531:. The dorsal flange is short and triangular while the ventral flange is long and more rectangular. The connection point between the two is strongly flexed, meaning they meet at an acute angle, tho the specific degree of flexion varies within the row. At least two groups of lateral osteoderms are identified, Group I in which the ratio between width and length is less than 1:1 and the flanges meet at an angle between 40 and 50°, and Group II in which the ratio between width and length is greater than 1:1 and the angle sits between 25 and 30°. Group I encompasses the first four preserved lateral osteoderms, while the remaining fall into Group II.
401:(ISIR267/1–7) consists of eight associated pieces of bone of the paramedian armour, the armour that is placed along the midline of the animal's back, as well as the associated lateral osteoderms that attach to the sides of the former. In addition to the holotype set of bones, an isolated osteoderm (ISIR286) has also been recovered and referred to the genus based on its shared anatomy. However, there are some differences between the isolated element and the type material. Seeing as these differences may be related to age, sex or simple intraspecific variation, it is currently believed that ISIR286 belonged to a different individual.
1808:
107:
128:
1826:
495:, running parallel to the posterior edge of the osteoderm. The eminence, which is surrounded by a distinct pattern of medium to large-sized pits and ridges that are collectively referred to as ornamentation, is also distinct in its location relative to the edges of the osteoderm. For example, similar to
512:
indicate that they were trunk osteoderms rather than neck osteoderms, with Haldar, Ray and
Bandyopadhyay interpreting as having formed the early to middle trunk armour. Taking this placement into account and applying proportions similar to those of other typothoracines would suggest that the complete
507:
As typical for members of the clade
Typothoracinae, the paramedian osteoderms are extremely wide, more than four times wider than they are long. Since the dorsal eminence is offset towards the midline, thus also shifting the flexion of the paramedian osteoderm, the medial portion of the paramedian
1114:
in the south featuring early diverging forms, high latitudes in the north featuring late diverging forms and the taxa clustering in low latitudes of North
America, Morocco and India which feature a mix of early and late diverging taxa. These clusterings of aetosaur diversity overlap with those of
516:
Overall the lateral osteoderms, which are located to the side of the main paramedian row, are described as reduced and horn-like, their convex anterior margin making them appear to curve backwards. They can generally be divided into a dorsal (upper) and ventral (lower) flange, which are highly
503:
among others, the eminence is not in contact with the back edge of the osteoderm and it is further noted for being offset much further towards the midline than it is in other aetosaurs. Another prominent ridge is located in the posteromedial corner of the osteoderm.
1068:, a paratypothoracine, again pushes the potential age of the formation back in time, ranging from the early to middle Norian to Rhaetian, with the presence of a desmatosuchine aetosaur suggesting a middle Norian age at the least based on the stratigraphy of the
1110:, much like the spread of metoposaurids and phytosaurs. Typothoracines most likely appeared a little later, during the early Norian, while diversifying during the middle Norian to Rhaetian. Geographically, aetosaurs can be found in three major clusters. High
1126:
and the undescribed phytosaur having
Laurasian affinities, while the dinosaurs of the region are more closely allied with Gondwanan groups. This may have been highly influenced by the position of India at the time, with the slow breakup of the
439:
The anterior bar of the osteoderms, the front-most section, is thick and weakly raised, taking up around 36% of the length of the element. A raised anterior bar is a trait that is almost universal among aetosaurs, yet absent in
484:. Observing the osteoderms from the front or back meanwhile shows that they are arched and made up of two main regions that connect at an oblique angle where the dorsal eminence, a raised region that forms the center of
475:
When viewed from above each paramedian osteoderm is rectangular in shape with a straight edge where the lateral osteoderms connect. A similar straight or sigmoid lateral edge is only present in two other typothoracines,
1236:
Haldar, A.; Ray, S.; Bandyopadhyay, S. (2023). "A new typothoracine aetosaur (Archosauria, Pseudosuchia) from the Upper
Triassic of India with insights on biostratigraphy, diversification, and paleobiogeography".
