29:
162:
Magellan
Seamounts. The lower slopes are gentle but steepen between 1,700–2,000-metre (5,600–6,600 ft) depth. Only the lower slopes are covered with thick sediment layers; the upper slopes have sediment accumulations only in sheltered areas and also feature step-like structures. A number of volcanic cones grew on Ioah and form morphostructures, with a density of about 11.1 vents per 1,000 square kilometres (390 sq mi). Some of these vents form alignments and Ioah lies at the intersection of two
48:
41:
161:
on the western; the reef deposits form a sometimes 5 kilometres (3.1 mi) wide and in total about 200 kilometres (120 mi) long ring around the summit platform of Ioah Guyot and cover an area of about 315 square kilometres (122 sq mi), making it the largest limestone outcrop of the
153:
with an arcuate shape; the two halves that make it up have dimensions of 110 by 66 kilometres (68 mi × 41 mi) and 83 by 65 kilometres (52 mi × 40 mi). The guyot rises 4.5 kilometres (2.8 mi) from the seafloor to 1,420 metres (4,660 ft)–1,380 metres
154:(4,530 ft) depth, forming a summit plateau with a surface area of 1,380 square kilometres (530 sq mi) that is covered by 25–75-metre (82–246 ft) high hills. The rim of the summit plateau is formed by volcanic rocks on the eastern part of the seamount and by
1722:
Zakharov, Yuri D.; Melnikov, Mikhael E.; Popov, Alexander M.; Pletnev, Sergej P.; Khudik, Vladimir D.; Punina, Tatiana A. (January 2012). "Cephalopod and brachiopod fossils from the
Pacific: Evidence from the Upper Cretaceous of the Magellan Seamounts".
145:
guyot lies south-southeast of Ioah and
Pallada guyot north-northwest, other seamounts in the area east of Ioah are Changpogo, Gramberg, Zatonskii and Arirang. There are about 1000 seamounts in the central western Pacific.
1474:
Koppers, Anthony A. P.; Staudigel, Hubert; Pringle, Malcolm S.; Wijbrans, Jan R. (October 2003). "Short-lived and discontinuous intraplate volcanism in the South
Pacific: Hot spots or extensional volcanism?".
1436:
Koppers, Anthony A.P.; Staudigel, Hubert; Wijbrans, Jan R.; Pringle, Malcolm S. (November 1998). "The
Magellan seamount trail: implications for Cretaceous hotspot volcanism and absolute Pacific plate motion".
311:-containing minerals were deposited over time on Ioah; presently the guyot contains about 150,000,000–200,000,000 tonnes (150,000,000–200,000,000 long tons; 170,000,000–220,000,000 short tons) of
1599:
Mel'nikov, M. E.; Tugolesov, D. D.; Pletnev, S. P. (August 2010). "The structure of the incoherent sediments in the Ita Mai Tai Guyot (Pacific Ocean) based on geoacoustic profiling data".
1354:
Glasby, Geoffrey P.; Ren, Xiangwen; Shi, Xuefa; Pulyaeva, Irina A. (2 February 2007). "Co–rich Mn crusts from the
Magellan Seamount cluster: the long journey through time".
1562:
Mel'nikov, M. E.; Pletnev, S. P.; Anokhin, V. M.; Sedysheva, T. E.; Ivanov, V. V. (November 2016). "Volcanic edifices on guyots of the
Magellan Seamounts (Pacific Ocean)".
644:
Asavin, A. M.; Kubrakova, I. V.; Mel’nikov, M. E.; Tyutyunnik, O. A.; Chesalova, E. I. (May 2010). "Geochemical zoning in ferromanganese crusts of Ita-MaiTai guyot".
760:
Okamoto, Nobuyuki; Usui, Akira (4 March 2014). "Regional
Distribution of Co-Rich Ferromanganese Crusts and Evolution of the Seamounts in the Northwestern Pacific".
1317:
Bogdanov, Yu. A.; Zonenshayn, L. P.; Lisitsyn, A. P.; Podrazhanskiy, A. M.; Sagalevich, A. M.; Sorokhtin, O. G. (August 1987). "Ferromanganese Ores on
Seamounts".
