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459:. East of the Tarava Seamounts lie the Va'a Tau Piti seamounts, which were sometimes considered part of the Tarava Seamounts but are considered geologically separate owing to their different configuration (east-west rather than northwest-southeast), which may reflect an origin close to the
817:
anomalies, considering that there is a discontinuity in the chain which would have formed about 43 million years ago at the time of a major change in the motion of the
Pacific Plate. The hotspot in question may be the
537:
The Tarava
Seamounts consist of eighteen separate edifices which extend across six longitudes and four latitudes over a length of 700 kilometres (430 mi), 200 kilometres (120 mi) away from the
546:
which reach depths of 580 metres (1,900 ft) below sea level, the Tarava
Seamounts consist of 4,000–4,500 metres (13,100–14,800 ft) high cones. Among the named edifices are Arere (‘Arere,
1794:
Sedov, A. P.; Kazakevich, G. I.; Matveenkov, V. V.; Volokitina, L. P.; Luk’yanov, S. V.; Rashidov, V. A. (2008-08-01). "Mechanism of the formation of volcanic chains of French
Polynesia".
809:: Fafa Piti has yielded ages of 43.5 ± 0.6 million years ago and Punu Taipu of 36.1 ± 0.5 million years ago. Such ages are consistent with an age progressive volcanism caused by a
1502:"Genus Profundiconus Kuroda, 1956 (Gastropoda, Conoidea): Morphological and molecular studies, with the description of five new species from the Solomon Islands and New Caledonia"
1441:
Ho, H.-C.; Séret, B.; Shao, K.-T. (2011-12-01). "Records of anglerfishes (Lophiiformes: Lophiidae) from the western South
Pacific Ocean, with descriptions of two new species".
838:
Deep-sea animals such as these living on the Tarava
Seamounts and their slopes have drawn attention, since they are poorly researched and possibly under threat from
1706:
Clouard, Valérie; Bonneville, Alain; Gillot, Pierre-Yves (2003). "The Tarava
Seamounts: a newly characterized hotspot chain on the South Pacific Superswell".
1593:"Pectinoidea (Bivalvia: Propeamussiidae, Entoliidae and Pectinidae) from the Tarava Seamounts, Society Islands and the Tuamotu Archipelago (French Polynesia)"
1640:"Deep-water Rissoidae of the genera Benthonella Dall, 1889 and Benthonellania Lozouet, 1990 (Gastropoda, Caenogastropoda, Rissooidea) from French Polynesia"
1361:
910:
482:
The South
Pacific Superswell is a large structure in the southern Pacific Ocean, where there are many volcanoes and the seafloor is unusually shallow.
239:
1889:
1874:
1869:
1408:
1277:
475:, but a number of such chains appear to correspond to short lasting volcanism, such as processes triggered by tension in the
766:
580:
549:
1735:
Delavenne, Juliette; Keszler, Louise; Castelin, Magalie; Lozouet, Pierre; Maestrati, Philippe; Samadi, Sarah (6 May 2019).
642:
1879:
704:
673:
611:
276:
735:
499:
1737:"Deep-sea benthic communities in the largest oceanic desert are structured by the presence of polymetallic crust"
283:
1884:
883:
893:
455:
The Tarava
Seamounts are also known as the Savannah Seamounts and were discovered during the 1996 ZEPOLYF1
874:
806:
456:
320:
852:
40:
526:
33:
830:
may have induced tectonic stress that propagated towards the location of the future Tarava
Seamounts.
1803:
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864:
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1388:
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1134:
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1071:
1050:
332:
269:
847:
1827:
1685:
Beu, Alan; Bouchet, Philippe; Jean, Tröndlé (2012). "Tonnoidean gastropods of French Polynesia".
1620:
1541:, a new genus and species of deep-sea spider crab from the western Pacific, and a new species of
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1545:
A. Milne-Edwards, 1875, from Papua New Guinea (Crustacea: Brachyura: Majoidea: Epialtidae)".
1301:
Fontaine, Fabrice R.; Barruol, Guilhem; Tommasi, Andréa; Bokelmann, Götz H. R. (2007-09-01).
