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Evolution of cephalopods

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existing septa? The prevailing argument suggests that a strand of tissue remained attached to the previous septum as the mollusc moved forwards and deposited its next septum, producing an obstacle to the complete closure of the septum and becoming mineralised itself. 10 or more septa are found in mature individuals, occupying around a third of the shell – septa form very early and have been found in specimens as small as 2 mm in length. Septa are uniformly spaced, which is inconsistent with a gastropod affinity. Unlike monoplacophoran fossils, there is no evidence of muscle scarring in
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them to recolonise shallow waters. The loss of the shell may also have resulted from evolutionary pressure to increase manoeuvrability, resulting in a more fish-like habit. This pressure may have increased as a result of the increased complexity of fish in the late Palaeozoic, increasing the competitive pressure. Internal shells still exist in many non-shelled living cephalopod groups but most truly shelled cephalopods, such as the ammonites, became extinct at the end of the
4226: 4236: 247: 175:, none of the 30+ Cambrian cephalopod genera are known to have survived into the Ordovician. Cambrian cephalopods differ from their descendants by account of their small size (a few centimetres in length); long, tapering shells; smooth shell surfaces; closely spaced septa; and lack of deposits in their body chamber; several more specific features are also only seen in certain groups of Cambrian cephalopod. 581:, a Silurian–Triassic group of orthocones, are paraphyletic to the coleoids and ammonoids – that is, the latter groups arose from within the Bactritida. An increase in the diversity of the coleoids and ammonoids is observed around the start of the Devonian period, and corresponds with a profound increase in fish diversity. This could represent the origin of the two derived groups. 565: 328:, which were quite small; their shells were slightly curved, and the internal chambers were closely spaced. The siphuncle penetrated the septa with meniscus-like holes. This marks an important difference from the earlier cephalopods, whose siphuncle was at the edge of the septum and against the shell wall. On the basis of muscle scars preserved in such genera as 625:, which had ten arms, but the status of its shell is ambiguous as it has not been extracted from the concretion that preserves the only fossil. Accordingly, it has been interpreted as both an internal and an external shell; the specimen may represent a 'squid' or a belemnoid, although due to preservation its affinities are not known well. 588:
species. It is thought that competitive pressure from fish forced the shelled forms into deeper water, which provided an evolutionary pressure towards shell loss and gave rise to the modern coleoids, a change which led to greater metabolic costs associated with the loss of buoyancy, but which allowed
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as well as cephalopods – a siphuncle is essential to ally a fossil shell conclusively to the cephalopoda. Chambered gastropods can be distinguished from cephalopod shells by the absence of a siphuncle, the irregular spacing of septa, the layering of the shell and (in younger or unmetamorphosed rocks)
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The preservation of cephalopod soft parts is not entirely unusual; soft-bodied fossils, especially of coeloids (squid), are relatively widespread in the Jurassic, but phosphatized remains are unknown before this period. On the other hand, soft parts – including a possible ink sac – are
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and they considered that animal as early form of cephalopod. Unlike other early cephalopods, it did not have a shell and appeared to possess jet propulsion in the manner of "derived" cephalopods, complicated the question of the order in which cephalopod features developed. Due to its morphology is
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Understanding of early cephalopod origins is by necessity biased by the available fossil material, which on the whole consists of shelly fossils. Critical fossils are detailed below; since their stratigraphic age has guided the interpretation of the fossils, they are listed in descending order of
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and some coeloids, appeared to be able to propel themselves forwards by directing their jet backwards. Because they had an external shell, they would not have been able to generate their jets by contracting their mantle, so must have used alternate methods, such as by contracting their funnels or
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The ancestors of coleoids (including most modern cephalopods) and the ancestors of the modern nautilus, had diverged by the Floian Age of the Early Ordovician Period, over 470 million years ago. We know this because the orthocerids were the first known representatives of the neocephalopoda, were
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both emerged during the Darriwilian. The direction of coiling would prove to be crucial to the future success of the lineages; endogastric coiling would only permit large size to be attained with a straight shell, whereas exogastric coiling – initially rather rare – permitted the spirals familiar
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of larger animals, and the earliest accepted cephalopods date to the Middle Cambrian Period. During the Cambrian, cephalopods are most common in shallow near-shore environments, but they have been found in deeper waters too. Cephalopods were thought to have "undoubtedly" arisen from within the
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is the latest septate mollusc before the first sipunculate cephalopods – a point that has been taken to prove its relevance to the Cephalopoda. The absence of this siphuncle has been taken as evidence against cephalopod ancestry – how, it is argued, could a siphuncle evolve to penetrate
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also appear during this time; they are restricted to shallow water and have short exogastric conchs. The mid Ordovician saw the first cephalopods with septa strong enough to cope with the pressures associated with deeper water, and could inhabit depths greater than 100–200 m. The
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Early cephalopods were likely predators, near the top of the food chain. In the Early Palaeozoic, their range was far more restricted than today: They were mainly constrained to sub-littoral regions of shallow shelves of the low latitudes, and usually occur in association with
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Sumner-Rooney, Lauren H.; Schrödl, Michael; Lodde-Bensch, Eva; Lindberg, David R.; Heß, Martin; Brennan, Gerard P.; Sigwart, Julia D. (2015). "A neurophylogenetic approach provides new insight to the evolution of Scaphopoda: A neurophylogenetic approach in Scaphopoda".
