A new ichnotaxon of fossil bird track from the Early Cretaceous Tianjialou Formation （Barremian-Albian）, Shandong Province, China

It is well known that fossil bird tracks are geological records of ancient birds walking on the sediments. Prior to the 1980s, little attention was paid to fossil bird tracks partly because of the difficulties of field discrimination. Over the last decade, new discoveries on the bird origin and early evolution, as well as their relation to dinosaurs[1] have greatly stimulated dinosaur and ancient bird studies.Accordingly, the paleoenvironmental, paleoecological and early evolutional significan…     

Chenguodaite （Ag9FeTe2S4）： a new tellurosulfide mineral from the gold district of East Shandong Peninsula,China

Chenguodaite, approved by IMA-CNMMN （2004-042a）, was discovered in the Bunan quartz vein-type gold deposit in the gold district of East Shandong Peninsula. The mineral occurs in high grade Au-Ag-Cu ores, coexisting with galena, chalcopyrite, hessite, electrum, unnamed Ag6TeS2 and AglsFeBiTe3Se, enclosed and replaced by native silver and acanthite. In the reflected light microscope, the mineral has light gray color, indistinguishable anistropism and hardness around 2-3. The color indices of chenguodaite relative to ICE C illuminator are： x=0.3027, y=0.3076, Y=25.78%,λd=474 nm, Pe=3.68%, similar to those of canfieldite. The average chemical composition from 16 microprobe analyses is Ag8.97Fe1.00Te1.99S4.04, idealized to AggFeTe2S4. The polycrystalline X-ray diffraction of chenguodaite by Gandolfi camera and synchrotron oscillation photography results in 67 reflections with the 12 strongest being （relative intensity in bracket）： 6.742（69）, 6.416（39）, 5.951（33）, 3.265（100）, 2.981（24）, 2.649（22）, 2.25（24）, 2.188（71）, 2.142（22）, 2.123（31）, 2.044（23）, 1.949（33）, which are indexed to a primitive orthorhombic cell with a=12.769 （2） A, b= 14.814（2） A, c= 16.233 （1） A, V= 3070.6 A^3, Z= 9, Dcal.=6.85 g/cm^3. The name is for the late Prof. Chen Guoda, a famous Chinese geologist and the founder of Diwa-Geodepression theory of tectonics.