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tyle="MARGIN: 0cm 0cm 0pt" class=MsoNormal>tyle="COLOR: black; mso-font-kerning: 18.0pt" lang=EN-US>t;Times New Roman">Proposal to Further Investigate the Cretaceous-Paleogene Boundary Section at t1 ns = "urn:schemas-microsoft-com:office:smarttags" />t1:place w:st="on">t1:City w:st="on">Dangyangt1:City>, tyle="mso-spacerun: yes"> t1:State w:st="on">Hubeit1:State>t1:place> Provincetyle="FONT-SIZE: 14pt" lang=EN-US>t;urn:schemas-microsoft-com:office:office" />
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tyle="MARGIN: 0cm 0cm 0pt" class=MsoNormal>tyle="COLOR: black; mso-font-kerning: 18.0pt" lang=EN-US>t;Times New Roman">Proposal to Further Investigate the Cretaceous-Paleogene Boundary Section at t1 ns = "urn:schemas-microsoft-com:office:smarttags" />t1:place w:st="on">t1:City w:st="on">Dangyangt1:City>, tyle="mso-spacerun: yes"> t1:State w:st="on">Hubeit1:State>t1:place> Provincetyle="FONT-SIZE: 14pt" lang=EN-US>t;urn:schemas-microsoft-com:office:office" />
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tyle="MARGIN: 0cm 0cm 0pt; mso-pagination: widow-orphan; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-outline-level: 2" class=MsoNormal>tyle="FONT-FAMILY: 宋体; COLOR: black; FONT-SIZE: 12pt; mso-font-kerning: 18.0pt; mso-bidi-font-family: 宋体" lang=EN-US>Paleoenvironmental and Paleoclimatic Changes During 47tyle="FONT-FAMILY: 宋体; COLOR: black; FONT-SIZE: 12pt; mso-font-kerning: 18.0pt; mso-bidi-font-family: 宋体">～25 ka BP as Indicated by Jing’erwa Section in Nihewan Basint;urn:schemas-microsoft-com:office:office" />
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tyle="MARGIN: 0cm 0cm 0pt; mso-pagination: widow-orphan; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-outline-level: 2" class=MsoNormal>tyle="FONT-FAMILY: 宋体; COLOR: black; FONT-SIZE: 12pt; mso-font-kerning: 18.0pt; mso-bidi-font-family: 宋体" lang=EN-US>Paleoenvironmental and Paleoclimatic Changes During 47tyle="FONT-FAMILY: 宋体; COLOR: black; FONT-SIZE: 12pt; mso-font-kerning: 18.0pt; mso-bidi-font-family: 宋体">～25 ka BP as Indicated by Jing’erwa Section in Nihewan Basint;urn:schemas-microsoft-com:office:office" />
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tyle="MARGIN: 0cm 0cm 0pt; mso-pagination: widow-orphan; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-outline-level: 2">tyle="FONT-SIZE: 12pt; COLOR: black; FONT-FAMILY: 宋体; mso-font-kerning: 18.0pt; mso-bidi-font-family: 宋体">Organic Matter Types of Core SBt1 ns = "urn:schemas-microsoft-com:office:smarttags" />t1:chmetcnv w:st="on" TCSC="0" NumberType="1" Negative="True" HasSpace="True" SourceValue="1" UnitName="in">-01 int1:chmetcnv> the t1:place w:st="on">t1:PlaceName w:st="on">Sanshuit1:PlaceName> t1:PlaceType w:st="on">Basint1:PlaceType>t1:place> and Their Paleoclimate Implicationst;urn:schemas-microsoft-com:office:office" />
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tyle="MARGIN: 0cm 0cm 0pt; mso-pagination: widow-orphan; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-outline-level: 2">tyle="FONT-SIZE: 12pt; COLOR: black; FONT-FAMILY: 宋体; mso-font-kerning: 18.0pt; mso-bidi-font-family: 宋体">Organic Matter Types of Core SBt1 ns = "urn:schemas-microsoft-com:office:smarttags" />t1:chmetcnv w:st="on" TCSC="0" NumberType="1" Negative="True" HasSpace="True" SourceValue="1" UnitName="in">-01 int1:chmetcnv> the t1:place w:st="on">t1:PlaceName w:st="on">Sanshuit1:PlaceName> t1:PlaceType w:st="on">Basint1:PlaceType>t1:place> and Their Paleoclimate Implicationst;urn:schemas-microsoft-com:office:office" />
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tyle="MARGIN: 0cm 0cm 0pt" class=MsoNormal>tyle="FONT-FAMILY: Verdana; COLOR: black; FONT-SIZE: 10pt" lang=EN-US>Relationships between Landslide Forming Mechanisms and tyle="FONT-FAMILY: Verdana; COLOR: black; FONT-SIZE: 10pt; mso-bidi-font-family: Verdana" lang=EN-US>Climate Changes since Early Mid-Pleistocene in the Upper Reaches of  t1 ns = "urn:schemas-microsoft-com:office:smarttags" />t1:place w:st="on">Yellow Rivert1:place> and the Three Gorges Reservoir Areatyle="FONT-SIZE: 14pt" lang=EN-US>t;urn:schemas-microsoft-com:office:office" />
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tyle="MARGIN: 0cm 0cm 0pt" class=MsoNormal>tyle="FONT-FAMILY: Verdana; COLOR: black; FONT-SIZE: 10pt" lang=EN-US>Relationships between Landslide Forming Mechanisms and tyle="FONT-FAMILY: Verdana; COLOR: black; FONT-SIZE: 10pt; mso-bidi-font-family: Verdana" lang=EN-US>Climate Changes since Early Mid-Pleistocene in the Upper Reaches of  t1 ns = "urn:schemas-microsoft-com:office:smarttags" />t1:place w:st="on">Yellow Rivert1:place> and the Three Gorges Reservoir Areatyle="FONT-SIZE: 14pt" lang=EN-US>t;urn:schemas-microsoft-com:office:office" />
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