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Curved shells brought a number of benefits. Firstly, minerals are not required in as large quantities, as each successive whorl builds on the one before. Also, the organism is more stable (its centre of mass coincides with its centre of buoyancy) and more manoeuvrable.
340:, these animals are reconstructed with a straight body and dorsal shell, with the head at the anterior, concave surface of the shell, and the funnel (consisting of a pair of folds in the foot at the rear), not juxtaposed with the head as in later, oncocerid-like forms. 352:
Early cephalopods had fine shells that could not cope with the pressures of deep water. In the mid Tremadoc, these were supplemented by larger shells around 20 cm in length; these larger forms included straight and coiled shells, and fall into the orders
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would have allowed the shells of these early forms to become gas-filled (thus buoyant) in order to support them and keep the shells upright while the animal crawled along the floor, and separated the true cephalopods from putative ancestors such as
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The tentacles of the ancestral cephalopod developed from the mollusc's foot; the ancestral state is thought to have had five pairs of tentacles which surrounded the mouth. Smell-detecting organs evolved very early in the cephalopod lineage.
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with a snorkel-like tube on one surface. The snorkel has been seized upon as characteristic of a cephalopod-like water circulatory system, or perhaps as a precursor to the siphuncle. However, neither of these theories have been borne out.
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The Ellesmerocerids were the only shelled cephalopods known to have survived the end-Cambrian extinction; all subsequent cephalopods are thus thought to be derived from these forms, which diversified throughout the Ordovician period.
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has been interpreted as the earliest fossil coleoid, and its shell may be in a partly internalized state. Belemnoids proper appear slightly later in the Early Devonian, and represent the first unambiguous coleoids.
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stage. None of the fossils are complete, and none show the tip or opening of the shell. Approximately half of its shell was filled with septa; 7 were recorded in a 2 cm shell. Its shell contains transverse
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its microstructure, and the relatively thick width of the shell. The earliest such shells do not have the muscle scars which would be expected if they truly had a monoplacophoran affinity.
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Klug, Christian; Stevens, Kevin; Hoffmann, René; Zatoń, Michał; Clements, Thomas; Košťák, Martin; Weis, Robert; De Baets, Kenneth; Lehmann, Jens; Vinther, Jakob; Fuchs, Dirk (2023-12-07).
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Shigeno, S.; Sasaki, T.; Moritaki, T.; Kasugai, T.; Vecchione, M.; Agata, K. (2008). "Evolution of the cephalopod head complex by assembly of multiple molluscan body parts: Evidence from
197:. Its position in this group is suggested based on its shape and the presence of chambers. Under this hypothesis, it would be a precursor to the hypseloconids and then genera such as 1907:
Pohle, Alexander; Kröger, Björn; Warnock, Rachel C. M.; King, Andy H.; Evans, David H.; Aubrechtová, Martina; Cichowolski, Marcela; Fang, Xiang; Klug, Christian (December 2022).
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Yochelson, Ellis L.; Flower, Rousseau H.; Webers, Gerald F. (1973). "The bearing of the new Late Cambrian monoplacophoran genus Knightoconus upon the origin of the Cephalopoda".
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Unlike most modern cephalopods, most ancient varieties had protective shells. These shells at first were conical but later developed into curved nautiloid shapes seen in modern
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means the shell is curved so as the ventral side is longitudinally convex (belly out). Exogastric coiling allows the funnel to be pointed backwards, beneath the shell.
