Variable Deposition of Amyloid β-Protein (Aβ) with the Carboxy-Terminus that Ends at Residue Valine40 (Aβ40) in the Cerebral Cortex of Patients with Alzheimer's Disease: A Double-Labeling Immunohistochemical Study with Antibodies Specific for Aβ40 and the Aβ that Ends at Residues Alanine42/Threonine43 (Aβ42)

Amyloid -protein (A) deposits in the cerebral cortices of patients with Alzheimer's disease (AD) were investigated immunohistochemically to determine their carboxy terminal sequences. Antibodies specific for A terminating at residue valine₄₀ (A40) and at residues alanine₄₂/threonine₄₃ (A42) were used. Virtually all parenchymal A deposits were positive for A42. Many of these deposits were also partially or completely labeled for A40. The degree of A40 labeling varied from area to area within a given brain and from AD case to AD case. In contrast to parenchymal deposits, A40 labeled essentially all the vascular deposits which constitute amyloid angiopathy (AA), with A42 occurring variably in some of these deposits. Occasional AA was found, however, in which A42 predominated or was exclusively deposited. Such a diversity of A species, both in brain parenchyma and in AA, suggests that multiple C-terminal processing mechanisms occur in the cell types responsible for these deposits.     

In situ biochemical and bacterial variation of sediments enriched with mussel biodeposits

In order to estimate the qualitative variation of sedimented mussel deposits, biochemical and microbial measurements were undertaken after a sediment enrichment with fresh faeces and pseudo-faeces collected in a mussel farming area (Carteau, Gulf of Fos).During two months, cores sampled were investigated at three stations: a first station enriched with mussel deposits, a second considered as a reference station without mussel deposits and occasionally a third corresponding to a continuously enriched sediment under a rope culture.Carbohydrate, organic carbon and nitrogen contents in the sediments gave evidence of a short term variation after sedimentation.Bacterial production increased rapidly at the enriched station and returned to its initial level 8 days later. At this station, exoglucosidasic activity of bacteria, low at the beginning, presented a maximum two weeks after enrichment whereas exoproteolytic activity, which was high in the biodeposits, decreased in the course of the first week. These exoenzymatic activities were significantly higher at the enriched station than at the reference stations. Carbohydrate measurements were in agreement with these results.Degradation rate of biodeposits is discussed on the basis of exoenzymatic activity, organic carbon, nitrogen and free amino acid content at the three stations.     

Neprylisin decreases uniformly in Alzheimer's disease and in normal aging

The proteolysis of beta-amyloid (Abeta) requires neprylisin, an enzyme that has been shown as reduced in Alzheimer's disease (AD). We investigated whether a decrease in neprilysin levels contributes to the accumulation of amyloid deposits not only in AD but also in the normal aging. We analyzed neprilysin mRNA and protein levels in cerebral cortex from 10 cognitively normal elderly subjects with amyloid plaques (NA), 10 cases of AD, and 10 control cases free of amyloid plaques. We found a significant decrease in neprilysin mRNA levels in both AD and NA compared to control cases. Thereby, the defect of neprilysin appears to correlate with Abeta deposition but not with degeneration and dementia.     

Discards of the Algarve (southern Portugal) crustacean trawl fishery

This paper presents the first Holocene continuous record from the southern Bolivian Altiplano. In this area, the climate is now characterized by weak summer monsoon rains. The record is located north of Salar de Uyuni in a non-glacial valley (Rio Baja). Between 11600 and 2210 cal year BP, the rivers accumulated fine deposits, while under the present climatic conditions, the fine particles are carried downstream by strong water floods. These deposits contain a rich diatom flora showing that the valley floor was occupied by paleowetlands. Water input needed to be more or less continuous to explain that the paleowetlands survived over a long period of time. We show that diatoms can be used to reconstruct the relative variations in the water level and the salinity throughout time, despite of the spatial complexity of this type of environment. During the Holocene, the water level was low except during some periods, dated 11600–9800, 6330–5300, and 3110–2210 cal year BP. Saline and freshwater microhabitats were simultaneously present in the valley floor as indicated by a mixed diatom flora evidenced throughout the record. We propose a paleoclimatic scenario based on the assumption that the NE wet atmospheric flow of the monsoon was replaced by the westerlies of the southern hemisphere at the latitude of the study site.     

Mn(II)-oxidizing Bacteria are Abundant and Environmentally Relevant Members of Ferromanganese Deposits in Caves of the Upper Tennessee River Basin

The upper Tennessee River Basin contains the highest density of our nation's caves; yet, little is known regarding speleogenesis or Fe and Mn biomineralization in these predominantly epigenic systems. Mn:Fe ratios of Mn and Fe oxide-rich biofilms, coatings, and mineral crusts that were abundant in several different caves ranged from ca. 0.1 to 1.0 as measured using ICP-OES. At sites where the Mn:Fe ratio approached 1.0 this represented an order of magnitude increase above the bulk bedrock ratio, suggesting that biomineralization processes play an important role in the formation of these cave ferromanganese deposits. Estimates of total bacterial SSU rRNA genes in ferromanganese biofilms, coatings, and crusts measured approximately 7×10⁷–9×10⁹ cells/g wet weight sample. A SSU-rRNA based molecular survey of biofilm material revealed that 21% of the 34 recovered dominant (non-singleton) OTUs were closely related to known metal-oxidizing bacteria or clones isolated from oxidized metal deposits. Several different isolates that promote the oxidation of Mn(II) compounds were obtained in this study, some from high dilutions (10^–8–10^–10) of deposit material. In contrast to studies of caves in other regions, SSU rRNA sequences of Mn-oxidizing bacterial isolates in this study most closely matched those of Pseudomonas, Leptothrix, Flavobacterium, and Janthinobacterium. Combined data from geochemical analyses, molecular surveys, and culture-based experiments suggest that a unique consortia of Mn(II)-oxidizing bacteria are abundant and promoting biomineralization processes within the caves of the upper Tennessee River Basin.     

