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Flexibilia

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377: 695: 398: 352: 124: 102: 604:. Treatise on invertebrate paleontology. By Georges Ubaghs, R. C. Moore, H. Wienberg Rasmussen, N. Gary Lane, Albert Breimer, H. L. Strimple, J. C. Brower, Russell M. Jeffords, James Sprinkle, R. E. Peck, D. B. Macurda, Jr., D. L. Meyer, Michel Roux, Hertha Sieverts-Doreck, R. O. Fay, and R. A. Robison. Boulder, CO and Lawrence, KS: University of Kansas and Geological Society of America. 272:
acts as an intermediate form linking the generalized anatomy of other early cladids with the distinctive anatomy of flexibles, and several studies have considered it to be ancestral to the rest of the group. Although flexibles never reached the same abundance or diversity as many other crinoid
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Three infrabasal plates (in contrast to the five found in other dicyclic crinoids). Two of these plates (the zygous plates) are the result of fusion, and are larger than the remaining (azygous) plate. The azygous infrabasal is almost always located under the C
376: 548:"New crinoids from the Baltic region (Estonia): fossil tip‐dating phylogenetics constrains the origin and Ordovician–Silurian diversification of the Flexibilia (Echinodermata)" 311:
Uniserial, inward-curling arms without pinnules. The branchials are broad and connected by a patelloid suture. Branching is variable though often isotomous (symmetrical).
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Numerous small interradial and interbrachial plates among larger components of the calyx. Anal plates form a tube or thin linear series above the posterior basal.
333:, though the monophyly of these orders has been called into question. The most recent discussion of Flexibilia taxonomy considers Taxocrinida to be 326: 283: 209: 736: 268: 330: 214: 755: 254:. They exhibited a conserved body plan and consistent suite of characteristics throughout their long history. Previously considered a 397: 351: 775: 609: 729: 302:
5 basal plates and 5 radial plates in the calyx. The radials typically form a straight surface for the arm bases.
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Wright, David F.; Ausich, William I.; Cole, Selina R.; Peter, Mark E.; Rhenberg, Elizabeth C. (2017).
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Low, flexible tegmen with large ambulacral and small interambulacral plates radiating from the mouth.
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with unclear affinities, later investigation determined that flexibles are well-nested within
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onwards. Flexible fossils are very rare in the Ordovician (the most common taxa being
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groups, they remained a reliable component of crinoid faunas, particularly from the
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appears to have been an interval of rapid diversification for the group.
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Moore, Raymond C. (1978). Moore, Raymond C.; Teichert, Curt (eds.).
652: 488:"Aberrations in the infrabasal circlet of the cladid crinoid genus 274: 74: 69: 54: 49: 39: 546:
Wright, David F.; Toom, Ursula (2017). Sevastopulo, George (ed.).
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Thick stem comprising thin, circular columnals without cirri.
436: 496:Palaeogeography, Palaeoclimatology, Palaeoecology 747: 730: 325:. It is traditionally split into the orders 737: 723: 601:Part T, Echinodermata 2, Crinoidea, vol. 2 545: 100: 563: 507: 454: 748: 318:Flexibilia is strongly supported as a 634: 633: 597: 485: 689: 593: 591: 541: 539: 537: 535: 432: 430: 428: 426: 294:Major traits of Flexibilia include: 262:, a broad group ancestral to living 756:Middle Ordovician first appearances 13: 14: 787: 588: 532: 423: 693: 396: 375: 350: 337:and ancestral to Sagenocrinida. 266:crinoids. The Ordovician cladid 122: 32: 479: 408:(Carboniferous, United States) 1: 416: 776:Prehistoric echinoderm stubs 709:. You can help Knowledge by 509:10.1016/j.palaeo.2019.03.002 7: 486:Peter, M. E. (2019-05-15). 