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1.PAN style="COLOR: black; FONT-SIZE: 14pt; mso-font-kerning: 18.0pt; mso-bidi-font-weight: bold" lang=EN-US>Paleoenviromental and Paleoclimatic Changes inl:namespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />place w:st="on"> laceName w:st="on">Xingkai place w:st="on">laceType w:st="on">LakelaceType>place>laceName>place> Inferred from Stable Carbon and Nitrogen Isotopes of Bulk Organic Matter since le="COLOR: red; FONT-SIZE: 14pt; mso-font-kerning: 18.0pt; mso-bidi-font-weight: bold" lang=EN-US>28 ka B.P.le="COLOR: red; FONT-SIZE: 14pt" lang=EN-US>l:namespace prefix = o ns = "urn:schemas-microsoft-com:office:office" />p>p>
2.PAN style="COLOR: black; FONT-SIZE: 14pt; mso-font-kerning: 18.0pt; mso-bidi-font-weight: bold" lang=EN-US>Paleoenviromental and Paleoclimatic Changes inl:namespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />place w:st="on"> laceName w:st="on">Xingkai place w:st="on">laceType w:st="on">LakelaceType>place>laceName>place> Inferred from Stable Carbon and Nitrogen Isotopes of Bulk Organic Matter since le="COLOR: red; FONT-SIZE: 14pt; mso-font-kerning: 18.0pt; mso-bidi-font-weight: bold" lang=EN-US>28 ka B.P.le="COLOR: red; FONT-SIZE: 14pt" lang=EN-US>l:namespace prefix = o ns = "urn:schemas-microsoft-com:office:office" />p>p>
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5.<P 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>le="FONT-FAMILY: 宋体; COLOR: black; FONT-SIZE: 12pt; mso-font-kerning: 18.0pt; mso-bidi-font-family: 宋体" lang=EN-US>Productivity of l:namespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />laceName w:st="on">Paleo-SongliaolaceName> laceType w:st="on">LakelaceType> During the Late Cretaceous in Well Songke-1, place w:st="on">laceName w:st="on">SongliaolaceName> laceType w:st="on">BasinlaceType>place>l:namespace prefix = o ns = "urn:schemas-microsoft-com:office:office" />p>p>
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