1811:
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325:
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Deep water Pyramidelloidea from the Central and south Pacific. The Tibe Chrysallidini.
1727:
850:
crusts. Several new species have been discovered on the Tarava Seamounts, such as the
1863:
1831:
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1327:
1302:
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1226:
483:
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snails have been described from the Tarava Seamounts. Other species found there are
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ECIMAT (Estación de Ciencias Mariñas de Toralla) - Universidade de Vigo, 412 pp
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Linear chains of volcanoes in the Pacific have been attributed to deep
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1303:"Upper-mantle flow beneath French Polynesia from shear wave splitting"
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or a now extinct third hotspot. Alternatively, the formation of the
1232:
1025:
1362:
Plate velocities in hotspot reference frame: electronic supplement
543:
432:
1638:
Amati, Bruno; Giulio, Andrea Di; Oliverio, Marco (28 June 2022).
846:. The Tarava Seamounts are considered potential mining sites for
1374:
974:
1849:, description of some species found on the Tarava seamounts.
1537:
NG, PETER K.L.; FORGES, BERTRAND RICHER DE (2013-10-07). "
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Dijkstra, Henk H.; Maestrati, Philippe (2013-09-01).
1500:
Tenorio, Manuel J.; Castelin, Magalie (2016-01-29).
813:, whose volcano-building activity was influenced by
443:age, they may have formed under the influence of a
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21:
805:age. Only two seamounts have been dated, both by
486:processes may be responsible for its existence.
1360:Morgan, W. Jason; Morgan, Jason Phipps (2007).
1262:Special Paper 388: Plates, plumes and paradigms
1668:
1013:
8:
1260:Clouard, Valérie; Bonneville, Alain (2005).
1114:"Marine Gazetteer Place details:'Ori'o Mata"
1387:Andréfouët, Serge; Adjeroud, Mehdi (2019),
1177:"Marine Gazetteer Place details:Punu Taipu"
1072:"Marine Gazetteer Place details:Fafa Piti"
435:and a number of cone-shaped seamounts. Of
18:
1776:
1513:
1336:
1326:
1156:"Marine Gazetteer Place details:Otu'eroa"
897:together with five other pectinoids, and
1393:World Seas: an Environmental Evaluation
929:
906:
1198:"Marine Gazetteer Place details:Ua'ao"
1135:"Marine Gazetteer Place details:Otaha"
1051:"Marine Gazetteer Place details:Arere"
797:The seamounts are considered to be of
1248:Clouard, Bonneville & Gillot 2003
1218:Clouard, Bonneville & Gillot 2003
1093:"Marine Gazetteer Place details:Honu"
1038:Clouard, Bonneville & Gillot 2003
1002:Clouard, Bonneville & Gillot 2003
990:Clouard, Bonneville & Gillot 2003
963:Clouard, Bonneville & Gillot 2003
942:Clouard, Bonneville & Gillot 2003
16:Seamount chain in South Pacific ocean
7:
1708:Earth and Planetary Science Letters
639:), Orio'Mata (‘Ori‘o Mata Seamount
1401:10.1016/b978-0-08-100853-9.00039-7
14:
1847:The context of the TARASOC cruise
1307:Geophysical Journal International
1264:. Vol. 388. pp. 71–90.
1463:10.1111/j.1095-8649.2011.03106.x
1328:10.1111/j.1365-246x.2007.03475.x
909:
701:), Otu'eroa (‘Otu‘eroa Seamount
238:
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46:
39:
32:
1890:Seamounts of the Pacific Ocean
1852:Peñas A. & Rolán E., 2017
1:
1875:Hotspots of the Pacific Ocean
1728:10.1016/s0012-821x(02)01143-3
1870:Geology of the Pacific Ocean
1669:Beu, Bouchet & Jean 2012
1656:10.5252/zoosystema2022v44a12
1506:European Journal of Taxonomy
1014:Beu, Bouchet & Jean 2012
670:), Otaha ( ‘Otaha Seamount
527:GPX (secondary coordinates)
1911:
1761:10.1038/s41598-019-43325-0
431:. They are formed by five
1816:10.1134/S0001437008040127
1559:10.11646/zootaxa.3718.4.5
1395:, Elsevier, p. 845,
1364:(Report). pp. 73–74.
