Tracing the Source of the Elephant And Hippopotamus Ivory from ...

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Tracing the Source of the Elephant and Hippopotamus Ivory from the 14 th Century B.C. Uluburun Shipwreck: The Archaeological, Historical, and Isotopic Evidence Kathryn A. Lafrenz ABSTRACT The aim of this study is to establish the provenance of the elephant and hippopotamus ivory recovered from the 14th century B.C. Uluburun shipwreck in order to reconstruct the trade mechanisms operating in the eastern Mediterranean during the Late Bronze Age. Current research indicates that elephant ivory came either from Northeastern Libya, Southeastern Sudan via Egypt or northwestern Syria during this period. Hippopotamus ivory likewise was either obtained from Syria, Palestine, or Egypt. The majority of the artifacts from the Uluburun shipwreck are of Cypriot and Syro-Palestinian origin, and the cargo is reconstructed by the excavator, George Bass, as a “royal” cargo. Indeed, Late Bronze Age trade is largely understood as a form of gift- exchange between ruling elites, thereby reflecting a trade system organized by and for a centralized authority. With the transition to the Iron Age, an identifiable merchant class developed and trade became decentralized (relative to the preceding era) under a system of cabotage trade influenced by market forces rather than royal initiatives. If the ivory is shown to derive from several regions as opposed to originating from a single location, a revision of Late Bronze Age trade must be fashioned to include ruling elites acting as x
“merchants” to a larger degree than previously assumed. Indeed, the mechanisms of the LBA trade must be established in order to provide a complete picture of trade, especially since the import and historical data is arguably biased towards a simplistic, centralized trade system. The δ 13 C, δ 15 N, and δ 18 O reflect the climate and vegetation of the area in which a population lives, so that areas with similar climate and vegetation will produce similar isotopic signatures, even though these areas may be geographically distant from one another. Nevertheless, examining the 87 Sr/ 86 Sr ratios will distinguish between populations because this ratio mirrors the isotopic signature of the underlying rock, and is sufficiently unique to each area to warrant differentiation. Isotopic ratio analysis (carbon, nitrogen, oxygen, and/or strontium) was conducted on the collagen and apatite components of the ivory samples using mass spectrometry in order to differentiate between these areas and therefore provide the provenance. xi
Page 1 and 2: Tracing the Source of the Elephant
Page 3 and 4: Table of Contents List of Tables iv
Page 5 and 6: Mechanisms of Late Bronze Age trade
Page 7 and 8: List of Figures Figure 1. Morpholog
Page 9 and 10: Figure 35. Average δ 13 C values o
Page 11: Figure 69. KW 2557 (Hippopotamus tu
Page 15 and 16: skeletal part to verify the presenc
Page 17 and 18: possibility of sophisticated scient
Page 19 and 20: B.C. and resumed Egyptian campaigni
Page 21 and 22: urbanization at centers such as Enk
Page 23 and 24: incisors”) of the elephant. Each
Page 25 and 26: Dentine in elephant tusks is essent
Page 27 and 28: perpendicular to the tubules....[co
Page 29 and 30: Figure 3 : The incisors and canines
Page 31 and 32: for the elephant, is where the dent
Page 33 and 34: Chapter 3 The Archaeological, Histo
Page 35 and 36: pastoralism. Today most of the hipp
Page 37 and 38: emains in the Syro-Palestinian regi
Page 39 and 40: near Beersheba. An EB I lower right
Page 41 and 42: Figure 13: The distribution of Midd
Page 43 and 44: Figure 14: 18 th Dynasty Egyptian t
Page 45 and 46: Chapter 4 The Archaeological, Histo
Page 47 and 48: Figure 16: Present distribution of
Page 49 and 50: Maghreb was inaccessible or nonexis
Page 51 and 52: flooding and dense human population
Page 53 and 54: BCE), mentions imports of approxima
Page 55 and 56: The degree of contact between the L
Page 57 and 58: Minoan and Mycenaean sherds from th
Page 59 and 60: are lacking in North Africa, but th
Page 61 and 62: Part II: The Syrian Elephant Turnin
