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Mata Amarilla Formation

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115: 393: 342: 317: 324: 1046: 966: 499:. Varela (2014) recognized three informal sections (lower, middle, and upper) on the bases of sedimentological and sequence stratigraphic analysis. The lower section consists of fine-grained intervals with paleosols interbedded with laminated shale and coquina, representing coastal plain and lagoon paleoenvironments. 532:
features and paleosol-derived climatic proxies suggest a subtropical temperate-warm, at 12 ± 2.1 °C (53.6 ± 3.8 °F) and humid, with 1,404 ± 108 millimetres (55.3 ± 4.3 in)/yr, climate with marked rainfall seasonality during the deposition of this
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F. J. Goin, D. G. Poire, M. S. De Fuente, A. L. Cione, F. E. Novas, E. S. Bellosi, A. Ambrosio, O. Ferrer, N. D. Canessa, A. Carloni, J. Ferigolo, A. M. Ribeiro, M. S. Sales Viana, M. A. Reguero, M. G. Vucetich, S. Marenssi, M. F. Lima Filho and S. Agostinho. 2002. Paleontologia y geologia de los
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The Austral (or Magallanes) Basin, is located on the southwestern end of the South American Plate and it is bordered to the south by the Scotia Plate covering an area of approximately 230.000 square kilometres (88.803 sq mi). In the studied area, the Austral Basin underwent three main
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J. F. Petrulevicius, A. N. Varela, A. Iglesias, A. B. Zamuner, and D. G. Poiré. 2014. First Cenomanian record of insects in the southern Hemisphere, with Perforissidae (Fulgoroidea) and Cupedidae (Coleoptera) from southern Patagonia, Argentina. Cretaceous Research
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A. Iglesias, A. B. Zamuner, D. G. Poiré and F. Larriestra. 2007. Diversity, taphonomy, and palaeoecology of an angiosperm flora from the Cretaceous (Cenomanian-Coniacian) in southern Patagonia, Argentina. Palaeontology
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The foreland stage, in response to the regional change from extensive to compressive regime, resulted in the deposition of the continental Mata Amarilla Formation. This unit is mainly composed of grey and blackish
1180: 1122:. 1899. Nota preliminar sobre el Loncasaurus argentinus un representante de la familia de los Megalosauridae en la República Argentina . Anales de la Sociedad Científica Argentina 47:61-62 392: 1109:
sedimentos del cretacico superior aflorantes al sur del rio shehuen (Mata Amarilla, Provincia de Santa Cruz, Argentina). Actas del XV Congreso Geologico Argentino, El Calafate, 2002 1–6
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J. P. O'Gorman and A. N. Varela. 2010. The oldest lower Upper Cretaceous plesiosaurs (Reptilia, Sauropterygia) from Southern Patagonia, Argentina. Ameghiniana 47(4):447-459
1190: 1140: 1017:"U-Pb zircon constraints on the age of the Cretaceous Mata Amarilla Formation, Southern Patagonia, Argentina: Its relationship with the evolution of the Austral Basin" 1016: 872:
Martin, T.; Goin, F. J.; Schultz, J. A.; Gelfo, J. N. (2021). "Early Late Cretaceous mammals from southern Patagonia (Santa Cruz province, Argentina)".
1135: 341: 316: 1115:
J. Frenguelli. 1953. La Flora Fósil de la región del Alto Río Chalia en Santa Cruz (Patagonia). Paleontología. Notas del museo XVI(98):239-257
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M. B. Aguirre Urreta. 1989. The Cretaceous decapod Crustacea of Argentina and the Antarctic Peninsula. Palaeontology 32(3):499-552
286: 906: 1195: 1165: 1155: 1145: 941: 1058:"An abelisauroid dinosaur with a non-atrophied manus from the Late Cretaceous Pari Aike Formation of southern Patagonia" 251: 212: 205: 1160: 1150: 1170: 480: 156: 775: 454: 438:
were formed and filled with volcaniclastic and volcanic rocks intercalated with epiclastic sediments of the
398: 979:"A reappraisal of a putative record of abelisauroid theropod dinosaur from the Middle Jurassic of England" 464: 439: 146: 476: 526:
deposits. The upper section is dominated by fine-grained deposits, related to distal fluvial channels.
443: 373:, dated to 96.94 to 95.52 Ma. The middle section of the formation was previously considered to be the 990: 698: 410:
in age, but recent dating of a lava tuff layer shows that it dates back to 96.2 ± 0.7 Ma, during the
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Varela, A.N.; Poiré, D. G.; Martin, T.; Gerdes, A.; Goin, F. J.; Gelfo, J. N.; Hoffmann, S. (2012),
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tectonic stages: (i) a rift stage; (ii) a thermal subsidence stage; and (iii) a foreland stage.
