Knowledge (XXG)

Belemnoidea

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Diagenetic modifications of the shells are complex. Radiating calcitic crystals are thin, or very large, with a shape indicative of a strong alteration. In other samples, the aragonite - calcite boundary is not dependent on growth lines. In a given fossil sites, some specimens are calcite, others are
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The guard, phragmocone and pro-ostracum were all internal to the living creature, forming a skeleton which was enclosed entirely by soft muscular tissue. The original living creature would have been larger than the fossilized shell, with a long streamlined body and prominent eyes. The guard would
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Belemnoids were effectively neutrally buoyant, and swam in near-shore to mid-shelf oceans. Their fins could be used to their advantage in all water speeds; in a gentle current they could be flapped for propulsion; in a stronger current they could be held erect to generate lift; and when swimming
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guard whose main role appears to have been to counterbalance the front (towards the head) of the organism; it positions the centre of mass below the centre of buoyancy, increasing the stability of the swimming organism. The guard would account for between a third and a fifth of the length of the
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Very exceptional belemnoid specimens have been found showing the preserved soft parts of the animal. Elsewhere in the fossil record, bullet-shaped belemnite guards are locally found in such profusion that such deposits are referred to semi-formally as "belemnite battlefields" (cf.
566:" or "thunderstone" has also been traditionally applied to the fossilised rostra of belemnoids. The origin of these bullet-shaped stones was not understood, and thus a mythological explanation of stones created where lightning struck has arisen. 472:) is found. The guard is usually elongated and bullet-shaped (though in some subgroups the rostrum may only exist as a thin layer coating the phragmocone). The hollow region at the front of the guard is termed the 1198:
Barskov I.S., Kiyashko S.I.; Dauphin Y., Denis A. (1997). "Microstructures des zones calcitiques et aragonitiques des rostres de Goniocamax (Cephalopoda, Belemnitida) du Turonien de Sibérie du Nord".
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Dauphin, Y. (1988). "Microstructure versus mineralogical and chemical data to estimate the state of preservation of fossil shells : a belemnitid example (Cephalopoda - Coleoidea)".
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Dauphin, Y. (1984). "Etude de la variabilite microstructurale des rostres de belemnites a partir de specimens provenant d'un sondage D.S.D.P. (leg 36 site 330) de l'Atlantique sud".
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Dauphin, Y. (1988). "Diagenèse aragonite-calcite chez les CĂ©phalopodes Coleoides : exemples des rostres d'Aulacoceras (Trias de Turquie) et Belopterina (Eocène de France)".
1269: 1822: 482:). The phragmocone is usually only found with the better preserved specimens. Projecting forwards from one side of the phragmocone is the thin 638: 521:
have been in place toward the rear of the creature, with the phragmocone behind the head and the pointed end of the guard facing backward.
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Dauphin Y., Williams C.T. Barskov I.S. (2007). "Aragonitic rostra of the Turonian belemnitid Goniocamax: arguments from diagenesis".
331:. The belemnoids become extinct at the end of the Cretaceous period along with the ammonites. The belemnoids' origin lies within the 538:, can measure up to 46 centimetres (18 in) in length, giving the living animal an estimated length of 3 metres (10 ft). 1262: 1827: 1817: 509:, thus tending to preserve well. Broken guards show a structure of radiating calcite fibers and may also display concentric 1852: 1847: 1837: 1812: 1842: 1311: 1255: 136: 546:). It remains unclear whether these deposits represent post-mating mass death events, as are common among modern 1317: 1732: 1247: 757: 1779: 708: 1405: 913: 807: 783: 586:, southeast USA) has long been used as a global standard (Peedee Belemnite, "PDB") against which other 907: 887: 859: 801: 1807: 1218: 1092: 1040: 981: 853: 821: 745: 739: 651: 587: 575: 526: 871: 865: 827: 763: 839: 815: 1574: 893: 833: 795: 1472: 1454: 1108: 997: 939: 881: 751: 595: 591: 490: 300: 226: 131: 1027:
Fuchs, Dirk; Iba, Yasuhiro; Tischlinger, Helmut; Keupp, Helmut; Klug, Christian (October 2016).
