Buseck et al. have "rediscovered" an anaytical method developed in 1947 by Dennis Gabor for defining the morphology of crystals using electron microscopy. Unfortunately, the Buseck et al. paper adds nothing to further the understanding of the issue of life on Mars. It demonstrates that these authors fail to understand the work of Thomas-Keprta et al, 2001 who used a transmission electron microscope to image individual microscopic particles at multiple angles and orientations. From this, the 3-D morphology of the particles could be reconstructed. The technique used by Buseck et al. also uses a transmission electron microscope to image microscopic particles at many different angles in order to reconstruct a 3-D image. These two techniques, for this particular application, are essentially identical.
|In an effort to minimize contamination, sawing of samples in the Antarctic Meteorite Laboratory at JSC is done in a nitrogen cabinet without any type of lubrication.
The Buseck et al. PNAS paper is interesting in that they do not examine ALH84001's population of likely biogenically produced magnetite crystals or the reference MV-1 magnetite crystals; these magnetite populations are the central issues in the debate and without studying either population, at best, their conclusions are irrelevant to the question of life on Mars. Buseck et al. describes the 3-D geometry of a magnetite crystal from "an undescribed, uncultured magnetotactic coccus collected from Sweet Springs Natural Reserve, Morro Bay, CA." It is unclear why they would describe just any magnetite from a previously undescribed strain and compare the geometry of one crystal with one of the best described terrestrial magnetite populations, that of strain MV-1. Buseck et al. are trying to compare a quick study of "oranges (i.e., his undescribed magnetites) with a well-defined study of "apples" (magnetites from ALH84001 and MV-1).
Buseck et al. are trying to lay claim to discovering an analytical method of defining morphology of nanocrystals. Such work has been done for decades using conventional TEM techniques. We see no scientific basis for the Buseck et al. comments "we argue that the existing crystallographic and morphological evidence is inadequate to support the inference of former life on Mars" when he has not examined the magnetites in ALH84001 or MV-1.
|Magnetite crystals produced by terrestrial bacteria look very similar to crystals in ALH84001.
The statement at the conclusion of the Buseck et al. PNAS contribution is another example of researchers trying to use data to refute a scientific hypothesis when the data does not apply to the arguments. One must consider all the lines of evidence used to reach the conclusions. Furthermore, Buseck et al. state that three of the four lines of evidence proposed by McKay et al. 1996 have been refuted; that is incorrect. Gibson et al. 2001 (in Precambrian Research) show additional evidence to support all the original lines of evidence of possible biogenic activity within ALH84001 and its carbonate globules are valid. Additional evidence for possible biogenic activity was also described for two younger Martian meteorites-Nakhla (1.3 billion years old) and Shergotty (165 million years old) in that same report (Gibson et al. 2001).
The Buseck et al. paper appears to be little more than a poorly disguised advertisement for the technique of electron tomography, an attempt to capitalize on the intense debate surrounding the issue of life on Mars to gain publicity. We have been looking forward to the scientific results from Buseck et al. and were very disappointed.
Related Web Pages
Evidence of Martian life dealt critical blow (NAI)
Search for Past Life on Mars (McKay, Thomas-Keptra, et al.)
Mars Meteorites (JPL)