Analysis of information sources in references of the Wikipedia article "Red Deer Cave people" in English language version.
All of the [Maludong] human remains were recovered from within a series of deposits dating from 14,310±340 cal. yr BP (OZM149; 292 cm depth) to 13,590±160 cal. yr BP (OZM145; 166 cm depth), a period of about 720 years. Moreover, the high fine-grained ferrimagnetic content of the deposits (Text S1), with their high magnetic susceptibility, suggests these were formed under warm, wet conditions, consistent with the Bølling-Allerød interstadial (~14.7-12.6 ka). Human remains recovered in situ during the 2008 excavation and a reasonably complete calotte (specimen MLDG 1704) derived from a subsection of these deposits dated between 13,990±165 cal. yr BP (OZM148; 235 cm) and 13,890±140 cal. yr BP (OZM146; 200 cm)
{{cite journal}}: CS1 maint: DOI inactive as of November 2024 (link)All of the [Maludong] human remains were recovered from within a series of deposits dating from 14,310±340 cal. yr BP (OZM149; 292 cm depth) to 13,590±160 cal. yr BP (OZM145; 166 cm depth), a period of about 720 years. Moreover, the high fine-grained ferrimagnetic content of the deposits (Text S1), with their high magnetic susceptibility, suggests these were formed under warm, wet conditions, consistent with the Bølling-Allerød interstadial (~14.7-12.6 ka). Human remains recovered in situ during the 2008 excavation and a reasonably complete calotte (specimen MLDG 1704) derived from a subsection of these deposits dated between 13,990±165 cal. yr BP (OZM148; 235 cm) and 13,890±140 cal. yr BP (OZM146; 200 cm)
All of the [Maludong] human remains were recovered from within a series of deposits dating from 14,310±340 cal. yr BP (OZM149; 292 cm depth) to 13,590±160 cal. yr BP (OZM145; 166 cm depth), a period of about 720 years. Moreover, the high fine-grained ferrimagnetic content of the deposits (Text S1), with their high magnetic susceptibility, suggests these were formed under warm, wet conditions, consistent with the Bølling-Allerød interstadial (~14.7-12.6 ka). Human remains recovered in situ during the 2008 excavation and a reasonably complete calotte (specimen MLDG 1704) derived from a subsection of these deposits dated between 13,990±165 cal. yr BP (OZM148; 235 cm) and 13,890±140 cal. yr BP (OZM146; 200 cm)
{{cite journal}}: CS1 maint: DOI inactive as of November 2024 (link)All of the [Maludong] human remains were recovered from within a series of deposits dating from 14,310±340 cal. yr BP (OZM149; 292 cm depth) to 13,590±160 cal. yr BP (OZM145; 166 cm depth), a period of about 720 years. Moreover, the high fine-grained ferrimagnetic content of the deposits (Text S1), with their high magnetic susceptibility, suggests these were formed under warm, wet conditions, consistent with the Bølling-Allerød interstadial (~14.7-12.6 ka). Human remains recovered in situ during the 2008 excavation and a reasonably complete calotte (specimen MLDG 1704) derived from a subsection of these deposits dated between 13,990±165 cal. yr BP (OZM148; 235 cm) and 13,890±140 cal. yr BP (OZM146; 200 cm)