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style="MARGIN: 0cm 0cm 0pt; mso-pagination: widow-orphan; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-outline-level: 2" class=MsoNormal>style="FONT-FAMILY: 宋体; COLOR: black; FONT-SIZE: 12pt; mso-font-kerning: 18.0pt; mso-bidi-font-family: 宋体" lang=EN-US>New Isoxys (Arthropoda) from the Cambrian Mantou Formation, space prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" /><st1:place w:st="on"><st1:PlaceName w:st="on">Shandongst1:PlaceName> <st1:PlaceType w:st="on">Provincest1:PlaceType>st1:place>space prefix = o ns = "urn:schemas-microsoft-com:office:office" />

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style="MARGIN: 0cm 0cm 0pt; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-pagination: widow-orphan; mso-outline-level: 2" class=MsoNormal>style="FONT-FAMILY: 宋体; COLOR: black; FONT-SIZE: 12pt; mso-bidi-font-family: 宋体; mso-font-kerning: 18.0pt" lang=EN-US>Oligocene-Pliocene Sedimentary Facies Analysis and Sedimentary Evolution of space prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" /><st1:place w:st="on"><st1:PlaceName w:st="on">Xunhuast1:PlaceName> <st1:PlaceType w:st="on">Basinst1:PlaceType>st1:place> in Northeastern Margin of Qinghai-Tibet Plateauspace prefix = o ns = "urn:schemas-microsoft-com:office:office" />

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