919:(holotype in MNHN, Paris)
522:GPX (primary coordinates)
497:Map all coordinates using
26:
1270:10.1130/0-8137-2388-4.71
917:Parvamussium vesiculosum
884:Parvamussium vesiculosum
782:18.916667°S 151.838333°W
596:18.961667°S 154.096667°W
565:16.808333°S 155.193333°W
542:. Aside from five large
505:Download coordinates as:
1720:2003E&PSL.207..117C
1443:Journal of Fish Biology
787:-18.916667; -151.838333
601:-18.961667; -154.096667
570:-16.808333; -155.193333
807:potassium-argon dating
1375:Delavenne et al. 2019
975:Delavenne et al. 2019
894:Propeamussium watsoni
732:), Punu Taipu Guyot (
658:17.813333°S 154.075°W
517:GPX (all coordinates)
451:Geography and geology
1539:Samadinia longispina
1515:10.5852/ejt.2016.173
887:. Numerous deep-sea
875:Samadinia longispina
865:Profundiconus tarava
720:18.22°S 152.748333°W
689:18.758333°S 152.24°W
663:-17.813333; -154.075
627:18.376667°S 154.09°W
457:oceanographic cruise
1880:Oligocene volcanism
1808:2008Ocgy...48..578S
1753:2019NatSR...9.6977D
1455:2011JFBio..79.1722H
1319:2007GeoJI.170.1262F
778: /
747: /
725:-18.22; -152.748333
716: /
694:-18.758333; -152.24
685: /
654: /
632:-18.376667; -154.09
623: /
592: /
561: /
427:, southwest of the
295: /
270:South Pacific Ocean
1741:Scientific Reports
1699:10.11646/mr.32.2.1
1687:Molluscan Research
1389:"French Polynesia"
1040:, p. 121,122.
853:Lophiodes iwamotoi
820:Foundation hotspot
222:Orio'Mata Seamount
162:Fafa Piti Seamount
1609:10.5252/z2013n3a2
1410:978-0-08-100853-9
1279:978-0-8137-2388-4
1233:Sedov et al. 2008
1026:Sedov et al. 2008
751:19.275°S 150.98°W
461:East Pacific Rise
410:
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210:Otu'eroa Seamount
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1841:External links
1839:
1837:
1836:
1802:(4): 578–587.
1791:
1732:
1703:
1681:
1679:
1676:
1674:
1673:
1671:, p. 108.
1661:
1630:
1603:(3): 361–375.
1580:
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1449:(7): 1722–45.
1433:
1409:
1379:
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1250:, p. 128.
1237:
1235:, p. 584.
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1220:, p. 120.
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1028:, p. 579.
1018:
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1004:, p. 117.
994:
992:, p. 121.
979:
967:
965:, p. 119.
946:
944:, p. 118.
928:
926:
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840:climate change
835:
832:
577:), Fafa Piti (
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484:Asthenospheric
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186:Otaha Seamount
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174:Ua'ao Seamount
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1696:
1693:(2): 61–120.
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1598:
1594:
1587:
1585:
1581:
1576:
1572:
1568:
1564:
1560:
1556:
1553:(4): 357–66.
1552:
1548:
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1521:
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1016:, p. 63.
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500:OpenStreetMap
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477:Pacific Plate
474:
473:mantle plumes
466:
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450:
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425:Pacific Ocean
422:
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198:Honu Seamount
138:
42:
35:
25:
20:
1853:
1799:
1795:
1744:
1740:
1711:
1707:
1690:
1686:
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1538:
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1505:
1495:
1446:
1442:
1436:
1429:ResearchGate
1427:– via
1422:, retrieved
1392:
1382:
1377:, p. 9.