567:. Traits responsible for these results include the extreme width to length ratio, the narrow weakly raised anterior bar, medial offset of the dorsal eminence and the asymmetrical lateral osteoderms.
508:
osteoderm is much shorter than the lateral section, making up only about 40% of the total width. In addition to being of phylogenetic value, the great width of the osteoderms recovered from
450:, a derived trait not seen in any other members of the group. More broadly the margin of the entire medial section of the anterior bar is straight, but this is also shared by
1134:
opening land bridges and removing environmental barriers to allow for the migration of animal groups into the region which was not possible in other parts of the world.
456:. In contrast to the anterior bar, the posterior (back) end of the osteoderm is far more distinctive in its form, as it slopes and forms a bevel which is seen in
491:
The dorsal eminence forms the highest point of the osteoderms and is connected to a rounded ridge that spans the entire width of each osteoderm similar to
1855:
1106:
one of the few known aetosaurs from eastern and central
Gondwana. One hypothesis goes that aetosaur diversification was highly dependent on the
1860:
1850:
472:. The underside of the osteoderm is generally smooth but preserves a pronounced ventral strut or keel that runs along the width of the bone.
1278:
1177:. Another undescribed pseudosuchian from the formation is a second type of aetosaur that more closely resembles the only distantly related
1050:. Previously, Bandyopadhyay and Ray proposed that the Lower Dharmaram Formation was mid to late Norian in age based on the presence of a
366:
and lends credence to the idea that late
Triassic India represented a connective hub between Laurasian and Gondwanan fauna. The genus is
1807:
127:
404:
The genus was named in honor of N. Venkata Raja Reddy, an enthusiast who helped with the discovery of fossils in the
1122:
India in particular is known to display a mix of
Laurasian and Gondwanan fauna during the Late Triassic, with both
853:
805:
650:
1046:
The age of the Lower
Dharmaram Formation has been a matter of debate which is only added to by the description of
436:
are deemed unique to this taxon, its the specific combination of features that sets it apart from its relatives.
386:
317:
1271:
886:
428:
is known, it can be readily distinguished from other aetosaurs by the combination of features present on its
1061:
1057:
754:
674:
405:
1107:
1082:
also has major implications for the geography of aetosaurs. Generally, aetosaurs are best represented from
910:
602:
1366:
771:
723:
568:
333:
278:
255:
1264:
698:
1829:
122:
106:
1690:
1564:
626:
564:
552:
394:
345:
234:
1714:
1637:
1452:
1242:
1155:
1069:
221:
1665:
1595:
1335:
1182:
1116:
523:
446:. The anterior bar also features a straight anteriomedial margin which is considered an
1779:
1734:
1647:
1588:
1502:
1151:
1128:
1115:
metoposaurids and phytosaurs with the exception of the more southern latitudes, though
836:
560:
452:
341:
328:
that formed the paramedian and lateral armour. Based on the osteoderms the carapace of
1844:
1757:
1750:
1706:
1698:
1682:
1628:
1546:
1531:
1523:
1482:
1440:
1189:
1099:
1091:
442:
385:
is known from a series of osteoderms that have been recovered from the Late
Triassic
64:
30:
1654:
1602:
1539:
1516:
1462:
1351:
1326:
1193:
1186:
1164:
1073:
544:
485:
458:
447:
349:
195:
1246:
416:
and translates to "crocodile". The species name "armatum" simply means armoured.
1765:
1581:
1173:
1160:
1052:
464:
354:
332:
was disc-shaped and very wide, with curved, horn-like elements along its sides.
