This year has seen three studies on high resolution x-ray computed tomography applied to archaeobotany, one using ct-scanning to recovered chaff hidden in ceramics (see Finding Rice Domestication in Clay), and two using a synchrotron to peer inside seeds, including soybeans and horsegram.

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This is actually, quite logical: established stands of pulses could be maintained and wild-type dormant seeds would constitute an established seed, and would recurrently add new plants to the the stand over a series of years. But due to annual human harvests mutations that reduced dormancy would get selected, and would be particularly important for any new populations planted in areas without existing wild populations. In this context we can expect the gradual evolution for thinner coated, more easily germinating seeds through selection across what are presumably multiple loci, as is evident in our archaeological horsegram data (shown left).
Soybean oil content in charred seeds?
The claim for earliest use of a synchrotron to look at charred archaeological pulse seeds, however, goes to our colleagues in China, in collaboration with Prof. Gary Carwford, Shandong archaeobotanist Xuexiang Chen. They argue that soybean underwent selection for increased oil content in prehistory during domestication-- undoubtedly true-- and that this can be tracked archaeological through a change in the number and size of pores visible on the inside of charred soybeans viewed through the synchrotron and High-Resolution Computed Tomography. I remain unconvinced on this last point, and although the paper reports on examination of modern soybeans and, other oily crop seeds, and experimentally charred seeds none of these are illustrated or really described so as to support this interpretation. The authors infer that more small pore is a product of more oil whereas large pores represent burned out protein, but is this true. The differences look to me more like artefacts of carbonization processes, and not a good proxy for the internal anatomy of the original uncharred soybeans. As the few illustrated example suggest larger and irregular pore are present in seeds with more distorted external surface anatomy (e.g. c), whereas small pores are more evident in better preserved examples (e.g. f).
Soybean oil content in charred seeds?
The claim for earliest use of a synchrotron to look at charred archaeological pulse seeds, however, goes to our colleagues in China, in collaboration with Prof. Gary Carwford, Shandong archaeobotanist Xuexiang Chen. They argue that soybean underwent selection for increased oil content in prehistory during domestication-- undoubtedly true-- and that this can be tracked archaeological through a change in the number and size of pores visible on the inside of charred soybeans viewed through the synchrotron and High-Resolution Computed Tomography. I remain unconvinced on this last point, and although the paper reports on examination of modern soybeans and, other oily crop seeds, and experimentally charred seeds none of these are illustrated or really described so as to support this interpretation. The authors infer that more small pore is a product of more oil whereas large pores represent burned out protein, but is this true. The differences look to me more like artefacts of carbonization processes, and not a good proxy for the internal anatomy of the original uncharred soybeans. As the few illustrated example suggest larger and irregular pore are present in seeds with more distorted external surface anatomy (e.g. c), whereas small pores are more evident in better preserved examples (e.g. f).
Unfortunately, the central claim in this
paper does not really add up, or at least are not well justified and
explained in the text. This makes me very nervous about accepting the main
conclusion of the paper, i.e. that the authors have demonstrated an increase in
oil content in soybean during domestication by measuring the quantity of
bubbles (voids) of different sizes in charred archaeological soybeans. Small voids
are attributed to oil content and large voids to protein—but this is never
demonstrated (for example in modern and experimental charred examples) or backed up by citations on soybean anatomy, as to why these voids should differ
between oil and protein. That soybeans are oily, in contrast to most pulses is
clear, but this also has major implications for the nature of archaeological
finds. Most carbonized archaeological soybean are poorly preserved, distorted,
full of large voids and small voids and very shiny on their interior. This is
contrast to pretty much every other pulse I have seen archaeobotanically, from
Vigna spp. to lentils and peas to Lablab. Even in the Chinese samples,
presumably subjected to similar formation processes Vigna angularis seed present typical features of carbonized pulses,
including a dense charred matrix with distinct cotyledons. In Glycine
cotyledons are rarely evident and their interiors are heavily distorted by voids
and bubbles. The obvious deduction is that this state of things is the result
of the oil content in soybeans, and of course many other oily seeds, from
cotton to sesame, also tend to show similar levels of bubbling and porosity
when charred. If large voids in soybean are due to protein burning up during
carbonization then surely one would expect to see this in any pulse, all of
which have at least 20% protein content. It is true that the oil in soybean is
contained in fresh seeds in many small droplets/sacs but upon charring things
are likely to end up being very different. Oils are going to burn to more
readily to gas than carbohydrates or proteins and thus create more bubbles and
explosions of expanding gas. As this progresses and cracks to the outside of the
seed allow penetration of gas (and some oxygen) from the exterior, one would
expect this to speed up. The persistence of small voids then might be predicted
to be the result of less oxidation, less temperature and perhaps other variables of charring conditions of a given seed. Cracking and penetration of gases into
the charring seed may indeed be affected by aspects of domestication—thinning of
seed coat, increase in seed size. Indeed, larger seeds seem likey to leave
larger parts of their interior cotyledons unexposed to exterior cracks and oxygen; and in this context would be expected to preserved more small oil
bubbles as a side effect of seed volume increase: i.e. the difference over time
would reflect preservation artefacts rather than selection for genetic change.
It is hard to see how at this stage we can deduce difference in underlying
phenotype and genetics from this sort of data—at least until we have much
better grasp on who charring conditions affect the distribution of seed
contents, and this calls for some systematic experiments.
Undoubtedly soybeans were selected for oil content, but when
and how this took place in relation to other domestication traits remains sadly
unclear. I find I have to reject to conclusions of Zong et al., although their paper doe illustrate the potential analytical power of using a synchrotron to peer inside archaeological seeds
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