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Table 2 Maximum (U) and minimum (L) time constrains (MYA) used for dating at nodes in Fig. 2

From: Mitogenomic evaluation of the historical biogeography of cichlids toward reliable dating of teleostean divergences

Node

Constraint

Reference information

A

L416

Psarolepis fossil (the earliest Sarcopterygii) from Ludlow (Silurian) [2]Lophosteus and Andreolepis fossils (the earliest Actinopterygii) from Ludlow (Silurian) [64]

A

U528

Probable divergence time between chondrichthyans and osteichthyans (528 MYA), based on both fossils and molecules [58]

B

L392

Stem-actinopterans known from the Givetian/Eifelian boundary [57]

B

U450

Probable divergence time between sarcopterygians and actinopterygians (450 MYA), based on both fossils and molecules [6, 58]

C

L345

Tournasian Cosmoptychius as the earliest stem-group neopterygian [57]

C

U392

Estimated divergence time between polypterids and actinopterans [57]

D

L130

Protosephuru (paddlefish) from Hauterivian (Cretaceous) [57]

E

L284

Brachydegma from early Permian [57]

F

L136

Stem-hiodontid Yambiania from the Lower Cretaceous [57]

G

L112

Osteoglossoid fossil from the Aptian (Cretaceous) [4]

H

L151

Stem-elopomorph Elopsomolos from the Kimmeridgian (Jurassic) [57]

I

L90

Albuloid fossil from the Cenomanian (Cretaceous) [4]

J

L50

Anguillid and congrid fossils from the Ypresian (Tertiary) [4]

K

L146

Stem-ostariophysan Tischlingerichthys from Tithonian (Jurassic) [57]

L

L57

Clupeid fossil from the Thanetian (Tertiary) [4]

M

L50

Cyprinid fossil from the Ypresian (Tertiary) [4]

N

L74

Esociform fossil from the Campanian (Cretaceous) [4]

O

L94

Polymixiid fossil from the Cenomanian (Cretaceous) [4]

P

L50

Pleuronectiform fossil from the Ypresian (Tertiary) [4]

Q

L98

Tetraodontiform fossil from the Cenomanian (Cretaceous) [2]

R

L32

Estimated divergence time between Takifugu and Tetraodon [2]