39:
1150:
was the home to a wide variety of animals. This includes dinosaurs such as the
1772:
1573:
1553:
1475:
1317:
548:
429:
393:, more specifically from a locality near the village of Rampur within India's
325:
84:
49:
362:
is among the few aetosaurs recovered from the region that would later become
1490:
1168:
1143:
1060:
in Germany, whereas other researchers suggests that the fauna postdates the
367:
182:
139:
89:
1426:
1404:
1378:
1311:
1287:
1111:
1095:
1083:
398:
363:
314:
310:
208:
159:
79:
74:
59:
54:
44:
1722:
169:
94:
69:
1305:
1131:
1087:
1064:, indicating its age to be late Norian to Rhaetian. The discovery of
580:
409:
149:
413:
390:
324:. It was described in 2023 on the basis of a series of associated
321:
1298:
1260:
1256:
1185:
importance like phytosaurs and aetosaurs, animals like
1181:. While archosaurs were plentiful, including groups of
517:
asymmetric with a much larger ventral flange like in
513:
armour would have been disc-like in its appearance.
1733:
1664:
1636:
1627:
1563:
1501:
1461:
1450:
1424:
1377:
1350:
412:"suchus", which is derived from the Egyptian deity
408:. The second part of the name utilizes the Greek
1098:record is comparably poor with the exception of
1272:
1056:-like phytosaur and its correlation with the
370:, meaning it only includes a single species,
8:
1142:The Lower Dharmaram Formation represents an
1674:
1633:
1508:
1467:
1458:
1432:
1421:
1356:
1347:
1295:
1279:
1265:
1257:
105:
20:
1146:dominated environment and in addition to
1231:
1229:
468:and inconsistently among individuals of
1227:
1225:
1223:
1221:
1219:
1217:
1215:
1213:
1211:
1209:
1205:
1196:are as of yet unknown from the region.
571:indicates that the closest relative of
539:Multiple features of the osteoderms of
1102:as the westernmost region. This makes
543:indicate that it was a member of the
432:. Though only few traits observed in
297:Haldar, Ray & Bandyopadhyay, 2023
7:
902:
878:
828:
821:
797:
746:
739:
715:
690:
666:
642:
619:
594:
586:
1239:Journal of Vertebrate Paleontology
14:
547:, one of the major clades within
254:Haldar, Ray & Bandyopadhyay,
1856:Prehistoric pseudosuchian genera
1825:
1824:
1806:
344:and more specifically the clade
126:
1171:which may have been similar to
348:, where it is recovered as the
1:
1861:Fossil taxa described in 2023
1247:10.1080/02724634.2023.2253292
1851:Late Triassic pseudosuchians
424:Although little material of
1163:as well as a wide range of
1119:could be a factor at play.
1877:
1042:Stratigraphy and geography
854:Paratypothorax andressorum
806:Rioarribasuchus chamaensis
651:Coahomasuchus chathamensis
579:from the Late Triassic of
470:Paratypothorax andressorum
340:belonged to the subfamily
1820:
1803:
1677:
1511:
1470:
1435:
1420:
1401:
1359:
1346:
1294:
1167:including an undescribed
924:
907:
900:
883:
876:
850:
833:
826:
819:
802:
795:
768:
751:
744:
737:
720:
713:
695:
688:
671:
664:
647:
640:
624:
617:
599:
592:
387:Lower Dharmaram Formation
284:
277:
123:Scientific classification
121:
113:
104:
23:
887:Tecovasuchus chatterjeei
563:and is deeply nested in
1062:Ischigualasto Formation
755:Redondasuchus rineharti
675:Coahomasuchus kahleorum
497:Desmatosuchus spurensis
406:Pranhita-Godavari Basin
309:is an extinct genus of
911:Kocurypelta silvestris
603:Aetosauroides scagliai
577:Kocurypelta silvestris
1108:Carnial Pluvial Event
928:Venkatasuchus armatum
772:Typothorax coccinarum
724:Apachesuchus heckerti
569:Phylogenetic analysis
555:. More specifically,
372:Venkatasuchus armatum
334:Phylogenetic analysis
291:Venkatasuchus armatum
116:Venkatasuchus armatus
1058:Löwenstein Formation
114:Life restoration of
1159:and an undescribed
699:Aetosaurus ferratus
318:Dharmaram Formation
837:Paratypothorax sp.
