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Guabirotuba Formation

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965: 559: 359: 366: 290: 1368: 683: 1506: 486: 338: 694: 672: 882: 822: 462: 698: 547: 638:
fauna described by Sedor et al. in 2017, the age of the formation has been defined as late Middle Eocene, or "Barrancan", which is a sub-age of the
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has provided insight in the paleocurrents of the fluvial environment, with predominant flow directions towards the northwest and east-northeast.
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Wagner Rogério, Daniel; Vieira Dias, Eliseu; Sedor, Fernando Antonio; Weinschütz, Luiz Carlos; Del Mouro, Lucas; Leitão Waichel, Breno (2012),
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Sedor, Fernando A.; Oliveira, Édison V.; Silva, David D.; Fernandes, Luiz A.; Cunha, Renata F.; Ribeiro, Ana M.; Dias, Eliseu V. (2017),
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Monteiro Machado, Denise Alessandra; Fernandes, Luiz Alberto; Góes, Ana Maria; de Mesquita, Maria José; Macedo de Lima, Fabio (2012),
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The sub-ages "Barrancan" and "Vacan" are based on respectively the Gran Barranca Member and the Cañadón Vaca section of the
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Paleogene phorusrhacid bird (Aves, Phorusrhacidae) from the Guabirotuba Formation, Curitiba Basin, Paraná, South of Brazil
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in Patagonia, Argentina and are not formally established; some authors consider the "Barrancan" as the upper age of the
1422:"Paleogene Land Mammal Faunas of South America; a Response to Global Climatic Changes and Indigenous Floral Diversity" 242: 203: 964: 1496: 1420:
Woodburne, M.O.; Goin, F.J.; Bond, M.; Carlini, A.A.; Gelfo, J.N.; LĂłpez, G.M.; Iglesias, A.; Zimicz, A.N. (2013),
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The Guabirotuba Formation is one of few formations in Brazil providing Paleogene mammal faunas, between the older
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The age of the formation has been a matter of debate, with early descriptions assigning the formation to the
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Características Geológico-Geotécnicas na Formação Guabirotuba Erosão - Movimentos Gravitacionais de Massa
515:. The formation is the lowermost sedimentary unit in the 3,000 square kilometres (1,200 sq mi) 491: 1300: 1501: 1471: 1476: 588: 558: 438: 1334:
Sedor, Fernando A.; Vieira Dias, Eliseu; Da Cunha, Renata Floriano; Alvarenga, Herculano (2014),
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The 60 to 80 metres (200 to 260 ft) thick Guabirotuba Formation comprises a basal
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The 60 to 80 metres (200 to 260 ft) thick formation has provided several fossil
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The sediments of the formation contain between 0.24 and 2.61% heavy minerals.
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The depositional environment of the Guabirotuba Formation was a
