OfTable A2. Big element composition and Uncommon Earth Elements (REEs) + ZrOfTable A2. Main element

OfTable A2. Big element composition and Uncommon Earth Elements (REEs) + Zr
OfTable A2. Main element composition and Uncommon Earth Components (REEs) + Zr and Nb composition of Shuangshan nepheline syenite. The big element and trace element had been obtained by X-ray fluorescence (XRF) and ICP-MS, respectively, at the State Important Laboratory of Ore Deposit Geochemistry from the Chinese Academy of Sciences. Sample DZ1802 57.26 19.17 4.61 0.75 2.72 6.80 6.00 0.33 0.05 0.47 1.51 99.67 140 254 23 72 ten 1 9 2 12 3 84 8 1 8 1 1143 232 DZ1806 56.70 21.23 4.29 0.72 1.49 5.57 six.68 0.41 0.05 0.26 1.66 99.07 257 458 36 105 15 1 13 2 11 three 69 eight 1 12 2 3447 531 DZ1808 60.38 21.37 3.62 0.32 0.25 7.44 four.12 0.37 0.05 0.30 0.99 99.21 DZ1809 DZ1818 DZ1821 52.66 16.55 6.56 0.85 7.20 4.43 6.00 0.49 0.20 0.38 three.83 99.15 684 1431 160 553 80 9 63 9 51 10 285 29 4 24 3 1230 729 DZ1828 56.76 19.75 5.48 0.69 1.82 six.21 six.70 0.40 0.04 0.58 0.68 99.11 248 358 30 82 11 1 11 2 11 two 79 eight 1 eight 1 2109 451 DZ1830 56.81 19.30 5.20 0.71 2.39 7.54 five.97 0.35 0.05 0.52 0.98 99.83 398 627 53 154 20 2 18 3 17 4 118 12 two 14 two 2568 582 ZK5036 56.11 19.82 five.04 0.37 1.94 7.88 five.27 0.25 0.05 0.50 1.67 98.90 531 791 68 190 25 three 23 three 20 four 137 14 2 15 2 3642SiO2 Al2 O3 TFe2 O3 MgO CaO Na2 O K2 O MnO P2 O5 TiO2 LOI Total La Ce Pr Nd Sm Eu Gd Tb Dy Ho Y Er Tm Yb Lu Zr NbOxide (wt ) 57.53 56.99 17.73 20.10 five.44 three.96 0.55 0.46 3.13 1.30 five.87 3.72 7.05 eight.87 0.52 0.34 0.05 0.09 0.43 0.64 1.21 2.62 99.51 99.09 Trace element ( /g) 279 261 318 458 435 603 42 41 62 123 123 206 17 17 29 two two 3 15 15 24 2 2 three 16 15 19 four three four 120 108 120 12 11 12 two 2 2 15 14 13 2 two 2 2529 2305 1748 787 546
mineralsArticleOnychites from Polish Jura and Their Functional MorphologyPrzemyslaw SztajnerInstitute of Marine and Environmental Sciences, University of Szczecin, 70-383 Szczecin, Poland; [email protected]: Onychites aff. barbatus is excessively rare within the Polish Jura. This paper describes a current uncover from the basal middle Oxfordian. The specimen is preserved within a manner common for other finds of this kind in platy limestones, i.e., as compressed and flattened imprints with remnants of Apricitabine web carbonized organic matter. Great preservation with the surfaces enables a precise reconstruction on the original structure. Accordingly, I hypothesize around the attachment to soft components as well as the function with the belemnite onychites. The high diversity of identified onychites, specially from Europe (NW Tethys), indicates that they served many different purposes. Keywords: onychites; mega-hooks; Belemnitida; functional morphology; Oxfordian; paleogeography1. Introduction Onychites have been first reported by Fraas [1], who described a single species that he named Onychoteuthis barbata. Quenstedt [2] described and illustrated 4BP-TQS supplier Further many species, such as O. barbata. Following subsequent minor revisions, one of the most total of that is that of Engeser [3], at present, ten types represented by quite a few specimens are recognized in the German Jura, ranging in the Pliensbachian to the reduced Tithonian. Further specimens were described from the Arctic (most lately [4]), from New Zealand [5], and, lately, from Poland [6]. Out of 27 specimens of belemnites with preserved arms like arm-hooks known from Europe (mostly Germany), only two bear onychites [5]. Hence, it truly is supposed that onychites had been a sexual feature, discovered in all probability in mature males who may have employed it for competition among one particular a further or for mating, analogous to many arm modifications inside the present-day cephalopods. Presumably, around the basis of th.