793:Paratypothoracini
378:History and naming
1838:
1837:
1816:
1815:
1801:
1800:
1797:
1796:
1793:
1792:
1789:
1788:
1738:(Desmatosuchinae
1691:Aetobarbakinoides
1623:
1622:
1619:
1618:
1565:Paratypothoracini
1416:
1415:
1412:
1411:
1397:
1396:
1038:
1037:
1029:
1028:
1020:
1019:
1011:
1010:
1002:
1001:
993:
992:
984:
983:
975:
974:
966:
965:
957:
956:
948:
947:
939:
938:
865:
864:
783:
782:
627:Stagonolepidoidea
615:Stagonolepididae
565:Paratypothoracini
559:falls within the
553:Stagonolepidoidea
395:Adilabad district
346:Paratypothoracini
302:
301:
258:
235:Paratypothoracini
1868:
1828:
1827:
1811:
1810:
1715:Neoaetosauroides
1675:
1638:Stagonolepidinae
1634:
1509:
1468:
1459:
1453:Stagonolepididae
1433:
1422:
1357:
1348:
1341:
1340:
1296:
1281:
1274:
1267:
1258:
1251:
1250:
1233:
1183:biostratigraphic
1156:Jaklapallisaurus
1094:, whereas their
1070:Chinle Formation
903:
879:
829:
822:
798:
747:
740:
716:
691:
667:
643:
620:
595:
587:
293:
289:
253:
246:
233:
222:Stagonolepididae
220:
207:
131:
130:
109:
99:
36:
29:Temporal range:
21:
16:Genus of reptile
1876:
1875:
1871:
1870:
1869:
1867:
1866:
1865:
1841:
1840:
1839:
1834:
1812:
1805:
1785:
1739:
1737:
1729:
1668:
1666:Desmatosuchinae
1660:
1615:
1596:Rioarribasuchus
1559:
1497:
1455:
1446:
1429:
1408:
1393:
1373:
1342:
1336:Aetosauriformes
1301:
1300:
1290:
1285:
1255:
1254:
1235:
1234:
1207:
1202:
1140:
1117:collection bias
1044:
1039:
1030:
1021:
1012:
1003:
994:
985:
976:
967:
958:
949:
940:
866:
784:
711:Typothoracinae
537:
524:Rioarribasuchus
422:
380:
336:indicates that
298:
295:
287:
286:
273:
270:V. armatum
252:
244:
231:
218:
205:
125:
100:
98:
97:
92:
87:
82:
77:
72:
67:
62:
57:
52:
47:
42:
35:Norian–Rhaetian
34:
33:
27:
17:
12:
11:
5:
1874:
1872:
1864:
1863:
1858:
1853:
1843:
1842:
1836:
1835:
1833:
1832:
1821:
1818:
1817:
1814:
1813:
1804:
1802:
1799:
1798:
1795:
1794:
1791:
1790:
1787:
1786:
1784:
1783:
1780:Sierritasuchus
1776:
1769:
1762:
1754:
1746:
1744:
1735:Desmatosuchini
1731:
1730:
1728:
1727:
1719:
1711:
1703:
1695:
1687:
1678:
1672:
1662:
1661:
1659:
1658:
1651:
1648:Polesinesuchus
1643:
1641:
1631:
1625:
1624:
1621:
1620:
1617:
1616:
1614:
1613:
1606:
1599:
1592:
1589:Paratypothorax
1585:
1578:
1569:
1567:
1561:
1560:
1558:
1557:
1550:
1543:
1536:
1528:
1520:
1512:
1506:
1503:Typothoracinae
1499:
1498:
1496:
1495:
1487:
1479:
1471:
1465:
1456:
1451:
1448:
1447:
1445:
1444:
1436:
1430:
1425:
1418:
1417:
1414:
1413:
1410:
1409:
1402:
1399:
1398:
1395:
1394:
1392:
1391:
1390:
1389:
1383:
1381:
1375:
1374:
1372:
1371:
1370:
1369:
1360:
1354:
1344:
1343:
1339:
1338:
1329:
1320:
1314:
1308:
1299:
1292:
1291:
1286:
1284:
1283:
1276:
1269:
1261:
1253:
1252:
1204:
1203:
1201:
1198:
