Table 1 Comparisons of 14C dates based on modern (SM003) and fossil (M22-M24) sand dollars and fossil mollusks reported in Peng et al.12.

From: Changing surface ocean circulation caused the local demise of echinoid Scaphechinus mirabilis in Taiwan during the Pleistocene–Holocene transition

Lab code

Sample ID

Species

pMC (%)

∆14C (%)

14C age (yr BP)

Calendric age (yr BP)

MIS

Sources

NTUAMS-6682–1

SM003

S. mirabilis

107.84 ± 0.84

78.4 ± 0.6

Modern

Modern

 

This study

NTUAMS-7067–1

M22

S. mirabilis

3.21 ± 0.08

− 967.9 ± 24.3

27,623 ± 202

31,420 ± 280

3

This study

NTUAMS-7068–1

M23

S. mirabilis

0.36 ± 0.02

− 996.4 ± 51.3

45,211 ± 413

48,620 ± 965

3

This study

NTUAMS-7069–1

M24

S. mirabilis

 < 0.11

 < − 998.9

 > 55,000

  

This study

 

α

Pecten byoritsuensis

   

44,900 ± 1400

3

Ref.12

 

β

Pecten byoritsuensis

   

36,700 ± 600

3

Ref.12

 

γ

Pecten byoritsuensis

   

30,900 ± 300

3

Ref.12

  1. MIS Marine Isotope Stages. Modern is younger than AD 1950.