tint, compressed, unstructured, adhesive, almost without bones and shells.<br />

37 – 56 cm Heterogeneous horizon of crashed shells and bones interchanging with lenses of fine-grained material.<br />

MUNIBE Suplemento - Gehigarria 31, 2010<br />

S.C. <strong>Aranzadi</strong>. Z.E. Donostia/San Sebastián

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