Notothfix halsei gen. n., sp n., representative of a new family of freshwater cladocerans (Branchiopoda, Anomopoda) from SW Australia, with a discussion of ancestral traits and a preliminary molecular phylogeny of the order

The definitive version is available at www.blackwell-synergy.comThe parthenogenetic female of a new anomopod crustacean, Notothrix halsei gen. n. et sp. n., is described from Lake Angove and found in five other sites in SW Australia. Although macrotrichid-like at first glance, a detailed morphological study including thoracic appendages revealed a set of primitive characters and similarities with primitive families, in particular with the Eurycercidae and Acantholeberidae. Ancestral traits of Notothrix gen. n. comprise: (i) a single large head pore; (ii) second maxilla; (iii) incomplete dorsal merger of valves; (iv) second antenna with a three- and a four-segmented branch; (v) six trunk limbs; (vi) two setae on a sixth endite in the first limb, vs. complete row of posterior setae on the second limb; (vii) large number of setae on exopodites III-V; (viii) well-developed gnathobase V; and (ix) massive postabdomen with wide, telson-like terminus between end-claws that show complex spinulation but no basal spine. Analysis of the complete 18S (SSU) rRNA gene sequence including taxa from all but four anomopod families and using Ctenopoda as an outgroup, confirms our separation of the new taxon, the Nototrichidae fam. n. Although different alignments resulted in different trees, the analyses confirm an isolated position of Notothrix, which has the shortest SSU rRNA gene length known for anomopods. However, the phylogenies derived from a comparison of 18S rRNA gene sequences between families of the order Anomopoda, does not resolve the descent of the various family groups.Kay Van Damme, Russell J. Shiel, H. J. Dumon

Modelling the multiphase near-surface chemistry related to ozone depletions in polar spring

Near-total depletions of ozone have been observed in the Arctic spring since the mid1980s. The autocatalytic reaction cycles involving reactive halogens are now recognized to be of main importance for ozone depletion events in the polar boundary layer. We present sensitivity studies using the model MISTRA in the boxmodelmode on the influence of chemical species on these ozone depletion processes. In order to test the sensitivity of the chemistry under polar conditions, we compared base runs undergoing fluxes of either Br2,BrCl, or Cl2 to induce ozone depletions, with similar runs including a modification of thechemical conditions. The role of HCHO, H2O2, DMS, Cl2, C2H6, HONO, NO2, and RONO2 was investigated. Cases with elevated mixing ratios of HCHO, H2O2, DMS, Cl2, and HONO induceda shift in bromine speciation from Br/BrO to HOBr/HBr, while high mixing ratios of C2H6 induced a shift from HOBr/HBr to Br/BrO. The shifts from Br/BrO to HOBr/HBr accelerated the aerosol debromination, but also increased the total amount of deposited bromine at thesurface (mainly via increased deposition of HOBr). For all NOy species studied (HONO, NO2, RONO2) the chemistry is characterized by an increased bromine deposition on snow reducing the amount of reactive bromine in the air. Ozone is less depleted under conditions of high mixing ratios of NOx. The production of HNO3 led to the acid displacement of HCl, and the release of chlorine out of salt aerosol (Cl2 or BrCl) increased