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A newly described species of 13: 963: 523:of southeastern Brazil, overlying 14: 1528: 1351:Da Silva Felipe, RogĂ©rio (2011), 1259:Revista Brasileira de GeociĂŞncias 1211:Wagner RogĂ©rio et al., 2012, p.44 704: 466:was also found in the formation. 1272:10.25249/0375-7536.2012423563572 1141:Bellosi & Krause, 2014, p.31 364: 357: 288: 45: 1217: 1014: 634:, but after the discovery of a 1467:Eocene Series of South America 1427:Journal of Mammalian Evolution 1309:Journal of Mammalian Evolution 643:South American land mammal age 553: 469: 373:Guabirotuba Formation (Brazil) 157:60–80 m (200–260 ft) 1: 1462:Geologic formations of Brazil 1120:Monteiro Machado, 2012, p.570 1111:Monteiro Machado, 2012, p.567 1102:Monteiro Machado, 2012, p.566 1081:Monteiro Machado, 2012, p.565 1046:Monteiro Machado, 2012, p.564 1034: 1129:Woodburne et al., 2014, p.19 971: 943: 922: 906: 888: 872: 856: 845: 829: 811: 800: 789: 776: 763: 750: 649:Paleontological significance 236:Approximate paleocoordinates 7: 1517:Geography of Paraná (state) 1150:Woodburne et al., 2014, p.7 1090:Da Silva Felipe, 2011, p.17 1072:Da Silva Felipe, 2011, p.12 977: 452:fossils, and indeterminate 10: 1533: 1360:, MINEROPAR, pp. 1–48 840:Oldfieldthomasiidae indet. 731: 419:in and around the city of 1440:10.1007/s10914-012-9222-1 1322:10.1007/s10914-016-9364-7 1202:Sedor et al., 2014, p.807 833: 823:Proeocoleophorus carlinii 736: 546:and metasediments of the 519:, a Cenozoic continental 463:Proeocoleophorus carlinii 352: 344: 330: 316: 311: 301: 283: 273: 234: 195: 190: 180: 166: 161: 153: 140: 128: 118: 23: 18: 1060:Sedor et al., 2017, p.39 1007: 684:Entre-CĂłrregos Formation 1497:Conglomerate formations 1407:10.4013/gaea.2012.82.01 883:Palaeothentoidea indet. 658:Maria Farinha Formation 1512:Paleontology in Brazil 968: 621: 596:Heavy mineral analysis 566: 1274:(inactive 2024-07-08) 967: 938:Phorusrhacidae indet. 917:Argyrolagoidea indet. 851:Notopithecidae indet. 795:Astegotheriini indet. 598:on the very abundant 561: 385:Guabirotuba Formation 19:Guabirotuba Formation 1492:Sandstone formations 1003:Notes and references 867:Astrapotheria indet. 677:Rio de Janeiro State 507:, a neighborhood of 448:, and indeterminate 397:SALMA classification 123:Geological formation 1487:Mudstone formations 1398:2012Gaea....8...42R 1022:Sarmiento Formation 806:Euphractinae indet. 744:Machlydotherium sp. 487:JoĂŁo JosĂ© Bigarella 254: /  215: /  25:Stratigraphic range 1371:2016-02-22 at the 969: 695:TremembĂ© Formation 679:, and the younger 669:ItaboraĂ­ Formation 567: 389:late Middle Eocene 1187:Guabirotuba Fauna 990:Macarao Formation 984:Abanico Formation 975: 974: 959:Pleurodira indet. 581:, deposited in a 511:, the capital of 381: 380: 1524: 1502:Fluvial deposits 1472:Paleogene Brazil 1448: 1447: 1446: 1416: 1415: 1414: 1409: 1367: 1366: 1365: 1359: 1347: 1346: 1345: 1330: 1329: 1328: 1305: 1295: 1289: 1281: 1280: 1279: 1248: 1247: 1246: 1230: 1212: 1209: 1203: 1200: 1194: 1184: 1151: 1148: 1142: 1139: 1130: 1127: 1121: 1118: 1112: 1109: 1103: 1100: 1091: 1088: 1082: 1079: 1073: 1070: 1061: 1058: 1047: 1044: 1028: 1018: 996:Soncco Formation 878:Paucituberculata 712: 711: 506: 495: 484: 450:side-neck turtle 415:. The formation 368: 367: 361: 294: 292: 291: 269: 268: 266: 265: 264: 259: 255: 252: 251: 250: 247: 230: 229: 227: 226: 225: 220: 216: 213: 212: 211: 208: 114: 44: 16: 15: 1532: 1531: 1527: 1526: 1525: 1523: 1522: 1521: 1477:Bartonian Stage 1452: 1451: 1444: 1442: 1412: 1410: 1373:Wayback Machine 1363: 1361: 1357: 1343: 1341: 1326: 1324: 1303: 1283: 1282: 1277: 1275: 1244: 1242: 1228: 1220: 1215: 1210: 1206: 1201: 1197: 1185: 1154: 1149: 1145: 1140: 1133: 1128: 1124: 1119: 1115: 1110: 1106: 1101: 1094: 1089: 1085: 1080: 1076: 1071: 1064: 1059: 1050: 1045: 1041: 