397:. Ioah developed the largest reefs of the Magellan Seamounts, with coral material accumulating to thicknesses of 200–300 metres (660–980 ft). During the
28:
1772:
1549:
Mel'nikov, M. E.; Pletnev, S. P.; Basov, I. A. (2006). "New
Geological and Paleontological Data on Fedorov Guyot, Magellan Seamounts, Pacific".
1512:
Mel'nikov, M. E.; Avdonin, V. V.; Pletnev, S. P.; Sedysheva, T. E. (January 2016). "Buried ferromanganese nodules of the Magellan Seamounts".
1391:
Keller, N. B.; Shcherba, I. G. (March 2006). "Features of the distribution of azooxanthellata scleractinia (Anthozoa) on mid-pacific guyots".
1644:
Pletnev, S. P. (1 September 2019). "Main Types of Aptian–Cenomanian Sedimentary Rocks on Guyots of the Magellan Mountains, Pacific Ocean".
1683:"The Main Types of Paleogene Sedimentary Rocks and Conditions of their Formation on the Guyots of the Magellan Seamounts (Pacific Ocean)"
61:
717:
Utkin, V. P. (June 2006). "Role of strike-slip faulting of the oceanic lithosphere in the formation of pacific volcanic belts".
138:
40:
1257:
Reich, Mike; Kutscher, Manfred (2015). "Sea pens (Octocorallia: Pennatulacea) from the Late Cretaceous of northern Germany".
1072:"First Find of Platinum in Cosmogenic Spherules of Ferromanganese Crusts (Fedorov Guyot, Magellan Seamounts, Pacific Ocean)"
1762:
1767:
504:
498:
307:
and reach thicknesses of 10 centimetres (3.9 in), although they only cover small sectors of Ioah Guyot.
178:
362:
were it still active. Compositionally, volcanic rocks from Ioah resemble these of the Rarotonga hotspot.
167:
1070:
Savelyev, D. P.; Khanchuk, A. I.; Savelyeva, O. L.; Moskaleva, S. V.; Mikhailik, P. E. (1 April 2020).
137:
seamount. It is also known as Fedorov and Ioan/ IOAN, which stands for "Institute of Oceanology of the
1608:
1484:
1446:
1400:
1363:
1326:
1083:
726:
338:; its estimated age is placed in a range between 88.5 and 86.2 million years. It was located in the
339:
1710:
1669:
1632:
1587:
1537:
1500:
1424:
1379:
1282:
1107:
785:
742:
669:
126:
86:
1740:
1702:
1682:
1661:
1624:
1579:
1529:
1462:
1416:
1342:
1274:
1099:
1071:
777:
661:
351:
347:
163:
1732:
1694:
1653:
1616:
1571:
1521:
1492:
1454:
1450:
1408:
1371:
1334:
1266:
1091:
769:
734:
653:
82:
359:
335:
1612:
1488:
1404:
1367:
1330:
1087:
730:
627:
625:
623:
621:
619:
617:
150:
130:
90:
1458:
1756:
1714:
1673:
1636:
1591:
1541:
1504:
1428:
1383:
1286:
1111:
789:
746:
673:
522:
493:
390:
355:
331:
190:
94:
78:
346:
age. The formation of Ioah and the other Magellan Seamounts has been explained by a
486:
458:
284:
210:
1736:
417:, and up to 150 metres (490 ft) sediments accumulated on the summit plateau.
773:
947:
945:
414:
405:
were emplaced on the seamount. Ferromanganese crusts developed later during the
318:. Some of these ferromanganese deposits form nodules encased within limestones.