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unit (Varela et al. 2012b; 2018), in accordance with previous paleobotanical interpretations.
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Santamarina, Patricio E.; Barreda, Viviana D.; Iglesias, Ari; Varela, Augusto N. (2018),
1057: 994: 1021: 705: 658: 582: 515: 244: 1129: 978: 893: 407: 66: 24: 936: 885: 1002: 937:"Salvinialean megaspores in the Late Cretaceous of southern Patagonia, Argentina" 910: 810: 607: 435: 41: 1050: 970: 1078: 803: 523: 519: 411: 406:
The middle section of the Mata Amarilla Formation has widely been regarded as
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The Mata Amarilla Formation has provided many fossil vertebrates, among which
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Paleogeography of the Late Cretaceous (90 Ma) with known distribution of
381: 193: 81: 76: 61: 56: 46: 1065: 1045: 965: 96: 71: 495:, alternating with whitish and yellowish-grey fine to medium grained 457: 431: 384:, fish and turtles, as well as fossil insects, flora and molluscs. 391: 969:
Material was copied from this source, which is available under a
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was deposited, representing a large passive-margin delta system.
472: 189: 340: 369:. The formation consists of sediments deposited during the 545: 1051:
Creative Commons Attribution 4.0 International License
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Creative Commons Attribution 4.0 International License
300: 292: 282: 243: 204: 199: 181: 167: 162: 152: 142: 134: 124: 18: 1181:Fossiliferous stratigraphic units of South America 1056:Ezcurra, M.D.; Agnolin, F.L.; Novas, F.E. (2010), 426:The rifting stage is related to the break-up of 323: 119:Map of Mata Amarilla and surrounding formations 867: 865: 863: 861: 8: 983:Proceedings of the Geologists' Association 113: 15: 1191:Geology of Santa Cruz Province, Argentina 518:deposits, intercalated with fine-grained 1141:Upper Cretaceous Series of South America 548: 453:stage resulted in the deposition of the 830: 720:Polyptychoceras (Polyptychoceras) sp. 479:. Towards the end of this stage, the 7: 331:Mata Amarilla Formation (Argentina) 14: 1136:Geologic formations of Argentina 1044: 964: 322: 315: 922:Santamarina et al., 2018, p.610 855:Santamarina et al., 2018, p.609 846:Santamarina et al., 2018, p.608 706:Anagaudryceras cf. politissimum 138:Upper, Middle and Lower members 1: 942:Acta Palaeontologica Polonica 886:10.1016/j.cretres.2021.105127 502:The middle section comprises 1003:10.1016/j.pgeola.2012.05.008 245:Approximate paleocoordinates 1176:Austral or Magallanes Basin 1212: 1186:Paleontology in Argentina 1079:10.11646/zootaxa.2450.1.1 310: 112: 23: 685:Treslagosodon shehuensis 678:Amarillodon meridionalis 510:representing meandering 481:Piedra Clavada Formation 157:Piedra Clavada Formation 1035:10.5027/andgeoV39n3-a01 741:Aonikenkissus zamunerae 355:fossiliferous formation 351:Mata Amarilla Formation 19:Mata Amarilla Formation 977:Rauhut, O.W.M (2012), 955:10.4202/app.00491.2018 776:Arcellites disciformis 567:Stratigraphic position 403: 399:Arcellites disciformis 346: 659:Elasmosauridae indet. 