Page 63 and 64:
Figure 22: Location of Ghab Valley
Page 65 and 66:
elephants show a lower preference f
Page 67 and 68:
similar to those of the African ele
Page 69 and 70:
Chapter 5 Ivory Workshops in the La
Page 71 and 72:
of the waste pieces may be reused f
Page 73 and 74:
ivory and silver (Odyssey XIX.55) a
Page 75 and 76:
century B.C. (LH I-LH IIIB), but th
Page 77 and 78:
ivory from a burnt deposit in Thebe
Page 79 and 80:
Tell Fakhariyah has only yielded ex
Page 81 and 82:
Figure 28: Comparison of utilizatio
Page 83 and 84:
Much of the discussion about Palest
Page 85 and 86:
(Lilyquist 1998: 27; Gachet 1993: 7
Page 87 and 88:
argues that for both of the types
Page 89 and 90:
The End of Ivory-working in the LBA
Page 91 and 92:
study residence and mobility. Katze
Page 93 and 94:
feeding on the plant (Sukumar and R
Page 95 and 96:
4‰ lower than those of marine pla
Page 97 and 98:
Studies which have focused on evalu
Page 99 and 100:
sediments in one area had isotopic
Page 101 and 102:
local environment, and thus answer
Page 103 and 104:
Figure 32: Sr concentrations plotte
Page 105 and 106:
Figure 34: 87 Sr/ 86 Sr vs. age of
Page 107 and 108:
Chapter 7 Ecological and Dietary Re
Page 109 and 110:
wide, straight lips of the hippo en
Page 111 and 112:
unlikely that many were actually ea
Page 113 and 114:
proportion of C3 to C4 vegetation i
Page 115 and 116:
diet as interpreted from the stable
Page 117 and 118:
had larger ranges than those elepha
Page 119 and 120:
Tchamba and Seme (1993) likewise re
Page 121 and 122:
fact adapted to the desert, and thi
Page 123 and 124:
Table 2: δ 13 C values and % C4 fr
Page 125 and 126:
Figure 35: Average δ 13 C values o
Page 127 and 128:
Table 4: Percentage of C3 plants in
Page 129 and 130:
Table 5: Isotope values for Ambosel
Page 131 and 132:
Figure 39: “Carbon and nitrogen i
Page 133 and 134:
Table 6 (continued) 120
Page 135 and 136:
Figure 41: δ 13 C versus δ 15 N f
Page 137 and 138:
Figure 43: δ 13 C versus δ 15 N f
Page 139 and 140:
Figure 44: δ 13 C versus 87 Sr/ 86
Page 141 and 142:
In conclusion, isotopic analysis ha
Page 143 and 144:
(Ugarit/Ras Shamra). Only two studi
Page 145 and 146:
fault and is filled with flood-basa
Page 147 and 148:
Figure 49: Geologic and fault map o
Page 149 and 150:
The Negev Desert in Southern Israel
Page 151 and 152:
The Eastern Mediterranean and the N
Page 153 and 154:
and water and sediment from the Nil
Page 155 and 156:
Figure 55: Contour diagrams for the
Page 157 and 158:
Figure 56: The Sr isotope ratios in
Page 159 and 160:
Figure 58: Schematic diagram along
Page 161 and 162:
strontium data from Betton and Cive
Page 163 and 164:
These flood basalts have 87 Sr/ 86
Page 165 and 166:
Figure 63: Map of the Libyan Desert
Page 167 and 168:
Table 7: Isotopic data of high-grad
Page 169 and 170:
Chapter 11 Analytical Procedures, S
Page 171 and 172:
Table 9: Collagen samples for analy
Page 173 and 174:
USF # Museum Catalog # Table 10: Ap
Page 175 and 176:
Figure 66: KW 1182 (Hippopotamus tu
Page 177 and 178:
Figure 70: KW 3842 (Elephant ivory)
Page 179 and 180:
Chapter 12 Results and Discussion R
Page 181 and 182:
d18O (apatite, per mil) 3 2 1 0 -1
Page 183 and 184:
and hippopotami are grazers. To com
Page 185 and 186:
fetched (with the Nile ≈ +2‰).
Page 187 and 188:
opposed to the 2-3 mg required for
Page 189 and 190:
international environment. The LBA
Page 191 and 192:
ecause they were subject to taxatio
Page 193 and 194:
were other ruling elites (Ratnagar
Page 195 and 196:
scientific archaeometric angle and
Page 197 and 198:
Chapter 13 Conclusion and Suggestio
Page 199 and 200:
compare, the more unique the region
Page 201 and 202:
Aufderheide, A.C., Neiman, F.D., Wi
Page 203 and 204:
Caubet, A., and Poplin, F. 1993. La
Page 205 and 206:
Finley, M.I. 1981. Mycenaean palace
Page 207 and 208:
Horn, P., and Müller-Sohnius, D.,
Page 209 and 210:
Liebowitz, H. 1987. Late Bronze II
Page 211 and 212:
Price, T.D., Grupe, G., and Schröt
Page 213 and 214:
Sherratt, A., and Sherratt, S. 1991
Page 215 and 216:
van der Merwe, N. J., Lee-Thorp, J.
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