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Because the characters differentiating monoplacophora from cephalopods are few, several monoplacophora have been mistaken for cephalopod ancestors. One such genus is
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A number of fossils have historically been considered to represent components of the cephalopods' history, but been reinterpreted on the basis of additional material.
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has originally been interpreted as a cirrate octopus. But later study shows that affinities as octopus is controversial, and even considered to be a non-mollusk.
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Etches, S.; Clarke, J.; Callomon, J. (2009). "Ammonite eggs and ammonitellae from the Kimmeridge Clay Formation (Upper Jurassic) of Dorset, England".
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Kröger, B.R.; Vinther, J.; Fuchs, D. (2011). "Cephalopod origin and evolution: A congruent picture emerging from fossils, development and molecules".
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This specimen from Early Cambrian was originally proposed as the earliest cephalopod shell. However, later study found that specimen is actually a
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Klug, Christian; Landman, Neil H.; Fuchs, Dirk; Mapes, Royal H.; Pohle, Alexander; Guériau, Pierre; Reguer, Solenn; Hoffmann, René (2019-07-31).
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An ammonitic ammonoid with the body chamber missing, showing the septal surface (especially at right) with its undulating lobes and saddles.
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but otherwise basal to all other major mollusc classes. The internal phylogeny of Mollusca, however, is wide open to interpretation – see
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Young, R. E.; Vecchione, M.; Donovan, D. T. (1998). "The evolution of coleoid cephalopods and their present biodiversity and ecology".
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are a group of shells that, whilst originally aligned to the monoplacophoran ancestry of the cephalopods, have been reinterpreted as
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on its concave side. Its morphology matches closely to that hypothesised for the last common ancestor of all cephalopods, and the
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and eventually jet propulsion in more derived cephalopods. However, because chambered shells are found in a range of molluscs –
3017: 502:, which was reclassified based on a depressed groove that forms a band around the shell, which is similar to a feature seen in 3974: 3734: 1553: 1146: 927: 109:, which lacked a siphuncle. Negative buoyancy (i.e. the ability to float) would have come later, followed by swimming in the 2799:
Briggs, D.E.G.; Kear, A.J.; Martill, D.M.; Wilby, P.R. (1993). "Phosphatization of soft-tissue in experiments and fossils".
2480:"Early growth-stages and classification of orthoceridan Cephalopods of the Darriwillian (Middle Ordovician) of Baltoscandia" 3331: 482:(silica); neither was it septate. This illusion was a result of the laminated texture of the organisms' tests. Therefore, 190:
is the oldest fossil to have been assigned to the cephalopods, dating from the Early Cambrian (Atdababian and Botomian), ~
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Giribet, G.; Okusu, A, A.; Lindgren, A.R., A. R.; Huff, S.W., S. W.; Schrödl, M, M.; Nishiguchi, M.K., M. K. (May 2006).
3719: 3379: 945:"Evidence for a clade composed of molluscs with serially repeated structures: monoplacophorans are related to chitons" 4739: 2569: 3786: 4265: 3791: 3389: 2280:"Fossil coleoid cephalopod from the Mississippian Bear Gulch Lagerstätte sheds light on early vampyropod evolution" 4036: 4026: 3950: 3225: 1739:
Smith, M.R. (2013). "Nectocaridid ecology, diversity and affinity: Early origin of a cephalopod-like body plan".
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which contains modern octopuses and vampire squids, although it is later considered to be synonymous with
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Webers, G.F.; Yochelson, E.L. (1989). Crame, J.A. (ed.). "Origins and Evolution of the Antarctic Biota".
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strongly dissimilar to confirmed early cephalopods, and thus their affinities to cephalopods and even to
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have been interpreted as cephalopod ancestors, but hyoliths proper are now recognized as brachiopods.
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thought to represent an ancestor to the cephalopods. It had a chambered, conical shell, but lacked a
3858: 2844:"A new cephalopod with soft parts from the Upper Carboniferous Francis Creek Shale of Illinois, USA" 4152: 4016: 3988: 3963: 3920: 3823: 3756: 3631: 3504: 3472: 3435: 2163:. SEPM Book. Vol. 93. Society for Sedimentary Geology (SEPM). pp. 135–150. Archived from 1966:
Hildenbrand, Anne; Austermann, Gregor; Fuchs, Dirk; Bengtson, Peter; Stinnesbeck, Wolfgang (2021).
