Nora N. Cesaretti

Tectonic insight based on anisotropy of magnetic susceptibility and compaction studies in the Sierras Australes thrust and fold belt (southwest Gondwana boundary, Argentina)

The Sierras Australes fold and thrust belt (Buenos Aires Province, Argentina) was in the southwestern Gondwanaland margin during the Paleozoic. The Tunas Formation (Permian) is exposed along the eastern part of it and continues eastward beneath the Claromeco Basin. Anisotropy of magnetic susceptibility (AMS) and compaction studies are described and compared with previous paleomagnetic studies with the aim of determining direction and magnitude of the main stresses acting during the sedimentation of the Tunas Formation. The anisotropy ellipsoids are triaxial with oblate or prolate shapes, reflecting different stages of layer parallel shortening during the evolution of the basin. Kmax axes trend NW-SE, parallel to the fold axes, while Kmin move from a horizontal (base) to a vertical orientation at the top of the succession, showing a change from a tectonic to almost a sedimentary fabric. The magnitude of anisotropy and compaction degree decreases toward the top of the succession. The AMS results are consistent with the outcrop structural observations and the compaction and paleomagnetic data. Regional pattern indicates a compression from the SW along this part of Gondwana, with a migration of the orogenic front and attenuation toward the NE in the foreland basin during the Upper Paleozoic. This deformation, locally assigned to the San Rafael noncollisional orogenic phase, is the result of the latitudinal movements toward the Equator of Gondwana (southern plates) and Laurentia (northern plates) during the Permian. This movement is the result of a rearrangement of the microplates that collided with Gondwana during the Late Devonian, to configure Pangea during the Triassic.

Biosilicification (chalcedony) in human cerebral cortex, hippocampus and cerebellum from aged patients.

Aluminum and silicon have been observed to be present in the human degenerated brain and normal elderly brains by using a combination of scanning electron microscopy and X-ray spectrometry (EDS-SEM). Al and Si of electric organs were also reported--in electrocytes and cholinergic nerves--from living electric fish (family Rajidae). A biogenically produced crystalline mineral phase (i.e., chalcedony) has also been observed in electric organs by using a mineralogical microscope. Based on this evidence we decided to explore the presence of chalcedony (SiO2) in the human central nervous system (CNS). Sections from aged patients (mean, 81 years) were collected after autopsy and observed using a Leica DMLP mineralogical microscope. Chalcedony was detected in cerebral cortex and cerebellum. In plane-polarized light, chalcedony is rounded in shape, 12-20 microm in size, translucent, with a low refraction index. The crossed-polarizer image shows first order birefringence color (grey-white) and radial extinction. Chalcedony was also detected in the hippocampus in large amounts and sizes (50-60 microm). Chalcedony is a microcrystalline fibrous form of silica. It consists of nanoscale intergrowths of quartz and the optically length-slow fibrous silica polymorph moganite. Chalcedony precipitation occurs at a specific pH (7-8) and oxidation potential (Eh; 0.0 to -0.2) in geological environments. This observation supports the important role played by pH and Eh conditions in silica precipitation in elderly brains, as has also been reported in peripheral cholinergic nerves in electric organ from living electric fish. Carbonic anhydrases (CAs) (silicase) are involved in physiological pH regulation and may also be participating in the polymerization-depolymerization of chalcedony in the human brain. This is the first time a biogenically produced crystalline mineral phase (i.e., chalcedony) has been observed in the human CNS from aged patients.