395: 344: 1196:Geology of Patagonia 1166:Siltstone formations 1156:Sandstone formations 1146:Cretaceous Argentina 783:Bignonites chalianus 465:Springhill Formation 345:Stratigraphic column 147:Alta Vista Formation 129:Geological Formation 995:2012PrGA..123..779R 874:Cretaceous Research 837:Varela et al., 2012 797:Laurophyllum kurtzi 713:Baculites cf. kirki 477:Río Mayer Formation 444:Tobífera Formations 375:Pari Aike Formation 287:Santa Cruz Province 263: /  224: /  25:Stratigraphic range 1049:available under a 790:Fitzroya tertiaria 671:Ausktribosphenidae 641:Ceratodus iheringi 451:thermal subsidence 449:Subsequently, the 404: 347: 804:?Schinopsis dubia 755:M. santacruzensis 748:Myrcia acutifolia 727:cf. Potamides sp. 634:Other vertebrates 630: 629: 371:Middle Cenomanian 339: 338: 34:96.94–95.52  1203: 1161:Shale formations 1151:Cenomanian Stage 1087: 1086: 1085: 1062: 1048: 1043: 1042: 1041: 1011: 1010: 1009: 968: 963: 962: 961: 923: 920: 914: 904: 898: 897: 869: 856: 853: 847: 844: 838: 835: 546: 522:and subordinate 512:fluvial channels 467:, and the black 326: 325: 319: 278: 277: 275: 274: 273: 268: 264: 261: 260: 259: 256: 239: 238: 236: 235: 234: 229: 225: 222: 221: 220: 217: 117: 108: 38: 16: 1211: 1210: 1206: 1205: 1204: 1202: 1201: 1200: 1171:Tuff formations 1126: 1125: 1094: 1092:Further reading 1083: 1081: 1060: 1055: 1039: 1037: 1014: 1007: 1005: 976: 959: 957: 934: 931: 926: 921: 917: 905: 901: 871: 870: 859: 854: 850: 845: 841: 836: 832: 828: 823: 811:Equisetites sp. 771: 736: 699:Glyphea oculata 694: 654:Chelidae indet. 636: 620:Middle Section 595:Middle Section 544: 539: 420: 390: 335: 334: 333: 332: 329: 328: 327: 271: 269: 265: 262: 257: 254: 252: 250: 249: 232: 230: 226: 223: 218: 215: 213: 211: 210: 120: 107: 106: 105: 104: 99: 94: 89: 84: 79: 74: 69: 64: 59: 54: 49: 44: 33: 32: 31: 12: 11: 5: 1209: 1207: 1199: 1198: 1193: 1188: 1183: 1178: 1173: 1168: 1163: 1158: 1153: 1148: 1143: 1138: 1128: 1127: 1124: 1123: 1116: 1113: 1110: 1106: 1102: 1099: 1093: 1090: 1089: 1088: 1053: 1029:(3): 359–379, 1022:Andean Geology 1012: 989:(5): 779–786, 974: 930: 927: 925: 924: 915: 899: 857: 848: 839: 829: 827: 824: 822: 821: 814: 807: 800: 793: 786: 779: 770: 767: 766: 765: 758: 751: 744: 735: 732: 731: 730: 723: 716: 709: 702: 693: 690: 689: 688: 681: 674: 668: 661: 656: 651: 644: 635: 632: 631: 628: 627: 625: 623: 621: 618: 616: 611: 603: 602: 600: 598: 596: 593: 591: 586: 583:Clasmodosaurus 578: 577: 574: 571: 568: 565: 562: 559: 555: 554: 543: 540: 538: 537:Fossil content 535: 516:crevasse splay 419: 416: 389: 386: 337: 336: 330: 321: 320: 314: 313: 312: 311: 308: 307: 302: 298: 297: 294: 290: 289: 284: 280: 279: 247: 241: 240: 208: 202: 201: 197: 196: 183: 179: 178: 169: 165: 164: 160: 159: 154: 150: 149: 144: 140: 139: 136: 132: 131: 126: 122: 121: 118: 110: 109: 102: 101: 100: 95: 90: 85: 80: 75: 70: 65: 60: 55: 50: 45: 40: 39: 29:Mid Cenomanian 21: 20: 13: 10: 9: 6: 4: 3: 2: 1208: 1197: 1194: 1192: 1189: 1187: 1184: 1182: 1179: 1177: 1174: 1172: 1169: 1167: 1164: 1162: 1159: 1157: 1154: 1152: 1149: 1147: 1144: 1142: 1139: 1137: 1134: 1133: 1131: 1121: 1117: 1114: 1111: 1107: 1105:50(2):445-466 1103: 1100: 1096: 1095: 1091: 1080: 1076: 1072: 1068: 1067: 1059: 1054: 1052: 1047: 1036: 1032: 1028: 1024: 1023: 1018: 1013: 1004: 1000: 996: 992: 988: 984: 980: 975: 972: 967: 956: 952: 948: 944: 943: 938: 933: 932: 928: 919: 916: 912: 908: 903: 900: 895: 891: 887: 883: 879: 875: 868: 866: 864: 862: 858: 852: 849: 843: 840: 834: 831: 825: 820: 819: 815: 813: 812: 808: 806: 805: 801: 799: 798: 794: 792: 791: 787: 785: 784: 780: 778: 777: 773: 772: 768: 764: 763: 762:Zygadenia sp. 759: 757: 756: 752: 750: 749: 