1165:pseudosuchians
1152:sauropodomorph
1139:
1136:
1129:supercontinent
1086:formations in
1043:
1040:
1036:
1035:
1032:
1031:
1027:
1026:
1023:
1022:
1018:
1017:
1014:
1013:
1009:
1008:
1005:
1004:
1000:
999:
996:
995:
991:
990:
987:
986:
982:
981:
978:
977:
973:
972:
969:
968:
964:
963:
960:
959:
955:
954:
951:
950:
946:
945:
942:
941:
937:
936:
933:
932:
923:
920:
919:
916:
915:
906:
901:
899:
896:
895:
892:
891:
882:
877:
875:
872:
871:
868:
867:
863:
862:
859:
858:
849:
846:
845:
842:
841:
832:
827:
825:
820:
818:
815:
814:
811:
810:
801:
796:
794:
790:
789:
786:
785:
781:
780:
777:
776:
767:
764:
763:
760:
759:
750:
745:
743:
738:
736:
733:
732:
729:
728:
719:
714:
712:
708:
707:
704:
703:
694:
689:
687:
684:
683:
680:
679:
670:
665:
663:
660:
659:
656:
655:
646:
641:
639:
635:
634:
631:
630:
623:
618:
616:
612:
611:
608:
607:
598:
593:
591:
585:
561:Typothoracinae
551:and sister to
536:
533:
519:Paratypothorax
488:, is located.
453:Paratypothorax
421:
418:
379:
376:
342:Typothoracinae
313:from the Late
300:
299:
296:
282:
281:
275:
274:
266:
264:
260:
259:
242:
238:
237:
229:
225:
224:
216:
212:
211:
203:
199:
198:
193:
186:
185:
180:
173:
172:
167:
163:
162:
157:
153:
152:
147:
143:
142:
137:
133:
132:
119:
118:
111:
110:
102:
101:
93:
88:
83:
78:
73:
68:
63:
58:
53:
48:
43:
38:
37:
28:
15:
13:
10:
9:
6:
4:
3:
2:
1873:
1862:
1859:
1857:
1854:
1852:
1849:
1848:
1846:
1831:
1823:
1822:
1819:
1809:
1782:
1781:
1777:
1775:
1774:
1770:
1768:
1767:
1763:
1760:
1759:
1758:Gorgetosuchus
1755:
1753:
1752:
1751:Desmatosuchus
1748:
1747:
1745:
1742:
1741:sensu stricto
1736:
1732:
1725:
1724:
1720:
1717:
1716:
1712:
1709:
1708:
1707:Chilenosuchus
1704:
1701:
1700:
1699:Calyptosuchus
1696:
1693:
1692:
1688:
1685:
1684:
1683:Adamanasuchus
1680:
1679:
1676:
1673:
1671:
1667:
1663:
1657:
1656:
1652:
1650:
1649:
1645:
1644:
1642:
1639:
1635:
1632:
1630:
1629:Desmatosuchia
1626:
1612:
1611:
1610:Venkatasuchus
1607:
1605:
1604:
1600:
1598:
1597:
1593:
1591:
1590:
1586:
1584:
1583:
1579:
1576:
1575:
1571:
1570:
1568:
1566:
1562:
1556:
1555:
1551:
1549:
1548:
1547:Redondasuchus
1544:
1542:
1541:
1537:
1534:
1533:
1532:Gorgetosuchus
1529:
1526:
1525:
1524:Chilenosuchus
1521:
1519:
1518:
1514:
1513:
1510:
1507:
1504:
1500:
1493:
1492:
1488:
1485:
1484:
1483:Coahomasuchus
1480:
1478:
1477:
1473:
1472:
1469:
1466:
1464:
1460:
1457:
1454:
1449:
1443:
1442:
1441:Aetosauroides
1438:
1437:
1434:
1431:
1428:
1423:
1419:
1407:
1406:
1400:
1387:
1386:
1385:
1384:
1382:
1380:
1376:
1368:
1364:
1363:
1362:
1361:
1358:
1355:
1353:
1349:
1345:
1337:
1333:
1330:
1328:
1324:
1321:
1319:
1315:
1313:
1309:
1307:
1303:
1302:
1297:
1293:
1289:
1282:
1277:
1275:
1270:
1268:
1263:
1262:
1259:
1248:
1244:
1240:
1232:
1230:
1228:
1226:
1224:
1222:
1220:
1218:
1216:
1214:
1212:
1210:
1206:
1199:
1197:
1195:
1191:
1190:temnospondyls
1188:
1184:
1180:
1179:Desmatosuchus
1176:
1175:
1170:
1166:
1162:
1158:
1157:
1153:
1149:
1148:Venkatasuchus
1145:
1137:
1135:
1133:
1130:
1125:
1124:Venkatasuchus
1120:
1118:
1113:
1109:
1105:
1104:Venkatasuchus
1101:
1100:South America
1097:
1093:
1092:North America
1089:
1085:
1081:
1080:Venkatasuchus
1077:
1075:
1071:
1067:
1066:Venkatasuchus
1063:
1059:
1055:
1054:
1049:
1048:Venkatasuchus
1041:
1034:
1033:
1025:
1024:
1016:
1015:
1007:
1006:
998:
997:
989:
988:
980:
979:
971:
970:
962:
961:
953:
952:
944:
943:
935:
934:
931:
930:
929:
922:
921:
918:
917:
914:
913:
912:
905:
904:
898:
897:
894:
893:
890:
889:
888:
881:
880:
874:
873:
870:
869:
861:
860:
857:
856:
855:
848:
847:
844:
843:
840:
839:
838:
831:
830:
824:
823:
817:
816:
813:
812:
809:
808:
807:
800:
799:
792:
791:
788:
787:
779:
778:
775:
774:
773:
766:
765:
762:
761:
758:
757:
756:
749:
748:
742:
741:
735:
734:
731:
730:
727:
726:
725:
718:
717:
710:
709:
706:
705:
702:
701:
700:
693:
692:
686:
685:
682:
681:
678:
677:
676:
669:
668:
662:
661:
658:
657:
654:
653:
652:
645:
644:
638:Aetosaurinae
637:
636:
633:
632:
629:
628:
622:
621:
614:
613:
610:
609:
606:
605:
604:
597:
596:
589:
588:
584:
582:
578:
574:
573:Venkatasuchus
570:
566:
562:
558:
557:Venkatasuchus
554:
550:
546:
542:
541:Venkatasuchus
534:
532:
530:
526:
525:
520:
514:
511:
510:Venkatasuchus
505:
502:
498:
494:
489:
487:
483:
479:
473:
471:
467:
466:
461:
460:
455:
454:
449:
445:
444:
443:Desmatosuchus
437:
435:
434:Venkatasuchus
431:
427:
426:Venkatasuchus
419:
417:
415:
411:
407:
402:
400:
396:
392:
388:
384:
383:Venkatasuchus
377:
375:
373:
369:
365:
361:
360:Venkatasuchus
357:
356:
351:
347:
343:
339:
338:Venkatasuchus
335:
331:
330:Venkatasuchus
327:
323:
319:
316:
312:
308:
307:
306:Venkatasuchus
294:
292:
283:
280:
279:Binomial name
276:
272:
271:
265:
262:
261:
257:
251:
250:
249:Venkatasuchus
243:
240:
239:
236:
230:
227:
226:
223:
217:
214:
213:
210:
204:
201:
200:
197:
194:
191:
188:
187:
184:
181:
178:
175:
174:
171:
168:
165:
164:
161:
158:
155:
154:
151:
148:
145:
144:
141:
138:
135:
134:
129:
124:
120:
117:
112:
108:
103:
96:
91:
86:
81:
76:
71:
66:
61:
56:
51:
46:
41:
32:
31:Late Triassic
26:
25:Venkatasuchus
22:
19:
1778:
1771:
1764:
1756:
1749:
1740:
1721:
1713:
1705:
1697:
1689:
1681:
1669:
1655:Stagonolepis
1653:
1646:
1609:
1608:
1603:Tecovasuchus
1601:
1594:
1587:
1580:
1572:
1552:
1545:
1540:Kryphioparma
1538:
1530:
1522:
1517:Apachesuchus
1515:
1489:
1481:
1474:
1463:Aetosaurinae
1439:
1403:
1367:Pseudosuchia
1352:Pseudosuchia
1331:
1327:Pseudosuchia
1322:
1241:. e2253292.