312:
241:
142:
134:
1698:
1657:
1620:
1575:
1525:
1412:
1375:
1338:
1095:
932:
930:
928:
738:
657:
589:
587:
517:
474:
446:
426:
370:
304:
288:
202:
106:
1744:
1706:
1665:
1628:
1583:
1533:
1466:
1420:
1346:
1278:
1103:
781:
665:
462:
434:
406:
386:
374:
308:
253:
233:
222:
206:
194:
158:
547:
1496:
966:
964:
962:
960:
801:
799:
442:
430:
378:
319:
296:
292:
280:
268:
264:
198:
174:
171:
98:
74:
604:
602:
574:
572:
570:
568:
236:
and other carbonates were emplaced on the seamount, followed during the
1220:
1208:
1033:
982:
631:
470:
454:
438:
410:
343:
272:
260:
245:
218:
214:
102:
903:
901:
1270:
697:
695:
478:
466:
398:
394:
366:
300:
237:
226:
1124:
1057:
877:
865:
686:
342:
as it formed. Some secondary volcanic cones may be much younger, of
489:
482:
450:
114:
993:
991:
888:
886:
402:
382:
276:
249:
230:
155:
110:
1160:
1148:
1136:
951:
919:
101:
87 million years ago, but may have continued erupting into the
315:
853:
593:
1244:
1232:
1172:
936:
225:
cover the exposed rocks and formed through the breakup of
970:
805:
608:
578:
330:
The seamount developed about 87 million years ago on the
1045:
1021:
907:
701:
21:
508:which is usually found in much shallower waters.
385:system. A secondary reefal phase occurred during
1299:
997:
892:
259:Ferromanganese crusts on the seamount contain
485:has been identified on Ioah Guyot, including
8:
425:Species that lived on Ioah Guyot during the
712:
710:
189:Volcanic rocks found on Ioah Guyot include
27:
18:
1196:
1184:
1009:
854:Mel'nikov, Tugolesov & Pletnev 2010
841:
829:
817:
762:Marine Georesources & Geotechnology
594:Mel'nikov, Tugolesov & Pletnev 2010
534:
350:that would now be located close to the
542:
540:
538:
7:
1477:Geochemistry, Geophysics, Geosystems
1439:Earth and Planetary Science Letters
971:Mel'nikov, Pletnev & Basov 2006
806:Mel'nikov, Pletnev & Basov 2006
609:Mel'nikov, Pletnev & Basov 2006
579:Mel'nikov, Pletnev & Basov 2006
1687:Russian Journal of Pacific Geology
1646:Russian Journal of Pacific Geology
1564:Russian Journal of Pacific Geology
322:of cosmic origin have been found.
217:formed by hydrothermal processes.
14:
1681:Pletnev, S. P. (1 January 2021).
393:times and a third one during the
381:on Ioah Guyot which developed a
46:
39:
1514:Lithology and Mineral Resources
139:Academy of Sciences of the USSR
1773:Seamounts of the Pacific Ocean
166:. The seamount rises from the
1:
1737:10.1016/j.geobios.2011.11.011
1459:10.1016/S0012-821X(98)00175-7
65:Location in the Pacific Ocean
16:Seamount in the Pacific Ocean
1319:International Geology Review
774:10.1080/1064119x.2013.877110
47:
505:Peponocyathus australiensis
252:deposits on the slopes and
121:Geography and geomorphology
1789:
1300:Keller & Shcherba 2006
998:Keller & Shcherba 2006
893:Keller & Shcherba 2006
646:Geochemistry International
377:and volcanic rocks formed
1699:10.1134/S1819714021010061
1658:10.1134/S1819714019050087
1621:10.1134/s0001437010040144
1576:10.1134/s1819714016060038
1526:10.1134/s0024490215060073
1413:10.1134/s000143700602010x
1376:10.1007/s00367-007-0055-5
1339:10.1080/00206818709466192
1096:10.1134/S1028334X20040157
739:10.1134/S1028334X06050023
658:10.1134/s0016702910050010
499:Fungiacyathus pliciseptus
256:have also been reported.