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Monks, H. J. D.; Hardwick, J. D.; Gale, A. S. (1996). "The function of the belemnite guard".
1029:"The locomotion system of Mesozoic Coleoidea (Cephalopoda) and its phylogenetic significance" 1371: 1100: 1048: 989: 579: 444: 437: 1613: 1596: 1519: 901: 682: 614: 396: 296: 285: 218: 112: 1096: 1044: 985: 688: 666: 1676: 1580: 1529: 1524: 1486: 1242: 724: 622: 262: 122: 972:
Doyle, P.; Shakides, E. V. (2004). "The Jurassic Belemnite Suborder Belemnotheutina".
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Like some modern squid, belemnoid arms carried a series of small hooks for grabbing
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rapidly by jet propulsion they could be tucked in to the body for streamlining.
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Normally with fossil belemnoids only the back part of the shell (called the
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period; well-formed belemnoid guards can be found in rocks dating from the
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Comparation of hard parts of Phragmoteuthida, Belemnitida and Diplobelida.
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and with negative buoyancy. To the rear of the creature was a heavy
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from the Jurassic near Moneva Teruel, Spain. The barnacle borings (
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and other marine animals with their arms and ate them with their
670: 535: 501:, belemnoid guards are evolutionarily novel and are composed of 392: 384: 1730: 1251: 1219:"The Cephalopoda: Squids, octopuses, nautilus, and ammonites" 1310: 269:. The name "belemnoid" comes from the Greek word βέλεμνον, 1243:
TONMO.com Cephalopod Fossils articles and discussion forums
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Belemnoids possessed a central rostrom/guard made of
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meaning "a dart or arrow" and the Greek word είδος,
1739: 1664: 1502: 1326: 1289: 327:marine rocks, often accompanying their cousins the 650:Belemnoid from the very top bedding plane of the 1015:Webster's New Universal Unabridged Dictionary. 347:) onward through the Cretaceous. Other fossil 1263: 8: 578:composition of a belemnoid rostrum from the 261:, but, unlike the squid, they possessed ten 1078: 1076: 1074: 1072: 1070: 1727: 1508: 1332: 1270: 1256: 1248: 253:, very similar in many ways to the modern 126:, showing arm hooks and outline of mantle 111: 31: 1543:First appearance of long-lasting lineages 960:The Ammonites: Their life and their world 436:A belemnoid fossil with preserved guard, 257:. Like them, the belemnoids possessed an 951: 698:, with belemnites in the stomach region 962:. London: Cambridge University Press. 7: 677:illumination, from Cairn Hill mine, 415:hooks from the arms of cephalopods. 311:Belemnoids were numerous during the 27:Extinct group of squid-like animals 380:complete organism, arms included. 