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1.<P style=&quot;MARGIN: 0cm 0cm 0pt; mso-pagination: widow-orphan; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-outline-level: 2&quot; class=MsoNormal>ot;COLOR: black; FONT-SIZE: 14pt; mso-font-kerning: 18.0pt; mso-bidi-font-weight: bold&quot; lang=EN-US>ot;Times New Roman&quot;>Affirmation of Pterospathodus eopennatus Zone (Conodonta) and the Age of the Silurian Shamao Formation in pace prefix = st1 ns = &quot;urn:schemas-microsoft-com:office:smarttags&quot; />place w:st=&quot;on&quot;>ot;on&quot;>Zigui, ot;on&quot;>Hubeiplace> as Well as the Correlation of the Related Strataot;mso-spacerun: yes&quot;>&nbsp; pace prefix = o ns = &quot;urn:schemas-microsoft-com:office:office&quot; /><o:p>o:p>

2.<P style=&quot;MARGIN: 0cm 0cm 0pt; mso-pagination: widow-orphan; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-outline-level: 2&quot; class=MsoNormal>ot;COLOR: black; FONT-SIZE: 14pt; mso-font-kerning: 18.0pt; mso-bidi-font-weight: bold&quot; lang=EN-US>ot;Times New Roman&quot;>Affirmation of Pterospathodus eopennatus Zone (Conodonta) and the Age of the Silurian Shamao Formation in pace prefix = st1 ns = &quot;urn:schemas-microsoft-com:office:smarttags&quot; />place w:st=&quot;on&quot;>ot;on&quot;>Zigui, ot;on&quot;>Hubeiplace> as Well as the Correlation of the Related Strataot;mso-spacerun: yes&quot;>&nbsp; pace prefix = o ns = &quot;urn:schemas-microsoft-com:office:office&quot; /><o:p>o:p>

3.<P style=&quot;MARGIN: 0cm 0cm 0pt; mso-pagination: widow-orphan; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-outline-level: 2&quot; class=MsoNormal>ot;FONT-FAMILY: 宋体; COLOR: black; FONT-SIZE: 12pt; mso-font-kerning: 18.0pt; mso-bidi-font-family: 宋体&quot; lang=EN-US>A New Burgess Shale-Type Biota from the Upper Shilongdong Formation, Lower Cambrian of pace prefix = st1 ns = &quot;urn:schemas-microsoft-com:office:smarttags&quot; />ot;on&quot;>Central ot;on&quot;>Hubei pe w:st=&quot;on&quot;>Provincepe>, South ountry-region w:st=&quot;on&quot;>place w:st=&quot;on&quot;>Chinaplace>ountry-region>pace prefix = o ns = &quot;urn:schemas-microsoft-com:office:office&quot; /><o:p>o:p>

4.<P style=&quot;MARGIN: 0cm 0cm 0pt; mso-pagination: widow-orphan; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-outline-level: 2&quot; class=MsoNormal>ot;FONT-FAMILY: 宋体; COLOR: black; FONT-SIZE: 12pt; mso-font-kerning: 18.0pt; mso-bidi-font-family: 宋体&quot; lang=EN-US>A New Burgess Shale-Type Biota from the Upper Shilongdong Formation, Lower Cambrian of pace prefix = st1 ns = &quot;urn:schemas-microsoft-com:office:smarttags&quot; />ot;on&quot;>Central ot;on&quot;>Hubei pe w:st=&quot;on&quot;>Provincepe>, South ountry-region w:st=&quot;on&quot;>place w:st=&quot;on&quot;>Chinaplace>ountry-region>pace prefix = o ns = &quot;urn:schemas-microsoft-com:office:office&quot; /><o:p>o:p>

5.<P style=&quot;MARGIN: 0cm 0cm 0pt; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-pagination: widow-orphan; mso-outline-level: 2&quot; class=MsoNormal>ot;FONT-FAMILY: 宋体; COLOR: black; FONT-SIZE: 12pt; mso-bidi-font-family: 宋体; mso-font-kerning: 18.0pt&quot; lang=EN-US>The Origin and Cambrian Explosion of Animals: Fossil Evidences from pace prefix = st1 ns = &quot;urn:schemas-microsoft-com:office:smarttags&quot; />ountry-region w:st=&quot;on&quot;>place w:st=&quot;on&quot;>Chinaplace>ountry-region>pace prefix = o ns = &quot;urn:schemas-microsoft-com:office:office&quot; /><o:p>o:p>

6.<P style=&quot;MARGIN: 0cm 0cm 0pt; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-pagination: widow-orphan; mso-outline-level: 2&quot; class=MsoNormal>ot;FONT-FAMILY: 宋体; COLOR: black; FONT-SIZE: 12pt; mso-bidi-font-family: 宋体; mso-font-kerning: 18.0pt&quot; lang=EN-US>The Origin and Cambrian Explosion of Animals: Fossil Evidences from pace prefix = st1 ns = &quot;urn:schemas-microsoft-com:office:smarttags&quot; />ountry-region w:st=&quot;on&quot;>place w:st=&quot;on&quot;>Chinaplace>ountry-region>pace prefix = o ns = &quot;urn:schemas-microsoft-com:office:office&quot; /><o:p>o:p>

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