10: 792: 688: 340: 642: 206: 201: 119:Scientific classification 117: 108: 99: 30:Middle Ordovician–Permian 23: 443:Journal of Paleontology 705:-related article is a 111:Onychocrinus ramulosus 16:Superorder of crinoids 761:Lopingian extinctions 668:Paleobiology Database 456:10.1017/jpa.2016.142 565:10.1111/pala.12324 718: 717: 701:This prehistoric 683: 682: 636:Taxon identifiers 611:978-0-8137-3021-9 244:Middle Ordovician 229: 228: 223: 197: 783: 739: 732: 725: 697: 690: 676: 675: 663: 662: 661: 631: 630: 624: 623: 595: 586: 585: 567: 543: 530: 529: 511: 483: 477: 476: 458: 434: 400: 379: 354: 217: 192: 187: 127: 126: 104: 94: 31: 27:Temporal range: 21: 20: 791: 790: 786: 785: 784: 782: 781: 780: 771:Crinoidea stubs 746: 745: 744: 743: 686: 684: 679: 671: 666: 657: 656: 651: 638: 628: 627: 612: 596: 589: 544: 533: 484: 480: 435: 424: 419: 414: 413: 412: 409: 401: 392: 380: 371: 355: 343: 289:Late Ordovician 238:of specialized 191: 185: 121: 95: 93: 92: 87: 82: 77: 72: 67: 62: 57: 52: 47: 42: 37: 29: 28: 25: 17: 12: 11: 5: 789: 779: 778: 773: 768: 763: 758: 742: 741: 734: 727: 719: 716: 715: 698: 681: 680: 678: 677: 664: 648: 646: 640: 639: 626: 625: 610: 587: 558:(6): 893–910. 531: 478: 449:(4): 829–846. 421: 420: 418: 415: 411: 410: 402: 395: 393: 381: 374: 372: 359:Forbesiocrinus 356: 349: 346: 345: 344: 342: 339: 316: 315: 312: 309: 306: 303: 300: 227: 226: 225: 224: 212: 204: 203: 199: 198: 183: 179: 178: 173: 169: 168: 163: 159: 158: 153: 149: 148: 143: 139: 138: 133: 129: 128: 115: 114: 106: 105: 97: 96: 88: 83: 78: 73: 68: 63: 58: 53: 48: 43: 38: 33: 26: 15: 9: 6: 4: 3: 2: 788: 777: 774: 772: 769: 767: 764: 762: 759: 757: 754: 753: 751: 740: 735: 733: 728: 726: 721: 720: 714: 712: 708: 704: 699: 696: 692: 691: 687: 674: 669: 665: 660: 654: 650: 649: 647: 645: 641: 637: 632: 621: 617: 613: 607: 603: 602: 594: 592: 583: 579: 575: 571: 566: 561: 557: 553: 552:Palaeontology 549: 542: 540: 538: 536: 527: 523: 519: 515: 510: 505: 501: 497: 493: 491: 482: 474: 470: 466: 462: 457: 452: 448: 444: 440: 433: 431: 429: 427: 422: 407: 406: 399: 394: 390: 389:Mississippian 386: 385: 378: 373: 369: 365: 364:Carboniferous 361: 360: 353: 348: 347: 338: 336: 332: 328: 327:Sagenocrinida 324: 321: 313: 310: 307: 304: 301: 297: 296: 295: 292: 290: 286: 285: 284:Protaxocrinus 280: 276: 271: 270: 265: 261: 257: 253: 249: 245: 241: 237: 233: 221: 216: 213: 211: 210:Sagenocrinida 208: 207: 205: 200: 195: 190: 184: 181: 180: 177: 174: 171: 170: 167: 164: 161: 160: 157: 156:Echinodermata 154: 151: 150: 147: 144: 141: 140: 137: 134: 131: 130: 125: 120: 116: 113: 112: 107: 103: 98: 91: 86: 81: 76: 71: 66: 61: 56: 51: 46: 41: 36: 22: 19: 711:expanding it 700: 685: 643: 600: 555: 551: 499: 495: 490:Cupulocrinus 489: 481: 446: 442: 405:Onychocrinus 403: 382: 357: 335:paraphyletic 320:monophyletic 317: 293: 282: 279:Cupulocrinus 278: 269:Cupulocrinus 267: 231: 230: 220:paraphyletic 188: 182:Superorder: 109: 18: 331:Taxocrinida 287:), but the 215:Taxocrinida 172:Parvclass: 750:Categories 644:Flexibilia 417:References 391:, Indiana) 384:Taxocrinus 264:articulate 236:superorder 232:Flexibilia 189:Flexibilia 24:Flexibilia 766:Crinoidea 659:Q50822283 582:134049045 574:0031-0239 526:134102417 518:0031-0182 502:: 52–61. 465:0022-3360 240:Paleozoic 166:Crinoidea 142:Kingdom: 136:Eukaryota 653:Wikidata 473:13806992 275:Silurian 256:subclass 252:crinoids 152:Phylum: 146:Animalia 132:Domain: 703:crinoid 368:Indiana 341:Gallery 260:Cladida 248:Permian 202:Orders 176:Cladida 162:Class: 620:531991 618:  608:  580:  572:  524:  516:  471:  463:  196:, 1895 194:Zittel 673:94456 578:S2CID 522:S2CID 469:S2CID 323:clade 234:is a 707:stub 616:OCLC 606:ISBN 570:ISSN 514:ISSN 461:ISSN 329:and 299:ray. 281:and 35:PreꞒ 560:doi 504:doi 500:522 451:doi 246:to 752:: 670:: 655:: 614:. 590:^ 576:. 568:. 556:60 554:. 550:. 534:^ 520:. 512:. 498:. 494:. 467:. 459:. 447:91 445:. 441:. 425:^ 366:, 250:) 222:?) 85:Pg 738:e 731:t 724:v 713:. 622:. 584:. 562:: 528:. 506:: 475:. 453:: 387:( 370:) 362:( 242:( 218:( 186:† 90:N 80:K 75:J 70:T 65:P 60:C 55:D 50:S 45:O 40:Ꞓ

Index

PreꞒ

O
S
D
C
P
T
J
K
Pg
N

Onychocrinus ramulosus
Scientific classification
Edit this classification
Eukaryota
Animalia
Echinodermata
Crinoidea
Cladida
Flexibilia
Zittel
Sagenocrinida
Taxocrinida
paraphyletic
superorder
Paleozoic
Middle Ordovician
Permian

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