125:The guyot belongs to the
26:
179:Ogasawara Fracture Zones
1451:1998E&PSL.163...53K
1259:Journal of Paleontology
129:which stretch from the
1076:Doklady Earth Sciences
719:Doklady Earth Sciences
1125:Mel'nikov et al. 2016
1058:Mel'nikov et al. 2016
878:Mel'nikov et al. 2016
866:Mel'nikov et al. 2016
687:Mel'nikov et al. 2016
1763:Cretaceous volcanoes
1497:10.1029/2003GC000533
1245:Zakharov et al. 2012
1233:Zakharov et al. 2012
1221:Bogdanov et al. 1987
1209:Bogdanov et al. 1987
1173:Zakharov et al. 2012
1034:Bogdanov et al. 1987
983:Bogdanov et al. 1987
937:Zakharov et al. 2012
632:Bogdanov et al. 1987
481:. Presently, a rich
62:class=notpageimage|
1613:2010Ocgy...50..582M
1489:2003GGG.....4.1089K
1405:2006Ocgy...46..238K
1368:2007GML....27..315G
1331:1987IGRv...29..968B
1247:, pp. 146–147.
1161:Koppers et al. 2003
1149:Koppers et al. 1998
1137:Koppers et al. 2003
1088:2020DokES.491..199S
952:Koppers et al. 1998
920:Koppers et al. 1998
731:2006DokES.409..692U
340:Southern Hemisphere
1356:Geo-Marine Letters
1046:Glasby et al. 2007
1022:Glasby et al. 2007
908:Glasby et al. 2007
702:Glasby et al. 2007
177:, between the two
168:East Mariana Basin
164:strike-slip faults
127:Magellan Seamounts
87:Magellan Seamounts
1768:Miocene volcanoes
1551:Tikhookean. Geol.
352:Rarotonga hotspot
113:developed on the
93:that has erupted
35:
34:
1780:
1748:
1718:
1677:
1640:
1595:
1558:
1545:
1508:
1470:
1432:
1387:
1350:
1303:
1297:
1291:
1290:
1271:10.1666/10-109.1
1254:
1248:
1242:
1236:
1230:
1224:
1218:
1212:
1206:
1200:
1194:
1188:
1182:
1176:
1170:
1164:
1158:
1152:
1146:
1140:
1134:
1128:
1122:
1116:
1115:
1067:
1061:
1055:
1049:
1043:
1037:
1031:
1025:
1019:
1013:
1007:
1001:
995:
986:
980:
974:
968:
955:
949:
940:
934:
923:
917:
911:
905:
896:
890:
881:
875:
869:
863:
857:
851:
845:
839:
833:
827:
821:
815:
809:
803:
794:
793:
757:
751:
750:
714:
705:
699:
690:
684:
678:
677:
641:
635:
629:
612:
606:
597:
591:
582:
576:
563:
562:
560:
558:
552:Seamount Catalog
544:
149:Ioah Guyot is a
83:Marshall Islands
50:
49:
43:
31:
19:
1788:
1787:
1783:
1782:
1781:
1779:
1778:
1777:
1753:
1752:
1751:
1721:
1680:
1643:
1598:
1561:
1548:
1511:
1473:
1435:
1390:
1353:
1316:
1312:
1307:
1306:
1298:
1294:
1256:
1255:
1251:
1243:
1239:
1231:
1227:
1219:
1215:
1207:
1203:
1195:
1191:
1183:
1179:
1171:
1167:
1159:
1155:
1147:
1143:
1135:
1131:
1123:
1119:
1069:
1068:
1064:
1056:
1052:
1044:
1040:
1032:
1028:
1020:
1016:
1008:
1004:
996:
989:
981:
977:
969:
958:
950:
943:
935:
926:
918:
914:
906:
899:
891:
884:
876:
872:
864:
860:
852:
848:
840:
836:
828:
824:
816:
812:
804:
797:
759:
758:
754:
716:
715:
708:
700:
693:
685:
681:
643:
642:
638:
630:
615:
607:
600:
592:
585:
577:
566:
556:
554:
548:"Ioah Seamount"
546:
545:
536:
531:
514:
423:
360:Society hotspot
328:
187:
123:
81:, close to the
68:
67:
66:
64:
58:
57:
56:
55:
51:
17:
12:
11:
5:
1786:
1784:
1776:
1775:
1770:
1765:
1755:
1754:
1750:
1749:
1731:(1): 145–156.
1719:
1678:
1652:(5): 436–445.
1641:
1607:(4): 582–590.
1596:
1570:(6): 435–442.
1559:
1553:(in Russian).
1546:
1509:
1471:
1445:(1–4): 53–68.
