Table Of Content

Available online at www.sciencedirect.com Sedimen science @oinecr: Geology Sedimentary Geology 178 (2005) 315-316 www.elsevier.com/locate/sedgeo Contents Volume 178 (2005) Publisher’s note RE eA a ig ins wea a a hea eran e Chee ee ri Okmi S Col n eel pie gg a i Gh Unupayiyl ett g Arena cer aig l Publisher’s note IN 99 0B Fe eei nn i des oa RE me bike Oa yl ad gi i a AS alles ke Ree hatte si gee tang Research Papers Steep microbial boundstone-dominated platform margins—examples and implications SPs Tee, Fates ERS as Ga, TE eee we eer es 5 High-frequency cyclicity in the latest Messinian Adriatic foreland basin: Insight into palaeoclimate and palaeoenvironments of the Mediterranean Lago-Mare episode ee ee eee ee er ee 31 Automicrites in modern cyanobacterial stromatolitic deposits of Rangiroa, Tuamotu Archipelago, French Polynesia: Biochemical parameters underlaying their formation II UI aig id Se. bce eee A oe teh kh SR KN BS LE ee ee ee a 33 Sedimentary environment and diagenesis of the Lower Cretaceous Chaswood Formation, southeastern Canada: The origin of kaolin-rich mudstones ee re eo OE i ee bm Fae el RE OO aS Oe oD we ee ws 75 Environmental and diagenetic records from a new reference section for the Boreal realm: The Campanian chalk of the Mons basin (Belgium) Is ei I I ag eter a ress eh hcg h mm eed hoa ih wn wo SR wee a me ea 99 Metazoan—microbial framework fabrics in a Mississippian (Carboniferous) coral-sponge—microbial reef, Monto, Queensland, Australia er ee I, I cy etc waa ge lS eats ae Lee e rae oye e alae kins TyW hee. Se a.S e Re wD 113 Discussions Sea level changes versus hydrothermal diagenesis: Origin of Triassic carbonate platform cycles in the Dolomites, Italy—Discussion ee ee nes 0k, I nw ae ee ele ee ee ae ee 135 Sea level changes versus hydrothermal diagenesis: Origin of Triassic carbonate platform cycles in the Dolomites, Italy a ee a re Og aS aa haere eae a Ce ce age Peas ysS ara dk ig Gone e Ow eee 8 8 141 Sea level changes versus hydrothermal diagenesis: Origin of Triassic carbonate platform cycles in the Dolomites, Italy: Discussion a I oe, eee Ge a ok ee a RE WO we eR eS 145 Sea level changes versus hydrothermal diagenesis: Origin of Triassic carbonate platform cycles in the Dolomites, Italy ea eel Pe ee a hdr hf a Ae dW pA WK NCR kee EO Oa a Oe AR OE So ee ass 151 Erratum Erratum to “A genetic classification of carbonate platforms based on their basinal and tectonic settings in the Cenozoic” [Sedimentary Geology Volume 175 (2005) 49-72] EN oN turn teen eins hate AIG rk gw ia a Uy wing ala Oe yiarey Rew 155 doi: 10.1016/S0037-0738(05)00236-8 316 Contents Volume 178 (2005) Research Papers Expression and modelling of stratigraphic sequence distortion C. Robin, D. Rouby, D. Granjeon, F. Guillocheau, P. Allemand and S. Raillard..................0.... 159 Advance and application of the stratigraphic simulation model 2D-SedFlux: From tank experiment to geological scale simulation 1. eee, Fie Cel y. te. ees Ree Be SPOON oc ke ER ek ee ee es 187 A model of early calcite cementation in alluvial fans: Evidence from the Burdigalian sandstones and limestones of the Vallés-Penedés half-graben (NE Spain) ee a sg poe wh ky gd “Sk Aw AUR Soe be AA OO Dk Rv Rea ae eS 197 Condensation and phosphatization of the Middle and Upper Ordovician limestones on the Malopolska Block (Poland): Response to paleoceanographic conditions I ise Ee iS Ca TN eb Go ek Nw ce We AAAS SD AEE Oe AE ERE ORNS RTS 219 Carbonate-cemented stylolites and fractures in the Upper Jurassic limestones of the Eastern Iberian Range, Spain: A record of palaeofluids composition and thermal history R. Marfil, M.A. Caja, M. Tsige, I.S. Al-Aasm, T. Martin-Crespo and R. Salas....................04. 237 Sedimentary features of tsunami backwash deposits in a shallow marine Miocene setting, Mejillones Peninsula, northern Chile anne eG og yh ida WeE thie eos Ge w+ oe Sew ene bere elk ie ee 259 Unexpected trend in the compositional maturity of second-cycle sand ee kg hg Sg Wn We Pi ole hg OW EP ES LAD Ss 8 OR Oe aR 275 Grains in motion: A review RENE ie SPE ADEA US Ae OnE ge MO IRN wg Nes aOR SOME ONM ae as nC aOR SRY Pee gE orP EE ee Renee ot nt eee Ere 9° 8, SRS Me RSS Oe De ORO OO ER a Be Ce Oe we ee ee Be ek ee eee i Se eS ee, ee Ge