1037: 1032: 1031: 1019: 1015: 1010: 1005: 980: 707: 651: 624: 556: 500: 489: 478: 472: 431:deposited in a 377: 376: 375: 374: 371: 370: 369: 289: 287: 262: 260: 256: 253: 248: 245: 243: 241: 240: 223: 221: 217: 214: 209: 206: 204: 202: 201: 113: 112: 111: 110: 105: 100: 95: 90: 85: 80: 75: 70: 65: 60: 55: 50: 39: 38: 36: 29:Late Mid Eocene 12: 11: 5: 1530: 1520: 1519: 1514: 1509: 1504: 1499: 1494: 1489: 1484: 1479: 1474: 1469: 1464: 1450: 1449: 1417: 1375: 1348: 1331: 1296: 1249: 1234:Andean Geology 1219: 1216: 1214: 1213: 1204: 1195: 1152: 1143: 1131: 1122: 1113: 1104: 1092: 1083: 1074: 1062: 1048: 1038: 1036: 1033: 1030: 1029: 1012: 1011: 1009: 1006: 1004: 1001: 1000: 999: 993: 987: 979: 976: 973: 972: 970: 961: 956: 951: 945: 944: 942: 940: 935: 933:Phorusrhacidae 930: 924: 923: 921: 919: 914: 908: 907: 905: 903: 900:Nemolestes sp. 896: 890: 889: 887: 885: 880: 874: 873: 871: 869: 864: 858: 857: 855: 853: 847: 846: 844: 842: 837: 831: 830: 828: 826: 819: 813: 812: 810: 808: 802: 801: 799: 797: 791: 790: 788: 786: 778: 777: 775: 773: 770:Parutaetus sp. 765: 764: 762: 760: 757:Meteutatus sp. 752: 751: 749: 747: 740: 735: 729: 728: 725: 722: 719: 716: 706: 705:Fossil content 703: 688:Aiuruoca Basin 673:ItaboraĂ­ Basin 662:ParnaĂ­ba Basin 650: 647: 623: 620: 555: 552: 517:Curitiba Basin 471: 468: 423:and comprises 405:Curitiba Basin 379: 378: 372: 363: 362: 356: 355: 354: 353: 350: 349: 346: 342: 341: 332: 328: 327: 318: 314: 313: 309: 308: 306:Curitiba Basin 303: 299: 298: 285: 281: 280: 275: 271: 270: 238: 232: 231: 199: 193: 192: 188: 187: 182: 178: 177: 168: 164: 163: 159: 158: 155: 151: 150: 142: 138: 137: 130: 126: 125: 120: 116: 115: 108: 107: 106: 101: 96: 91: 86: 81: 76: 71: 66: 61: 56: 51: 46: 21: 20: 9: 6: 4: 3: 2: 1529: 1518: 1515: 1513: 1510: 1508: 1505: 1503: 1500: 1498: 1495: 1493: 1490: 1488: 1485: 1483: 1480: 1478: 1475: 1473: 1470: 1468: 1465: 1463: 1460: 1459: 1457: 1441: 1437: 1433: 1429: 1428: 1423: 1418: 1408: 1403: 1399: 1395: 1391: 1387: 1386: 1381: 1376: 1374: 1370: 1356: 1355: 1349: 1339: 1338: 1332: 1323: 1319: 1315: 1311: 1310: 1302: 1297: 1293: 1287: 1273: 1269: 1265: 1261: 1260: 1255: 1250: 1240: 1236: 1235: 1227: 1222: 1221: 1208: 1199: 1192: 1188: 1183: 1181: 1179: 1177: 1175: 1173: 1171: 1169: 1167: 1165: 1163: 1161: 1159: 1157: 1147: 1138: 1136: 1126: 1117: 1108: 1099: 1097: 1087: 1078: 1069: 1067: 1057: 1055: 1053: 1043: 1039: 1027: 1023: 1017: 1013: 997: 994: 991: 988: 985: 982: 981: 966: 962: 960: 957: 955: 952: 950: 947: 946: 941: 939: 936: 934: 931: 929: 926: 925: 920: 918: 915: 913: 910: 909: 904: 902: 901: 897: 895: 894:Sparassodonta 892: 891: 886: 884: 881: 879: 876: 875: 870: 868: 865: 863: 862:Astrapotheria 860: 859: 854: 852: 849: 848: 843: 841: 838: 836: 832: 827: 825: 824: 820: 818: 815: 814: 809: 807: 804: 803: 798: 796: 793: 792: 787: 785: 784: 780: 779: 774: 772: 771: 767: 766: 761: 759: 758: 754: 753: 748: 746: 745: 741: 739: 734: 730: 726: 723: 720: 717: 714: 713: 710: 702: 700: 699:TaubatĂ© Basin 696: 693: 689: 685: 682: 681:Tinguirirican 678: 674: 670: 667: 663: 659: 656: 646: 644: 641: 637: 633: 629: 619: 617: 613: 609: 605: 601: 597: 592: 590: 587: 584: 580: 576: 572: 565: 560: 551: 549: 548:Açungui Group 545: 544:Atuba Complex 541: 537: 533: 529: 526: 522: 518: 514: 510: 504: 499: 493: 488: 482: 477: 476:Riad Salamuni 467: 465: 464: 459: 455: 451: 447: 442: 440: 437: 434: 430: 426: 422: 418: 414: 410: 406: 402: 398: 394: 390: 386: 360: 351: 347: 343: 340: 336: 333: 329: 326: 322: 319: 315: 