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The class developed during the middle Cambrian, and underwent pulses of diversification during the
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means the shell is curved so as the ventral or lower side is longitudinally concave (belly in);
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clade. However genetic studies suggest that they are more basal, forming a sister group to the
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Kröger, B.; Yun-bai, Y. B. (2009). "Pulsed cephalopod diversification during the Ordovician".
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Sketch of the soft-part anatomy of early ellesmeroceridans, as reconstructed by Kröger (2007).
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Wells, M.J.; O'Dor, R.K. (July 1991). "Jet Propulsion and the Evolution of the Cephalopods".
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Ordovician orthocone nautiloids are the first for which trace fossil evidence is available.
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were once interpreted as early cephalopods, but today these tiny fossils are recognized as
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from the fossil record to develop, with their corresponding large size and diversity.
922:. Vol. 12: Palaeontology and Neontology of Cephalopods. Orlando, Fla.: Acad. Pr. 4235: 4189: 3915: 3863: 3641: 3457: 3358: 3321: 3316: 3272: 3267: 3220: 3186: 2944: 2902: 2828: 2732: 2688: 2670: 2623: 2605: 2565: 2452: 2325: 2307: 2085: 2054: 2036: 1997: 1948: 1930: 1881: 1846: 1807: 1725: 1682: 1674: 1617: 1549: 1501: 1414: 1367: 1332: 1290: 1209: 1168: 1142: 1020: 984: 923: 895: 2744: 2371: 1768: 1032: 686: 4374: 3781: 3348: 3326: 3134: 2936: 2898: 2863: 2816: 2724: 2678: 2662: 2613: 2597: 2535: 2499: 2464: 2444: 2402: 2359: 2315: 2299: 2253: 2132: 2044: 2028: 1987: 1979: 1938: 1920: 1893: 1873: 1842: 1803: 1756: 1721: 1664: 1656: 1607: 1597: 1541: 1489: 1449: 1406: 1379: 1359: 1324: 1278: 1204: 1134: 1012: 974: 964: 918:
Clarke, M.R.; Trueman, E.R., eds. (1988). "Main features of cephalopod evolution".
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has large internal conch which looks similar to external shell that can be seen in
147: 3626: 2234:"Pohlsepia Mazonensis, an Early 'Octopus' from the Carboniferous of Illinois, USA" 1282: 1047: 4616: 4599: 4522: 4142: 3766: 3593: 3582: 3536: 3479: 3428: 3208: 3012: 2406: 1602: 1535: 866:
Landing, Ed; Kröger, Björn (2009). "The Oldest Cephalopods from East Laurentia".
813: 479: 325: 300: 284: 220: 114: 110: 85: 65: 2385:
Landing, E.; Kröger, B. (2012). "Cephalopod ancestry and ecology of the hyolith
1968:"A potential cephalopod from the early Cambrian of eastern Newfoundland, Canada" 1576:
Kröger, B.R.; Servais, T.; Zhang, Y.; Kosnik, M. (2009). Kosnik, Matthew (ed.).
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Proceedings of the National Academy of Sciences of the United States of America
652: 647: 645:, and this genus probably shows how external shell become into internal conch. 330: 288: 258: 94: 88:-like ancestor with a curved, tapering shell, and to be closely related to the 2601: 2503: 2150:
Hagadorn, J.W.; Waggoner, B.M. (2002). "The Early Cambrian problematic fossil
1909:"Early cephalopod evolution clarified through Bayesian phylogenetic inference" 1545: 1138: 478:’s small, conical shell was not secreted but built from grains of the mineral 316: 4733: 4387: 4380: 4184: 4062: 4021: 3867: 3621: 3289: 3284: 2948: 2820: 2674: 2609: 2345:"Brachiopod identity of the alleged monoplacophoran ancestors of cephalopods" 2311: 2089: 2040: 1934: 1678: 1493: 1418: 1336: 433:
was previously described from poorly preserved specimen and considered as an
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Lipps, J.H.; Sylvester, A.G. (1 March 1968). "The enigmatic Cambrian fossil
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Stinchcomb, B. L. (1980). "New Information on Late Cambrian Monoplacophora
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Landing, Ed; Kröger, Björn; Westrop, Stephen R.; Geyer, Gerd (2023-01-12).
