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No. 237 Maritime Archaeology in the People's Republic of China ...

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Appendix 2. Wood identification<br />

Three samples <strong>of</strong> wood, one excavated from a wreck site <strong>in</strong><br />

Ch<strong>in</strong>a (Bai Jiao 1) and two obta<strong>in</strong>ed from dredge operators,<br />

were exam<strong>in</strong>ed to determ<strong>in</strong>e <strong>the</strong>ir wood type. Of <strong>the</strong> samples<br />

recovered by dredg<strong>in</strong>g <strong>the</strong> th<strong>in</strong>ner <strong>of</strong> <strong>the</strong> two samples is solid<br />

and <strong>in</strong> very good condition whilst <strong>the</strong> o<strong>the</strong>r sample is s<strong>of</strong>t and<br />

appears to be quite degraded. Sample Bai Jiao 1 is encrusted<br />

with concretion and also appears to be quite degraded. A small<br />

piece was removed from each sample and <strong>the</strong> transverse section<br />

polished to a 1200 grit f<strong>in</strong>ish prior to low power microscopic<br />

exam<strong>in</strong>ation. Where possible, radial and tangential longitud<strong>in</strong>al<br />

surfaces were sectioned (microtome) and slides prepared for<br />

high power microscopic exam<strong>in</strong>ation. The results <strong>of</strong> <strong>the</strong>se<br />

exam<strong>in</strong>ations are described below.<br />

Dredge Timbers<br />

tr a n S v e r S e Su r fa C e<br />

Samples A and B possessed identical features res<strong>in</strong> canals<br />

were present, with <strong>the</strong> majority <strong>in</strong> <strong>the</strong> more dense late wood<br />

bands. The bands <strong>of</strong> late wood had approximately <strong>the</strong> same<br />

dimensions as those <strong>of</strong> <strong>the</strong> early wood and <strong>the</strong>re was a very<br />

clear demarcation between <strong>the</strong> late and <strong>the</strong> early wood. The<br />

greater degree <strong>of</strong> degradation <strong>of</strong> Sample B was demonstrated<br />

by <strong>the</strong> substantial collapse and distortion (sideways collapse)<br />

<strong>of</strong> <strong>the</strong> early wood sections. Th<strong>in</strong> epi<strong>the</strong>lial cells surround <strong>the</strong><br />

res<strong>in</strong> canals.<br />

ra d i a l lo n G i t u d i n a l Su r fa C e<br />

Despite its apparently good condition a suitable slide could<br />

not be made <strong>of</strong> Sample A. A slide <strong>of</strong> Sample B showed <strong>the</strong><br />

presence <strong>of</strong> smooth-walled ray tracheids and large w<strong>in</strong>dowlike<br />

simple pits <strong>in</strong> <strong>the</strong> ray parenchyma. A polished section <strong>of</strong><br />

Sample B confirmed <strong>the</strong> presence <strong>of</strong> similar pits <strong>in</strong> <strong>the</strong> ray<br />

parenchyma <strong>of</strong> this sample but <strong>the</strong> nature <strong>of</strong> <strong>the</strong> walls <strong>of</strong> <strong>the</strong><br />

ray tracheids could not be determ<strong>in</strong>ed ow<strong>in</strong>g to <strong>the</strong> lack <strong>of</strong><br />

def<strong>in</strong>ition produced by polish<strong>in</strong>g.<br />

The size <strong>of</strong> <strong>the</strong> res<strong>in</strong> canals and <strong>the</strong> th<strong>in</strong> nature <strong>of</strong> <strong>the</strong><br />

epi<strong>the</strong>lial cells <strong>in</strong>dicate that <strong>the</strong> sample is a p<strong>in</strong>e ra<strong>the</strong>r than<br />

a larch, spruce or Douglas fir. The size and demarcation <strong>of</strong><br />

<strong>the</strong> late wood bears most resemblance to that <strong>of</strong> <strong>the</strong> pitch<br />

p<strong>in</strong>es. The features observed <strong>in</strong> <strong>the</strong> radial section however<br />

are typical <strong>of</strong> s<strong>of</strong>t p<strong>in</strong>es <strong>of</strong> <strong>the</strong> yellow p<strong>in</strong>e type. On <strong>the</strong> basis<br />

<strong>of</strong> <strong>the</strong> microscopic anatomical features this sample is more<br />

likely to be a yellow ra<strong>the</strong>r than a pitch p<strong>in</strong>e. P<strong>in</strong>es <strong>of</strong> <strong>the</strong><br />

yellow p<strong>in</strong>e type <strong>in</strong>clude P<strong>in</strong>us strobus L. (yellow p<strong>in</strong>e), P.<br />

lambertiana Dougl. (sugar p<strong>in</strong>e), P. monticola Dougl. (western<br />

white p<strong>in</strong>e), P. cembra L.v. sibirica Loud. and P. koraiensis<br />

Sieb. et Zucc. (Siberian yellow p<strong>in</strong>e, Siberian p<strong>in</strong>e, Korean<br />

p<strong>in</strong>e, Manchurian p<strong>in</strong>e). The latter group <strong>of</strong> p<strong>in</strong>es are native<br />

to Siberia and eastern Asia. Yellow p<strong>in</strong>e is low <strong>in</strong> strength and<br />

works easily but is not resistant to decay.<br />

Bai Jiao 1<br />

tr a n S v e r S e Su r fa C e<br />

The sample is a highly degraded s<strong>of</strong>twood. Although areas <strong>of</strong><br />

degradation on <strong>the</strong> transverse surface resembled res<strong>in</strong> canals<br />

none could be positively identified. There is an abrupt transition<br />

between <strong>the</strong> early wood and <strong>the</strong> late wood with a much greater<br />

abundance <strong>of</strong> <strong>the</strong> early wood. Rays are clearly visible.<br />

ta n G e n t i a l lo n G i t u d i n a l Su r fa C e<br />

Predom<strong>in</strong>antly uniseriate rays observed, rang<strong>in</strong>g <strong>in</strong> height<br />

from 6 to 25 cells high.<br />

ra d i a l lo n G i t u d i n a l Su r fa C e<br />

Evidence <strong>of</strong> spiral thicken<strong>in</strong>g <strong>in</strong> <strong>the</strong> axial tracheids. Cupressoid<br />

cross-field pits were observed <strong>in</strong> <strong>the</strong> ray parenchyma.<br />

The features identified above are found <strong>in</strong> yews (Taxus<br />

sp). Thus although <strong>the</strong> sample is highly degraded it is likely<br />

to be <strong>of</strong> this timber type. Yew occurs commonly <strong>in</strong> western<br />

and central Europe and less commonly <strong>in</strong> western Asia and<br />

<strong>No</strong>rth Africa. It is a strong, durable and resilient wood that is<br />

resistant to splitt<strong>in</strong>g.<br />

91

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