310: 307: 304: 300: 297: 286: 282: 279: 276: 272: 267: 258:27.5°S 39.8°W 239: 237: 233: 228: 219:25.5°S 49.3°W 200: 198: 194: 189: 186: 183: 179: 176: 172: 169: 165: 160: 156: 152: 149: 146: 143: 139: 136: 135: 131: 127: 124: 121: 117: 104: 99: 94: 89: 84: 79: 74: 69: 64: 59: 54: 49: 43: 34: 30: 26: 22: 17: 1443:, retrieved 1431: 1425: 1411:, retrieved 1392:(2): 42–46, 1389: 1383: 1362:, retrieved 1353: 1342:, retrieved 1336: 1325:, retrieved 1313: 1307: 1276:, retrieved 1263: 1257: 1243:, retrieved 1238: 1232: 1218:Bibliography 1207: 1198: 1146: 1125: 1116: 1107: 1086: 1077: 1042: 1016: 912:Theriiformes 898: 835:Notoungulata 821: 781: 768: 755: 742: 708: 652: 625: 593: 571:conglomerate 568: 536:amphibolites 513:Paraná State 473: 461: 443: 384: 382: 345:Year defined 312:Type section 263:-27.5; -39.8 224:-25.5; -49.3 185:Conglomerate 132: 1482:Divisaderan 1266:: 563–572, 1191:Fossilworks 1026:Casamayoran 783:Utaetus sp. 738:Dasypodidae 640:Divisaderan 602:, abundant 589:environment 554:Lithologies 530:comprising 501: [ 498:Guabirotuba 490: [ 479: [ 470:Description 454:terror bird 439:environment 399:) geologic 393:Divisaderan 321:Guabirotuba 261: / 222: / 197:Coordinates 40:42–38  33:Divisaderan 1456:Categories 1445:2019-02-15 1413:2019-03-04 1364:2019-03-04 1344:2019-03-04 1327:2017-10-26 1278:2019-03-04 1245:2019-03-04 1035:References 666:Itaboraian 608:tourmaline 586:floodplain 579:sandstones 564:floodplain 540:migmatites 521:rift basin 436:floodplain 429:sandstones 1316:: 39–55, 817:Cingulata 655:Tiupampan 614:and rare 606:, common 575:mudstones 458:Cingulata 425:mudstones 417:crops out 401:formation 339:Bigarella 317:Named for 175:sandstone 162:Lithology 154:Thickness 129:Underlies 1434:: 1–73, 1369:Archived 1286:citation 978:See also 949:Reptiles 692:Deseadan 690:and the 664:and the 632:Pliocene 532:gneisses 528:basement 525:Cambrian 509:Curitiba 421:Curitiba 335:Salamuni 331:Named by 325:Curitiba 191:Location 171:Mudstone 148:basement 145:Cambrian 141:Overlies 134:alluvium 1394:Bibcode 1241:: 29–48 954:Turtles 733:Mammals 721:Fossils 697:of the 686:of the 671:of the 660:of the 628:Miocene 612:kyanite 604:epidote 600:zircons 583:fluvial 542:of the 446:mammals 433:fluvial 403:of the 395:in the 284:Country 249:39°48′W 246:27°30′S 210:49°18′W 207:25°30′S 167:Primary 109:↓ 727:Notes 724:Images 636:mammal 616:rutile 413:Brazil 409:Paraná 337:& 302:Extent 296:Brazil 293:  278:Paraná 274:Region 1358:(PDF) 1304:(PDF) 1229:(PDF) 1008:Notes 928:Birds 718:Group 715:Class 505:] 494:] 483:] 387:is a 181:Other 1385:Gaea 1292:link 1193:.org 610:and 577:and 538:and 485:and 427:and 383:The 348:1962 119:Type 48:Preęž’ 1436:doi 1402:doi 1318:doi 1268:doi 1189:at 675:in 630:to 622:Age 407:in 1458:: 1432:21 1430:, 1424:, 1400:, 1388:, 1382:, 1314:24 1312:, 1306:, 1288:}} 1284:{{ 1264:42 1262:, 1256:, 1239:41 1237:, 1231:, 1155:^ 1134:^ 1095:^ 1065:^ 1051:^ 701:. 591:. 573:, 550:. 534:, 503:pt 492:pt 481:pt 460:; 441:. 411:, 323:, 173:, 98:Pg 42:Ma 27:: 1438:: 1404:: 1396:: 1390:8 1320:: 1294:) 1270:: 391:( 103:N 93:K 88:J 83:T 78:P 73:C 68:D 63:S 58:O 53:ęž’ 37:~ 35:) 31:(

Index

Stratigraphic range
Late Mid Eocene
Divisaderan
Ma
Preęž’
ęž’
O
S
D
C
P
T
J
K
Pg
N
Geological formation
alluvium
Cambrian
basement
Mudstone
sandstone
Conglomerate
Coordinates
25°30′S 49°18′W / 25.5°S 49.3°W / -25.5; -49.3
Approximate paleocoordinates
27°30′S 39°48′W / 27.5°S 39.8°W / -27.5; -39.8
Paraná
Brazil
Curitiba Basin

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