2001: 1952: 1885: 1877: 1686: 1621: 1371: 1363: 1024: 988: 537: 504: 498: 474:
was a cephalopod. However discoveries of more detailed fossils showed that
470: 395: 358: 304: 266:, dating to the Upper Cambrian. Its 14 known specimens hail from the basal 212: 130: 105: 2760:"Decay and fossilization of non-mineralized tissue in coleoid cephalopods" 4626: 4590: 4482: 4468: 4450: 4350: 4206: 4077: 3806: 3341: 3171: 3077: 3035: 2421: 2363: 1410: 577:
and coleoids, and had appeared by the Floian. It is widely held that the
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have given rise to the "snorkel hypothesis". These fossils are aseptate
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Recognition of invertebrate fossil fragments in rocks and thin sections
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When it was discovered in 1888, it was thought that the early Cambrian
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to some gastropods was used to support this view. The development of a
69: 35: 20: 1669: 1578:"The Origin and Initial Rise of Pelagic Cephalopods in the Ordovician" 1472:
Holland, C.H. (1987). "The nautiloid cephalopods: A strange success".
1016: 887: 4717: 4571: 4549: 4436: 4343: 4201: 4052: 3661: 3279: 3027: 621: 519: 508:. The septa in this genus are either closely or irregularly spaced. 434: 373: 280: 224: 192: 186: 143: 118: 99: 89: 39: 24: 1265:. Late Cambrian molluscan faunas and the origin of the Cephalopoda. 4553: 4330: 4293: 4104: 3306: 2586:"Anatomy and evolution of the first Coleoidea in the Carboniferous" 2157:
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2154:: New insights from the Basin and Range". In Corsetti, F.A. (ed.). 616: 585: 574: 443: 369: 217: 139: 57: 52: 43: 28: 2419: 1965: 1760: 4566: 4394: 3489: 3203: 246: 437:. In 2010, Martin Smith and Jean-Bernard described specimens of 2559: 16:
Origin and diversification of cephalopods through geologic time
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Boyle, Peter; Rodhouse, Paul (2005). "Origin and Evolution".
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Wilbur, Karl M.; Trueman, E.R.; Clarke, M.R., eds. (1985),
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10.1130/0091-7613(1993)021<0805:LCFVTW>2.3.CO;2
564: 414:, enigmatic animal that is misidentified as stem-cephalopod 2919:
Chen, J. Y.; Teichert, C. (1983). "Cambrian cephalopods".
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Kröger, Björn; Vinther, Jakob; Fuchs, Dirk (August 2011).
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Chen, J.Y.; Teichert, C. (1983). "Cambrian cephalopods".
917: 92:(snails). The similarity of the early shelled cephalopod 84:
The cephalopods were once thought to have evolved from a
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Signor, P.W.; Ryan, D.A. (1993). "Lower Cambrian fossil
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Whalen, Christopher D.; Landman, Neil H. (2022-03-08).
227:. Although earlier molluscan fossils are also septate, 2798: 1906: 2941:
10.1130/0091-7613(1983)11<647:CC>2.0.CO;2
2583: 2525: 2384: 1637:"Primitive soft-bodied cephalopods from the Cambrian" 1431: 1329:
10.1130/0091-7613(1983)11<647:CC>2.0.CO;2
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By the mid Ordovician these orders are joined by the
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The earliest true cephalopod order to emerge was the
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Smith, Martin R.; Caron, Jean-Bernard (2010-05-01).
