Sublithospheric diamond ages and the supercontinent cycle.

Subduction related to the ancient supercontinent cycle is poorly constrained by mantle samples. Sublithospheric diamond crystallization records the release of melts from subducting oceanic lithosphere at 300-700 km depths and is especially suited to tracking the timing and effects of deep mantle processes on supercontinents. Here we show that four isotope systems (Rb-Sr, Sm-Nd, U-Pb and Re-Os) applied to Fe-sulfide and CaSiO inclusions within 13 sublithospheric diamonds from Juína (Brazil) and Kankan (Guinea) give broadly overlapping crystallization ages from around 450 to 650 million years ago.

Primordial and recycled helium isotope signatures in the mantle transition zone.

Isotope compositions of basalts provide information about the chemical reservoirs in Earth's interior and play a critical role in defining models of Earth's structure. However, the helium isotope signature of the mantle below depths of a few hundred kilometers has been difficult to measure directly. This information is a vital baseline for understanding helium isotopes in erupted basalts.

Deep mantle cycling of oceanic crust: evidence from diamonds and their mineral inclusions.

A primary consequence of plate tectonics is that basaltic oceanic crust subducts with lithospheric slabs into the mantle. Seismological studies extend this process to the lower mantle, and geochemical observations indicate return of oceanic crust to the upper mantle in plumes. There has been no direct petrologic evidence, however, of the return of subducted oceanic crustal components from the lower mantle.

Primary carbonatite melt from deeply subducted oceanic crust.

Partial melting in the Earth's mantle plays an important part in generating the geochemical and isotopic diversity observed in volcanic rocks at the surface. Identifying the composition of these primary melts in the mantle is crucial for establishing links between mantle geochemical 'reservoirs' and fundamental geodynamic processes. Mineral inclusions in natural diamonds have provided a unique window into such deep mantle processes.

[Ellipsoids of the spleen (ellipsoid macrophagal-lymphoid sheaths].

The ellipsoids of the spleen are considered as one of the links of the immune (lymphoid) apparatus of the lymphoreticular organ. Anatomical peculiarities of interrelations between the wall of the terminal part of the arterial bed, capillary, ellipsoid macrophagal-lymphoid microenvironment and reticular stroma of the ellipsoids of the spleen are discussed. Certain ultrastructural and immune-histological differences in the structure of the endothelial lining and cells, forming the ellipsoid sheaths, demonstrate functional interconnection of these formations not only with regulation of blood stream in the spleen vascular bed, but with transport of the antigenic material and lymphocytes into the white pulp.