745: 743: 742: 738: 737: 733: 729: 728: 724: 722: 721: 717: 715: 714: 710: 708: 707: 703: 701: 700: 696: 695: 691: 687: 686: 682: 680: 679: 675: 672: 669: 666: 662: 660: 657: 655: 652: 650: 649: 648:Lepidotes sp. 645: 643: 642: 638: 637: 633: 626: 624: 622: 619: 617: 615: 614:L. argentinus 612: 610: 609: 605: 604: 601: 599: 597: 594: 592: 590: 587: 585: 584: 580: 579: 575: 572: 569: 566: 563: 560: 557: 556: 553: 552: 547: 541: 536: 534: 531: 527: 525: 521: 517: 513: 509: 505: 500: 498: 494: 490: 484: 482: 478: 474: 470: 466: 462: 459: 456: 455:transgressive 452: 447: 445: 441: 437: 433: 429: 424: 417: 415: 413: 409: 408:Maastrichtian 401: 400: 394: 387: 385: 383: 378: 376: 372: 368: 364: 360: 359:Austral Basin 356: 352: 343: 318: 309: 306: 305:Austral Basin 303: 299: 295: 291: 288: 285: 281: 276: 267:56.5°S 48.8°W 248: 246: 242: 237: 228:49.5°S 71.5°W 209: 207: 203: 198: 195: 191: 187: 184: 180: 177: 173: 170: 166: 161: 158: 155: 151: 148: 145: 141: 137: 133: 130: 127: 123: 116: 111: 98: 93: 88: 83: 78: 73: 68: 63: 58: 53: 48: 43: 37: 30: 26: 22: 17: 1082:, retrieved 1070: 1064: 1038:, retrieved 1026: 1020: 1006:, retrieved 986: 982: 958:, retrieved 946: 940: 929:Bibliography 918: 907:Cerro Waring 902: 877: 873: 851: 842: 833: 818:Phylites sp. 816: 809: 802: 795: 788: 781: 774: 760: 753: 746: 739: 725: 718: 711: 704: 697: 683: 676: 646: 639: 613: 606: 588: 581: 549: 528: 501: 485: 448: 436:half-grabens 425: 421: 405: 397: 379: 361:in southern 350: 348: 272:-56.5; -48.8 233:-49.5; -71.5 949:: 607–616, 911:Fossilworks 608:Loncosaurus 520:floodplains 418:Description 270: / 231: / 206:Coordinates 1130:Categories 1098:51:174-185 1084:2019-10-13 1040:2019-10-13 1008:2019-10-13 960:2019-10-13 880:: 105127. 826:References 589:C. spatula 524:lacustrine 440:El Quemado 412:Cenomanian 894:245549530 665:Docodonta 551:Dinosaurs 542:Dinosaurs 508:siltstone 504:sandstone 497:sandstone 493:claystone 489:siltstone 461:sandstone 458:quartzose 402:indicated 382:dinosaurs 367:Argentina 363:Patagonia 296:Argentina 194:paleosols 186:Sandstone 176:claystone 172:Siltstone 163:Lithology 143:Underlies 135:Sub-units 1120:Ameghino 1073:: 1–25, 692:Molluscs 570:Material 564:Location 530:Paleosol 469:mudstone 428:Gondwana 200:Location 153:Overlies 1066:Zootaxa 991:Bibcode 734:Insects 576:Images 561:Species 475:of the 463:of the 432:grabens 357:of the 293:Country 258:48°48′W 255:56°30′S 219:71°30′W 216:49°30′S 168:Primary 103:↓ 892:  673:indet. 667:indet. 301:Extent 283:Region 1061:(PDF) 890:S2CID 769:Flora 573:Notes 558:Genus 353:is a 182:Other 1071:2450 913:.org 514:and 506:and 491:and 473:marl 471:and 442:and 434:and 349:The 190:tuff 125:Type 42:PreꞒ 1118:F. 1075:doi 1031:doi 999:doi 987:123 951:doi 909:at 882:doi 878:133 388:Age 1132:: 1069:, 1063:, 1027:39 1025:, 1019:, 997:, 985:, 981:, 947:63 945:, 939:, 888:. 876:. 860:^ 446:. 430:, 414:. 377:. 365:, 192:, 188:, 174:, 92:Pg 36:Ma 27:: 1077:: 1033:: 1001:: 993:: 973:. 953:: 896:. 884:: 663:? 97:N 87:K 82:J 77:T 72:P 67:C 62:D 57:S 52:O 47:Ꞓ

Index

Stratigraphic range
Mid Cenomanian
Ma
PreꞒ

O
S
D
C
P
T
J
K
Pg
N

Geological Formation
Alta Vista Formation
Piedra Clavada Formation
Siltstone
claystone
Sandstone
tuff
paleosols
Coordinates
49°30′S 71°30′W / 49.5°S 71.5°W / -49.5; -71.5
Approximate paleocoordinates
56°30′S 48°48′W / 56.5°S 48.8°W / -56.5; -48.8
Santa Cruz Province
Austral Basin

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