1433:
1399:(2): 238–241.
1388:
1362:(5): 315–323.
1351:
1325:(8): 968–984.
1313:
1311:
1308:
1305:
1304:
1302:, p. 239.
1292:
1249:
1237:
1235:, p. 145.
1225:
1223:, p. 981.
1213:
1211:, p. 982.
1201:
1189:
1177:
1175:, p. 146.
1165:
1153:
1141:
1129:
1127:, p. 439.
1117:
1062:
1050:
1048:, p. 319.
1038:
1036:, p. 976.
1026:
1024:, p. 320.
1014:
1012:, p. 443.
1002:
1000:, p. 238.
987:
985:, p. 977.
975:
956:
941:
939:, p. 147.
924:
912:
910:, p. 316.
897:
895:, p. 240.
882:
880:, p. 441.
870:
868:, p. 437.
858:
856:, p. 586.
846:
834:
832:, p. 438.
822:
810:
795:
752:
706:
704:, p. 317.
691:
679:
636:
634:, p. 971.
613:
598:
596:, p. 589.
583:
564:
533:
532:
530:
527:
526:
525:
520:
513:
510:
422:
419:
327:
324:
186:
183:
151:shield volcano
131:Mariana Trench
122:
119:
91:shield volcano
85:. Part of the
60:
59:
53:
52:
45:
44:
38:
37:
36:
33:
32:
24:
23:
15:
13:
10:
9:
6:
4:
3:
2:
1785:
1774:
1771:
1769:
1766:
1764:
1761:
1760:
1758:
1746:
1742:
1738:
1734:
1730:
1726:
1720:
1716:
1712:
1708:
1704:
1700:
1696:
1692:
1688:
1684:
1679:
1675:
1671:
1667:
1663:
1659:
1655:
1651:
1647:
1642:
1638:
1634:
1630:
1626:
1622:
1618:
1614:
1610:
1606:
1602:
1597:
1593:
1589:
1585:
1581:
1577:
1573:
1569:
1565:
1560:
1556:
1552:
1547:
1543:
1539:
1535:
1531:
1527:
1523:
1519:
1515:
1510:
1506:
1502:
1498:
1494:
1490:
1486:
1482:
1478:
1472:
1468:
1464:
1460:
1456:
1452:
1448:
1444:
1440:
1434:
1430:
1426:
1422:
1418:
1414:
1410:
1406:
1402:
1398:
1394:
1389:
1385:
1381:
1377:
1373:
1369:
1365:
1361:
1357:
1352:
1348:
1344:
1340:
1336:
1332:
1328:
1324:
1320:
1315:
1314:
1309:
1301:
1296:
1293:
1288:
1284:
1280:
1276:
1272:
1268:
1264:
1260:
1253:
1250:
1246:
1241:
1238:
1234:
1229:
1226:
1222:
1217:
1214:
1210:
1205:
1202:
1199:, p. 80.
1198:
1193:
1190:
1187:, p. 81.
1186:
1181:
1178:
1174:
1169:
1166:
1163:, p. 25.
1162:
1157:
1154:
1151:, p. 66.
1150:
1145:
1142:
1139:, p. 19.
1138:
1133:
1130:
1126:
1121:
1118:
1113:
1109:
1105:
1101:
1097:
1093:
1089:
1085:
1081:
1077:
1073:
1066:
1063:
1059:
1054:
1051:
1047:
1042:
1039:
1035:
1030:
1027:
1023:
1018:
1015:
1011:
1006:
1003:
999:
994:
992:
988:
984:
979:
976:
972:
967:
965:
963:
961:
957:
954:, p. 55.
953:
948:
946:
942:
938:
933:
931:
929:
925:
922:, p. 56.
921:
916:
913:
909:
904:
902:
898:
894:
889:
887:
883:
879:
874:
871:
867:
862:
859:
855:
850:
847:
844:, p. 72.
843:
838:
835:
831:
826:
823:
820:, p. 75.
