Bataksch leesboek, bevattende stukken in het Tobasch, Mandailingsch en Dairisch.

Mode of access: Internet.

Charter of the province of Pennsylvania.

Mode of access: Internet.

Geological and trace element evidence for a marine sedimentary environment of deposition and biogenicity of 3.45 Ga stromatolitic carbonates in the Pilbara Craton, and support for a reducing Archaean ocean

Bedded carbonate rocks from the 3.45 Ga Warrawoona Group, Pilbara Craton, contain structures that have been regarded either as the oldest known stromatolites or as abiotic hydrothermal deposits. We present new field and petrological observations and high-precision REE + Y data from the carbonates in order to test the origin of the deposits. Trace element geochemistry from a number of laminated stromatolitic dolomite samples of the c. 3.40 Ga Strelley Pool Chert conclusively shows that they precipitated from anoxic seawater, probably in a very shallow environment consistent with previous sedimentological observations. Edge-wise conglomerates in troughs between stromatolites and widespread cross-stratification provide additional evidence of stromatolite construction, at least partly, from layers of particulate sediment, rather than solely from rigid crusts. Accumulation of particulate sediment on steep stromatolite sides in a high-energy environment suggests organic binding of the surface. Relative and absolute REE + Y contents are exactly comparable with Late Archaean microbial carbonates of widely agreed biological origin. Ankerite from a unit of bedded ankerite–chert couplets from near the top of the stratigraphically older (3.49 Ga) Dresser Formation, which immediately underlies wrinkly stromatolites with small, broad, low-amplitude domes, also precipitated from anoxic seawater. The REE + Y data of carbonates from the Strelley Pool Chert and Dresser Formation contrast strongly with those from siderite layers in a jasper–siderite–Fe-chlorite banded iron-formation from the base of the Panorama Formation (3.45 Ga), which is clearly hydrothermal in origin. The geochemical results, together with sedimentological data, strongly support: (1) deposition of Dresser Formation and Strelley Pool Chert carbonates from Archaean seawater, in part as particulate carbonate sediment; (2) biogenicity of the stromatolitic carbonates; (3) a reducing Archaean atmosphere; (4) ongoing extensive terrestrial erosion prior to ∼3.45 Ga.

Evaluación poblacional de Ensis macha (Molina, 1782) en bahía Independencia-Pisco, 2010

Entre octubre y noviembre 2010 se realizó una evaluación poblacional de la concha navaja (Ensis macha) para determinar distribución, abundancia y estructura poblacional en los bancos naturales de bahía Independencia, empleando el muestreo al azar. Se colectó 672 individuos, la longitud valvar fluctuó entre 9 y 186 mm, promedio 126,2 mm, el 20,2% de ejemplares presentaron tallas menores a la mínima de extracción (≥120 mm). Las concentraciones variaron entre 0,5 y 76,5 ind.m-2, el área con mayor densidad promedio fue Balsero (12,5 ind.m-2), seguido de Canastones (3,6 ind.m-2), Morro Quemado (1,9 ind.m-2) y Tunga (1,5 ind.m-2). La biomasa relativa osciló entre 6,6 y 2.210,2 g.m-2, la mayor biomasa promedio se registró en Balsero con 359,7 g.m-2. La población y biomasa total fueron estimadas en 17,55 millones (±35,3%), y 498,65 t (±37,5%), respectivamente. En Morro Quemado, el recurso no se ha recuperado a pesar de la veda establecida en el litoral de Pisco (R.M. Nº 661-2008-PRODUCE); mientras que en Balsero se observaron signos de recuperación

Cartes gravées. Les environs de Naples de Pellegrino + L'Acarnanie, Cephalonie de Coronelli, carte ( ?) de Van Keulen + Isles Rhodienne de Delisle / [par Vincenzo Coronelli, Guillaume Delisle, Jean-Baptiste d'Anville]

Échelle(s) : [Echelles diverses]

Ejercicio diario en honor de la Santísima Trinidad, Santísimo Sacramento, Santísima Virgen María y demás angeles y santos ; van añadidos algunos documentos para vivir santamente

UANL

Delocalization of a hole in van der Waals clusters: Ionization potential of rare-gas and small Hg_n clusters

The size dependence of the ionization potential I_p(n) of van der Waals (vdW) bound clusters has been calculated by using a model Hamiltonian, which includes electron hopping, vdW interactions, and charge-dipole interactions. The charge-density and dipole-density distributions for both neutral and ionized n-atom clusters are determined self-consistently. The competition between the polarization energy of the neutral atoms surrounding a partially localized hole and the tendency toward hole delocalization in the ionized clusters is found to dominate the size dependence of I_p(n). To test our theory, we culculate I_p(Xe_n) and I_p(Kr_n) for n \le 300. Good quantitative agreement with experiment is obtained. The theory is also applied to calculate I_p(Hg_n). Comparison with experiments suggests that in Hg_n^+ clusters with n \le 20 the positive charge is mainly distributed within a trimer which is situated at the center of the cluster and which polarizes the n - 3 surrounding neutral atoms.

Slave-boson approach to the size-dependent transition from van der Waals to covalent bonding in Hg_n clusters

We use a microscopic theory to describe the dynamics of the valence electrons in divalent-metal clusters. The theory is based on a many-body model Harniltonian H which takes into account, on the same electronic level, the van der Waals and the covalent bonding. In order to study the ground-state properties of H we have developed an extended slave-boson method. We have studied the bonding character and the degree of electronic delocalization in Hg_n clusters as a function of cluster size. Results show that, for increasing cluster size, an abrupt change occurs in the bond character from van der Waals to covalent bonding at a critical cluster size n_c ~ 10-20. This change also involves a transition from localized to delocalized valence electrons, as a consequence of the competition between both bonding mechanisms.