25: 1128:Bull. Mus. Natn. Hist. Nat. Paris 613:, particularly in the Cretaceous 489:While belemnoid phragmocones are 1516:Earliest unambiguous cephalopods 994:10.1111/j.0031-0239.2004.00395.x 335:nautiloids, which date from the 265:of roughly equal length, and no 135: 590:samples are measured, for both 249:are an extinct group of marine 1612:the earliest cephalopod group 1298:The belemnite-cuttlefish-like 497:and are similarly composed of 1: 1823:Cephalopods by classification 1671:Probable misidentified genera 1642:Earliest coiled cephalopods: 1283:(listed by first occurrence) 1085:Paläontologische Zeitschrift 387:. Belemnoids were efficient 524:The guard of the belemnoid 1879: 1858:Devonian first appearances 1556:Probable coleoid ancestor 1130:. 4è sĂ©rie, 10 C: 107–135. 634:Note: all families extinct 299:), and diplobelids (order 295:), phragmoteuthids (order 120:Well preserved diplobelid 1863:Maastrichtian extinctions 1833:Carboniferous cephalopods 1605: 1511: 1442: 1422: 1362: 1335: 1308: 625:in which they are found. 601:Some belemnoids (such as 493:with the shells of other 212: 207: 132:Scientific classification 130: 119: 110: 34: 673:belemnite rostrum under 123:Clarkeiteuthis conocauda 440:remnants, and arm hooks 291:), aulacocerids (order 240:Artist's reconstruction 1828:Cretaceous cephalopods 1315: 1217:Vendetti, Jan (2006). 1181:Revue de PalĂ©obiologie 1162:Revue de PalĂ©obiologie 699: 685: 663: 643: 461: 441: 243: 1818:Paleozoic cephalopods 1780:Paleobiology Database 1314: 691: 669: 649: 641: 447: 435: 284:(which belong to the 238: 1853:Triassic cephalopods 1848:Jurassic cephalopods 1838:Devonian cephalopods 1813:Mesozoic cephalopods 1143:Acta Palaeontol. Pol 758:Palaeobelemnopseidae 621:to date the age the 617:of Europe, enabling 588:isotope geochemistry 530:, which is found in 527:Megateuthis gigantea 1843:Permian cephalopods 1097:1996PalZ...70..425M 1045:2016Letha..49..433F 986:2004Palgy..47..983D 411:frequently contain 407:, whose fossilized 319:periods, and their 280:Belemnoids include 41:Devonian–Cretaceous 1316: 1105:10.1007/BF02988082 958:Lehmann, U. 1981. 940:List of belemnites 700: 686: 664: 644: 544:"orthocone orgies" 462: 451:Hibolites hastatus 442: 391:that caught small 244: 1795: 1794: 1733:Taxon identifiers 1724: 1723: 1660: 1659: 1498: 1497: 1406:Paleocirroteuthis 1053:10.1111/let.12155 914:Rhiphaeoteuthidae 808:Salpingoteuthidae 784:Cylindroteuthidae 704:Clade Belemnoidea 635: 233: 232: 16:(Redirected from 1870: 1788: 1787: 1775: 1774: 1773: 1760: 1759: 1758: 1728: 1509: 1372:Muensterelloidea 1333: 1284: 1272: 1265: 1258: 1249: 1230: 1229: 1227: 1226: 1214: 1208: 1207: 1195: 1189: 1188: 1176: 1170: 1169: 1157: 1151: 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Australia 652:Zohar Formation 631: 615:Chalk Formation 596:oxygen isotopes 592:carbon isotopes 572: 560: 430: 421: 369: 309: 297:Phragmoteuthida 225: 221: 219:Phragmoteuthida 217: 198: 134: 106: 104: 103: 98: 93: 88: 83: 78: 73: 68: 63: 58: 53: 48: 40: 39: 36: 28: 23: 22: 15: 12: 11: 5: 1876: 1874: 1866: 1865: 1860: 1855: 1850: 1845: 1840: 1835: 1830: 1825: 1820: 1815: 1810: 1800: 1799: 1793: 1792: 1790: 1789: 1776: 1761: 1745: 1743: 1737: 1736: 1731: 1722: 1721: 1719: 1718: 1711: 1704: 1697: 1692: 1677:Nectocarididae 1674: 1672: 1668: 1666: 1662: 1661: 1658: 