819:
814:
811:
807:
802:
800:
796:
791:
787:
783:
779:
775:
771:
767:
763:
756:
753:
748:
744:
740:
736:
732:
728:
724:
720:
713:
711:
707:
703:
698:
696:
692:
688:
683:
680:
675:
671:
667:
663:
659:
655:
651:
647:
640:
637:
633:
628:
626:
624:
622:
620:
618:
614:
610:
605:
603:
599:
595:
590:
588:
584:
580:
575:
573:
571:
569:
565:
553:
549:
543:
541:
539:
535:
528:
524:
523:Vlinder Guyot
521:
519:
516:
515:
511:
509:
507:
506:
501:
500:
495:
494:zooxanthelles
491:
488:
487:scleractinian
484:
480:
476:
472:
468:
464:
460:
456:
452:
448:
444:
440:
436:
432:
428:
420:
418:
416:
412:
408:
404:
400:
396:
392:
391:Maastrichtian
388:
384:
380:
376:
372:
368:
363:
361:
357:
356:Samoa hotspot
353:
349:
345:
341:
337:
333:
332:Pacific Plate
325:
323:
321:
317:
314:
310:
306:
302:
298:
294:
290:
286:
282:
278:
274:
270:
266:
262:
257:
255:
251:
247:
243:
239:
235:
232:
228:
224:
220:
216:
213:; as well as
212:
208:
204:
200:
196:
192:
191:alkali basalt
184:
182:
180:
176:
173:
169:
165:
160:
157:
152:
147:
144:
140:
136:
132:
128:
120:
118:
116:
112:
108:
105:. During the
104:
100:
96:
95:alkali basalt
92:
88:
84:
80:
79:Pacific Ocean
76:
72:
63:
42:
30:
25:
20:
1728:
1724:
1693:(1): 72–83.
1690:
1686:
1649:
1645:
1604:
1600:
1567:
1563:
1554:
1550:
1517:
1513:
1483:(10): 1089.
1480:
1476:
1442:
1438:
1396:
1392:
1359:
1355:
1322:
1318:
1295:
1262:
1258:
1252:
1240:
1228:
1216:
1204:
1197:Pletnev 2021
1192:
1185:Pletnev 2021
1180:
1168:
1156:
1144:
1132:
1120:
1079:
1075:
1065:
1060:, p. 5.
1053:
1041:
1029:
1017:
1010:Pletnev 2019
1005:
978:
973:, p. 6.
915:
873:
861:
849:
842:Pletnev 2021
837:
830:Pletnev 2019
825:
818:Pletnev 2021
813:
808:, p. 5.
765:
761:
755:
722:
718:
689:, p. 4.
682:
649:
645:
639:
611:, p. 3.
581:, p. 4.
557:13 September
555:. Retrieved
551:
503:
497:
459:foraminifera
424:
364:
329:
285:ferrihydrite
258:
211:trachybasalt
188:
148:
124:
70:
69:
1520:(1): 1–12.
1265:(6): 1043.
475:sea urchins
447:cephalopods
415:Pleistocene
365:During the
334:and is now
313:phosphorite
248:sediments.
242:Pleistocene
185:Composition
143:Ita Mai Tai
135:Ita Mai Tai
1757:Categories
1601:Oceanology
1557:(1): 3–13.
1393:Oceanology
1082:(2): 199.
768:(3): 194.
725:(1): 693.
652:(5): 425.
529:References
518:Pako Guyot
463:gastropods
435:belemnites
427:Cretaceous
375:limestones
371:Cenomanian
305:todorokite
289:feroxyhyte
254:turbidites
234:limestones
223:sandstones
203:ankaramite
159:limestones
107:Cretaceous
89:, it is a
71:Ioah Guyot
22:Ioah Guyot
1745:0016-6995
1715:232042072
1707:1819-7159
1674:203654288
1666:1819-7159
1637:128475565
1629:0001-4370
1592:132364693
1584:1819-7140
1542:129963490
1534:0024-4902
1505:131213793
1467:0012-821X
1429:128414450
1421:0001-4370
1384:128543708
1347:0020-6814
1287:130123892
1279:0022-3360
1112:219638248
1104:1531-8354
790:128677808
782:1064-119X
747:128625849
674:129118428
666:0016-7029
443:bryozoans
431:ammonoids
407:Paleogene
387:Santonian
379:sediments
320:Spherules
309:Phosphate
207:phonolite
195:tholeiite
512:See also
496:such as
492:without
471:sea pens
455:crinoids
439:bivalves
429:include
297:hematite
293:goethite
281:feldspar
269:buserite
265:asbolane
227:basaltic
215:zeolites
199:hawaiite
175:seafloor
172:Jurassic
99:hawaiite
75:seamount
1725:Geobios
1609:Bibcode
1485:Bibcode
1447:Bibcode
1401:Bibcode
1364:Bibcode
1327:Bibcode
1310:Sources
1084:Bibcode
727:Bibcode
479:sponges
467:rudists
421:Biology
411:Miocene
348:hotspot
344:Miocene
336:extinct
326:History
273:calcite
261:apatite
246:pelagic
229:rocks.