1238:
1194:rhynchosaurs
1187:metoposaurid
1178:
1172:
1154:
1147:
1141:
1138:Paleoecology
1123:
1121:
1103:
1079:
1078:
1074:Dockum Group
1065:
1051:
1047:
1045:
927:
926:
925:
909:
908:
885:
884:
852:
851:
835:
834:
804:
803:
770:
769:
753:
752:
722:
721:
697:
696:
673:
672:
649:
648:
625:
601:
600:
576:
572:
556:
545:Aetosaurinae
540:
538:
529:Tecovasuchus
528:
522:
518:
515:
509:
506:
500:
496:
492:
490:
486:ossification
481:
478:Tecovasuchus
477:
474:
469:
463:
459:Tecovasuchus
457:
451:
448:autapomorphy
441:
438:
433:
425:
423:
403:
382:
381:
371:
359:
353:
350:sister taxon
337:
329:
305:
304:
303:
290:
285:
269:
268:
248:
247:
196:Pseudosuchia
189:
176:
115:
24:
18:
1766:Longosuchus
1582:Kocurypelta
1174:Nicrosaurus
1161:neotheropod
1053:Nicrosaurus
590:Aetosauria
493:Kocurypelta
482:Kocurypelta
465:Kocurypelta
420:Description
355:Kocurypelta
183:Archosauria
1845:Categories
1773:Lucasuchus
1670:sensu lato
1574:Garzapelta
1554:Typothorax
1476:Aetosaurus
1427:Aetosauria
1405:Aetosauria
1388:see below↓
1379:Aetosauria
1318:Sauropsida
1288:Aetosauria
1200:References
549:Aetosauria
501:Lucasuchus
430:osteoderms
326:osteoderms
209:Aetosauria
1491:Stenomyti
1304:Kingdom:
1169:phytosaur
1144:archosaur
1112:latitudes
1096:Gondwanan
1084:Laurasian
535:Phylogeny
368:monotypic
263:Species:
146:Kingdom:
140:Eukaryota
1830:Category
1312:Chordata
1310:Phylum:
1306:Animalia
399:holotype
364:Gondwana
315:Triassic
311:aetosaur
215:Family:
170:Reptilia
160:Chordata
156:Phylum:
150:Animalia
136:Domain:
1723:Scutarx
1316:Class:
288:†
267:†
241:Genus:
228:Tribe:
202:Order:
166:Class:
1132:Pangea
1088:Europe
581:Poland
410:suffix
397:. The
1332:Clade
1323:Clade
414:Sobek
391:India
322:India
190:Clade
177:Clade
1365:see
1192:and
1090:and
1072:and
575:was
527:and
499:and
480:and
256:2023
40:PreꞒ
1243:doi
389:of
352:to
320:of
1847::
1334::
1325::
1208:^
1076:.
583:.
521:,
462:,
374:.
358:.
192::
179::
90:Pg
1761:?
1743:)
1726:?
1718:?
1710:?
1702:?
1694:?
1686:?
1640:?
1577:?
1535:?
1527:?
1505:?
1494:?
1486:?
1280:e
1273:t
1266:v
1249:.
1245::
245:†
232:†
219:†
206:†
95:N
85:K
80:J
75:T
70:P
65:C
60:D
55:S
50:O
45:Ꞓ
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