1657: 1655: 1654: 1646: 1640: 1630: 1616: 1610: 1606: 1603: 1602: 1600: 1599: 1594: 1584: 1581:Syllipsimopodi 1560: 1554: 1544: 1540: 1539: 1530:Monoplacophora 1525:Plectronoceras 1512: 1506: 1500: 1499: 1496: 1495: 1493: 1492: 1491: 1490: 1487:Belemnotheutis 1483: 1476: 1463: 1452: 1450: 1443: 1440: 1439: 1437: 1436: 1430: 1423: 1420: 1419: 1417: 1416: 1409: 1402: 1395: 1388: 1381: 1374: 1369: 1367: 1366:Early coleoids 1363: 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UC Berkeley 1220: 1213: 1210: 1205: 1201: 1200:Geodiversitas 1194: 1191: 1186: 1182: 1175: 1172: 1167: 1163: 1156: 1153: 1148: 1144: 1137: 1134: 1129: 1122: 1119: 1114: 1110: 1106: 1102: 1098: 1094: 1090: 1086: 1079: 1077: 1075: 1073: 1071: 1067: 1062: 1058: 1054: 1050: 1046: 1042: 1038: 1034: 1030: 1023: 1020: 1017:2nd ed. 1979. 1016: 1011: 1008: 1003: 999: 995: 991: 987: 983: 979: 975: 974:Palaeontology 968: 965: 961: 955: 952: 945: 941: 938: 936: 933: 931: 928: 927: 923: 915: 911: 909: 905: 904: 903: 899: 895: 891: 889: 885: 884: 883: 879: 873: 869: 867: 863: 861: 857: 856: 855: 851: 847: 843: 841: 840:Dimitobelidae 837: 835: 831: 829: 825: 823: 819: 818: 817: 816:Belemnopseina 813: 809: 805: 803: 799: 797: 793: 791: 787: 785: 781: 780: 779: 775: 774: 773: 769: 765: 761: 759: 755: 753: 749: 747: 743: 741: 737: 736: 735: 731: 727: 726: 721: 719: 718: 713: 712: 710: 707: 706: 705: 702: 701: 697: 696: 690: 684: 680: 676: 672: 668: 661: 657: 653: 648: 640: 636: 628: 626: 624: 620: 616: 612: 611:index fossils 608: 604: 599: 597: 593: 589: 585: 581: 577: 569: 567: 565: 558:Thunderstones 557: 555: 553: 549: 545: 539: 537: 533: 529: 528: 522: 518: 514: 512: 508: 504: 500: 496: 492: 487: 485: 481: 480: 475: 471: 467: 459: 458: 453: 452: 446: 439: 434: 427: 425: 418: 416: 414: 410: 406: 402: 398: 394: 390: 386: 381: 378: 374: 366: 364: 362: 358: 354: 350: 346: 345:Carboniferous 342: 341:Mississippian 338: 334: 330: 326: 322: 318: 314: 306: 304: 302: 298: 294: 290: 287: 283: 278: 276: 272: 268: 264: 260: 256: 252: 248: 241: 237: 229: 228: 224: 220: 216: 211: 206: 203: 197: 194: 193: 190: 187: 184: 183: 180: 177: 174: 173: 170: 167: 164: 163: 160: 157: 154: 153: 150: 147: 144: 143: 138: 133: 129: 125: 124: 118: 114: 109: 102: 97: 92: 87: 82: 77: 72: 67: 62: 57: 52: 47: 33: 30: 19: 1740: 1713: 1708:Shelbyoceras 1706: 1701:Volborthella 1699: 1695:Kirengellida 1686: 1680: 1649: 1644:Tarphycerida 1632:Brevicones: 1628:Actinocerida 1618:Orthocones: 1592:Aulacocerids 1587: 1579: 1575:Gordoniconus 1573: 1567: 1535:Knightoconus 1533: 1532:-like form: 1523: 1515: 1485: 1478: 1471: 1458: 1447: 1413:Vampyronassa 1411: 1404: 1399:Palaeoctopus 1397: 1390: 1383: 1376: 1318:Evolution of 1299: 1223:. 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Index

Belemnoid
Preęž’
ęž’
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P
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Clarkeiteuthis conocauda
Scientific classification
Edit this classification
Eukaryota
Animalia
Mollusca
Cephalopoda
Coleoidea
Belemnoidea
Aulacocerida
Phragmoteuthida
Belemnitida
Diplobelida

Artist's reconstruction
cephalopod

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