Autophagy defects in Lafora disease

Lafora disease (LD) is an inherited and fatal form of neurodegenerative disorder characterized by the presence of an abnormal form of glycogen inclusions, called Lafora bodies, in neurons and other tissues. While Lafora bodies have been thought to underlie the neuropathology in LD, the specific process by which these inclusions might affect the neuronal functions was not very well understood. Here we review one of our recent studies on the LD animal model, wherein we have shown that the Lafora bodies might contribute to the impairment in the endosomal–lysosomal and autophagy pathways.     

Calcium translocations during the moulting cycle of the semiterrestrial isopod <Emphasis Type="Italic">Ligia hawaiiensis</Emphasis> (Oniscidea,Crustacea)

Terrestrial isopods moult first the posterior and then the anterior half of the body. During the moulting cycle they retain a significant fraction of cuticular calcium partly by storing it in sternal CaCO₃ deposits. We analysed the calcium content in whole Ligia hawaiiensis and the calcium distribution between the posterior, the anterior ventral, and the anterior dorsal cuticle during four stages of the moulting cycle. The results indicate that: (1) overall, about 80% of the calcium is retained and 20% is lost with the exuviae, (2) in premoult 68% of the calcium in the posterior cuticle is resorbed (23% moved to the anterior ventral cuticle, 17% to the anterior dorsal cuticle, and the remaining 28% to internal tissues), (3) after the posterior moult 83% of the calcium in the anterior cuticle is shifted to the posterior cuticle and possibly to internal storage sites, (4) following the anterior moult up to 54% of the calcium in the posterior cuticle is resorbed and used to mineralise the new anterior cuticle. ⁴⁵Ca-uptake experiments suggest that up to 80% of calcium lost with the anterior exuviae may be regained after its ingestion. Whole body calcium of Ligia hawaiiensis is only 0.7 times that of the fully terrestrial isopods. These terrestrial species can retain only 48% of whole body calcium, suggesting that the amount of calcium that can be retained by shifting it between the anterior and posterior integument is limited. We propose that fully terrestrial Oniscidea rely to a larger degree on other calcium sources like internal stores and uptake from the ingested exuviae.     

Speleothems from Sahastradhara Caves in Siwalik Himalaya,India: Possible Biogenic Inputs

Stalactites and moonmilk from Sahastradhara caves in Siwalik Himalayas were studied to understand the role of microbes in their genesis. Fourier spectroscopy in the moonmilk indicates a complex milieu of organic compounds that is unusual for inorganic formations. Stable C and O isotopes show trends in the moonmilk and stalactite, which suggest biogenic input; the geochemical inference is consistent with evidence from microscopy and laboratory-based microbial cultures. Light microscopy of moonmilk samples show the presence of a number of microbial forms similar to Cyanobacteria, and scanning electron microscope (SEM) images show microbial structures similar to Spirulina. The total number of microbial cells using SYBR Gold is 6.5 × 10⁵ cells, g sed^?1in moonmilk and 3.2 × 10⁵ cells, g sed^?1 in stalactites. FISH indicates approximately 3.5 × 10⁵ cells, g sed^?1 in moonmilk and 2 × 10⁵ cells, g sed^?1 in stalactites. SEM images of the moonmilk indicate a large network of microbial filaments along with minerals, which are identified as calcite based on their x-ray diffraction pattern. In vitro laboratory cultures with pure monogenic strains isolated from the moonmilk and stalactites raise pH in the medium, which facilitate calcite precipitation. The mineral precipitating isolates were identified as: Bacillus pumilis, B. cereus, B. anthracis, B. lentus, B. sphaericus, B. circulans and Actinomycetes. The Sahastradhara moonmilk and statactites are colonized by a diverse microbial community and the isolated bacterial strains induce biomineralization on different nutrient media, supporting their biogenic origin.     

许昌灵井遗址2005年出土石制品的初步研究

本文是灵井遗址2005年出土石制品的初步研究成果。文化遗物埋藏于上、下两套湖相沉积层内。在90m2范围内,共出土石制品2 452件,动物化石(包括人工骨器)约3 000件。石制品采用大石英岩和小脉石英砾石为原料,类型包括石器、石核、石片、断块和石器等。打片和加工采用锤击法,少量采用砸击法。石器毛坯多为断片和断块,多数器型不规则,但也有一些精致加工的小石器。脉石英石器以刮削器为主,还有尖状器、雕刻器、钻器等。石英岩石器以砍砸器为主,兼有手镐和石球。两种石料石器类型形成互补。由于脉石英质石料占主导,石器总体以小型为主。灵井石器工业具有中国北方旧石器时代主工业的特点,部分砾石制作的砍砸器等反映了南方主工业的因素。从地层、遗物和古环境判断,2005年出土的石制品属于旧石器时代晚期,根据上下地层关系分析,本地区不存在中石器文化遗存。