219:Breccia
201:, plus
103:Miocene
77:in the
1743:
1713:
1705:
1672:
1664:
1635:
1627:
1590:
1582:
1540:
1532:
1503:
1465:
1427:
1419:
1382:
1345:
1285:
1277:
1110:
1102:
788:
780:
745:
672:
664:
490:corals
451:corals
399:Eocene
395:Eocene
367:Aptian
301:quartz
238:Eocene
156:reefal
1711:S2CID
1670:S2CID
1633:S2CID
1588:S2CID
1538:S2CID
1501:S2CID
1425:S2CID
1380:S2CID
1283:S2CID
1108:S2CID
786:S2CID
743:S2CID
670:S2CID
483:fauna
403:tuffs
170:over
115:guyot
111:reefs
73:is a
1741:ISSN
1703:ISSN
1662:ISSN
1625:ISSN
1580:ISSN
1530:ISSN
1463:ISSN
1417:ISSN
1343:ISSN
1275:ISSN
1100:ISSN
778:ISSN
662:ISSN
559:2018
502:and
477:and
409:and
383:reef
358:and
303:and
277:clay
250:Clay
231:Reef
221:and
209:and
197:and
97:and
54:Ioah
1733:doi
1695:doi
1654:doi
1617:doi
1572:doi
1522:doi
1493:doi
1455:doi
1443:163
1409:doi
1372:doi
1335:doi
1267:doi
1092:doi
1080:491
770:doi
735:doi
723:409
654:doi
473:,
389:to
316:ore
244:by
141:".
133:to
1759::
1739:.
1729:45
1727:.
1709:.
1701:.
1691:15
1689:.
1685:.
1668:.
1660:.
1650:13
1648:.
1631:.
1623:.
1615:.
1605:50
1603:.
1586:.
1578:.
1568:10
1566:.
1555:25
1536:.
1528:.
1518:51
1516:.
1499:.
1491:.
1479:.
1461:.
1453:.
1441:.
1423:.
1415:.
1407:.
1397:46
1395:.
1378:.
1370:.
1360:27
1358:.
1341:.
1333:.
1323:29
1321:.
1281:.
1273:.
1263:85
1261:.
1106:.
1098:.
1090:.
1078:.
1074:.
990:^
959:^
944:^
927:^
900:^
885:^
798:^
784:.
776:.
766:32
764:.
741:.
733:.
721:.
709:^
694:^
668:.
660:.
650:48
648:.
616:^
601:^
586:^
567:^
550:.
537:^
469:,
465:,
461:,
457:,
453:,
449:,
445:,
441:,
437:,
433:,
401:,
373:,
354:,
299:,
295:,
291:,
287:,
283:,
279:,
275:,
271:,
267:,
263:,
205:,
193:,
181:.
117:.
109:,
1747:.
1735::
1717:.
1697::
1676:.
1656::
1639:.
1619::
1611::
1594:.
1574::
1544:.
1524::
1507:.
1495::
1487::
1481:4
1469:.
1457::
1449::
1431:.
1411::
1403::
1386:.
1374::
1366::
1349:.
1337::
1329::
1289:.
1269::
1114:.
1094::
1086::
792:.
772::
749:.
737::
729::
676:.
656::
561:.
413:-
369:-
240:-
Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.
