Karyological Features of Achyrocline (Asteraceae, Gnaphalieae): stable karyotypes, low DNA content variation and linkage of rRNA genes.

Many Achyrocline (Asteraceae, tribe Gnaphalieae) species are widely used in Argentina, Brazil and Uruguay as popular medicinal and aromatic plants. Achyrocline flaccida, A. satureioides, A. alata, and A. crassiuscula are distributed in Uruguay and popularly known as 'marcelas'. In order to characterize them, we performed chromosome counts, compared the karyotypes, mapped the 5S and 45S rDNA sites by fluorescent in situ hybridization, and estimated their DNA content. All species were diploid with 2n = 28 chromosomes, this being the first report for A. flaccida and A. crassiuscula. All species showed symmetrical karyotypes composed exclusively of biarmed chromosomes. DNA content estimated by flow cytometry revealed 2C values ranging from 5.73 to 6.03 pg, the amounts for A. alata and A. crassiuscula being higher than those for the other species. Cytogenetic mapping of 5S and 45S rDNA sequences in three species, A. flaccida, A. satureioides and A. alata, showed that in these species both sites co-localized in the pericentromeric region of chromosome 10. This site corresponds to the only DAPI(-) and CMA(+) band of their genomes. Southern blot hybridization of 5S and 45S rDNA on BamHI digested genomic DNA confirmed the tight linkage of these rDNA families into a single unit. Cytological data indicate that Achyrocline species are karyologically poorly differentiated, whereas the uncommon distribution of 5S and 45S rDNA suggests a close relationship with other genera of the Anthemidae tribe.

Impact of millennial mining activities on sediments and microfauna of the Tinto River estuary (SW Spain).

In this paper, we analyze two short cores collected in the Tinto estuary (SW Spain), and describe the palaeoenvironmental evolution of this area during the last two millennia, along with the influence of historical mining activities and recent industrial pollution on sediments and microfauna (foraminifera and ostracoda). Although there were no significant changes in the distribution of microorganisms, a first pollution period (0-150 AD) was recorded in high sediment pollution by Cu in the shallow palaeochannels of the middle estuary. During this period and the following 1700 years, tolerant pioneer species of both foraminifera and ostracoda were found predominantly in the inner, protected areas of the estuary, while the bottom sediments were subjected to high hydrodynamic gradients, and consequently showed lower density and diversity of organisms. In the last 150 years, acid mine drainage processes, introduction of a new mining period, and the polluted inputs derived from two industrial processes resulted in increased heavy metal contamination of the bottom sediments, and corresponding extirpation of ostracodes and restriction of foraminifers to the inner zones of the estuary.

Origin of the anomalies in light and middle REE in sediments of an estuary affected by phosphogypsum wastes (south-western Spain).

Sc, Y, Th, Cu and rare earth elements (REE) concentrations have been analyzed in 14 samples of surface sediments and in two gravity cores by means of ICP-MS. Mean concentrations of Sc, Y and Th in surface sediments are 6.23, 4.76 and 16.30 ppm, respectively, lower than those present in the Upper Continental Crust (UCC). Cu concentration in these sediments is very high, 1466 ppm, and is caused by inputs from the Odiel and Tinto rivers, affected by acid mine drainage. SigmaREE mean concentration is 106.8 ppm, lower than that observed in other rivers and estuaries. In the cores, Sc, Y and Th concentrations show a significant increase in the intermediate levels, between 10 and 40 cm depth. The same pattern exists with Cu, where concentrations of 4440 ppm can be reached. Vertical evolution patterns for Sc, Y, Cu and heavy REE (HREE) are similar, and contrary to those shown by Th, light REE (LREE) and middle REE (MREE). Plots of North American Shale Composite (NASC)-normalized REE data of surface sediments show a slight depletion in REE concentrations. Most samples present with middle REE enrichment relative to light REE and heavy REE. Conversely, samples of the intermediate levels of the cores show significant enrichment of REE relative to NASC and high values in the (La/Gd)NASC and (La/Yb)NASC ratios. These anomalies in the fractionation patterns caused by enrichments in LREE and MREE concentrations is related to the presence of high concentrations of Th. They were generated by effluents from fertilizer factories between 1968 and 1998 which used phosphorite as source material.