1370:
1355:
1310:
1306:
1296:
1261:
1255:
1213:
1201:. Retrieved
1192:
1180:. Retrieved
1171:
1159:. Retrieved
1150:
1138:. Retrieved
1129:
1117:. Retrieved
1108:
1096:. Retrieved
1087:
1075:. Retrieved
1066:
1054:. Retrieved
1045:
1033:
1021:
1009:
997:
977:, p. 4.
970:
916:
892:
882:
873:
863:
851:
848:polymetallic
837:
815:lithospheric
796:
536:
504:
503:
496:
481:
470:
454:
416:
414:
411:
299:18.3°S 153°W
1747:(1): 6977.
1508:(173): 15.
1313:(3): 1283.
785: /
773:151°50′18″W
754: /
742:150°58′48″W
723: /
711:152°44′54″W
692: /
680:152°14′24″W
661: /
649:154°04′30″W
630: /
618:154°05′24″W
599: /
587:154°05′48″W
568: /
556:155°11′36″W
333:Age of rock
304:-18.3; -153
302: /
277:Coordinates
1864:Categories
1796:Oceanology
1644:Zoosystema
1597:Zoosystema
1424:2021-10-19
1338:1885/34185
925:References
902:gastropods
899:tonnoidean
861:cone snail
857:anglerfish
770:18°55′00″S
739:19°16′30″S
708:18°13′12″S
677:18°45′30″S
646:17°48′48″S
615:18°22′36″S
584:18°57′42″S
553:16°48′30″S
1832:140187208
1824:0001-4370
1769:2045-2322
1617:1280-9551
1567:1175-5334
1524:2118-9773
1471:1095-8649
1419:263724857
1347:0956-540X
1288:133484558
889:rissoidae
880:pectinoid
803:Oligocene
608:), Honu (
441:Oligocene
421:seamounts
1787:31061398
1625:85597202
1575:26258232
1543:Rochinia
1479:22141884
1203:21 March
1182:21 March
1161:21 March
1140:21 March
1119:21 March
1098:21 March
1077:21 March
1056:21 March
467:Regional
290:153°00′W
266:Location
261:Location
56:124miles
1804:Bibcode
1778:6502874
1749:Bibcode
1716:Bibcode
1678:Sources
1547:Zootaxa
1451:Bibcode
1315:Bibcode
834:Biology
811:hotspot
445:hotspot
315:Geology
287:18°18′S
137:Papeete
1895:Guyots
1830:
1822:
1785:
1775:
1767:
1650:(12).
1623:
1615:
1573:
1565:
1522:
1487:916582
1485:
1477:
1469:
1417:
1407:
1345:
1286:
1276:
870:majoid
868:, the
859:, the
822:, the
799:Eocene
544:guyots
437:Eocene
433:guyots
1828:S2CID
1621:S2CID
1483:S2CID
1415:S2CID
1284:S2CID
872:crab
490:Local
54:200km
1820:ISSN
1783:PMID
1765:ISSN
1613:ISSN
1571:PMID
1563:ISSN
1551:3718
1520:ISSN
1475:PMID
1467:ISSN
1405:ISBN
1343:ISSN
1274:ISBN
1205:2024
1184:2024
1163:2024
1142:2024
1121:2024
1100:2024
1079:2024
1058:2024
878:and
842:and
415:The
347:PreꞒ
321:Type
1812:doi
1773:PMC
1757:doi
1724:doi
1712:207
1695:doi
1652:doi
1605:doi
1555:doi
1510:doi
1459:doi
1397:doi
1333:hdl
1323:doi
1311:170
1266:doi
512:KML
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397:Pg
341:Ma
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402:N
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387:J
382:T
377:P
372:C
367:D
362:S
357:O
352:Ꞓ
131:s
126:t
121:n
116:u
111:o
106:m
101:a
96:e
91:S
86:a
81:v
76:a
71:r
66:a
61:T
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