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Association of Australasian Palaeontologists Memoirs
368:, whose first chambers are small and spherical, and 2227: 2225: 2223: 827:Begtson, Stefan (1970). "The Lower Cambrian fossil 401: 2758:Kear, A.J.; Briggs, D.E.G.; Donovan, D.T. (1995). 2115:: The whole truth or just a piece of the beast?". 1859: 1349: 1263:Geological Society of London, Special Publications 635:contains some important genera of early coleoids. 2757: 2391:Palaeogeography, Palaeoclimatology, Palaeoecology 2231: 2187: 2185: 865: 794:Palaeogeography, Palaeoclimatology, Palaeoecology 711: 709: 4731: 2220: 2149: 1087: 1085: 1083: 2420:Moysiuk, J.; Smith, M.R.; Caron, J.-B. (2017). 1260: 826: 23:have a long geological history, with the first 2706: 2704: 2702: 2389:s.l. in the Cambrian evolutionary radiation". 2182: 2071: 1571: 1569: 1567: 1565: 1467: 1465: 1463: 913: 911: 909: 907: 905: 706: 201:that eventually gave rise to the cephalopods. 79: 4266: 2971: 2555: 2553: 2551: 2549: 2521: 2519: 2517: 2477: 2277: 1533: 1425: 1256: 1254: 1252: 1250: 1248: 1246: 1244: 1242: 1240: 1162: 1160: 1158: 1128: 1080: 791: 343: 279:separated by about half a millimetre, with a 38:period to become diverse and dominant in the 2918: 2143: 1814: 1781: 1699: 1306: 1094:"On the anatomy and relationships of recent 787: 785: 783: 781: 779: 777: 775: 2835: 2699: 1775: 1562: 1460: 1302: 1300: 1169:"Some lesser known features of the ancient 902: 679: 676:moving the head in and out of the chamber. 446:more broadly are rejected by most authors. 262:is arguably the earliest known crown-group 4273: 4259: 2978: 2964: 2792: 2546: 2514: 2471: 2191: 2110: 2104: 1634: 1343: 1237: 1155: 1091: 936: 859: 748: 746: 287:have been said to be the ancestors of the 4546:First appearance of long-lasting lineages 2682: 2617: 2319: 2257: 2065: 2048: 1991: 1942: 1924: 1732: 1668: 1611: 1601: 1508: 1208: 1124: 1122: 1120: 1118: 1039: 978: 968: 772: 4212:Transgenerational epigenetic inheritance 2985: 2751: 2336: 1820: 1476:. President's anniversary address 1986. 1297: 1226: 1222: 1220: 563: 405: 315: 245: 163:With the exception of the shelly genera 129: 2841: 2528:South African Journal of Marine Science 2422:"Hyoliths are Palaeozoic lophophorates" 1471: 743: 4732: 1393:Brock, G.A. (2004). "A new species of 1166: 1115: 4254: 3975:Dialogues Concerning Natural Religion 2959: 2273: 2271: 2269: 1821:Runnegar, B. (2011). "Once again: Is 1738: 1534:Boyle, Peter; Rodhouse, Paul (2004). 1527: 1392: 1217: 1046:Lemche, H.; Wingstrand, K.G. (1959). 134:Fossil orthoconic nautiloid from the 125: 2342: 2232:Kluessendorf, J.; Doyle, P. (2000). 752: 486:’s classification is now uncertain. 2076:and its occurrence in California". 1900: 1853: 1782:Mazurek, D.; Zatoń, M. (2011). "Is 1700:Mazurek, D.; Zatoń, M. (2011). "Is 294: 270:(north-east China) of the earliest 13: 4313: 3380:Evolutionary developmental biology 2912: 2868:10.1111/j.1502-3931.1987.tb02028.x 2266: 1537:Cephalopods: Ecology and fisheries 1454:10.1111/j.1502-3931.1973.tb01199.x 853:10.1111/j.1502-3931.1970.tb00829.x 311: 14: 4756: 2801:Journal of the Geological Society 1474:Journal of the Geological Society 1101:(Link to free full text + plates) 1066:(Link to free full text + plates) 995: 372:, whose siphuncles are thin. The 239: 4519:Earliest unambiguous cephalopods 4234: 4225: 4224: 2903:10.1111/j.1502-3931.2008.00133.x 1847:10.1111/j.1502-3931.2011.00296.x 1808:10.1111/j.1502-3931.2010.00253.x 1726:10.1111/j.1502-3931.2010.00253.x 1210:10.1111/j.1475-4983.2007.00644.x 662: 596: 402:Fossils mistaken for cephalopods 291:, the first "true cephalopods". 4037:Extended evolutionary synthesis 3226:Gene-centered view of evolution 2874: 2634: 2577: 2413: 2378: 2008: 1959: 1693: 1628: 1386: 725: 671:The earliest cephalopods, like 531: 489: 461: 204: 4615:the earliest cephalopod group 4301:The belemnite-cuttlefish-like 4165:Hologenome theory of evolution 4032:History of molecular evolution 3258:Evolutionarily stable strategy 3147:Last universal common ancestor 820: 651:is considered as belonging to 1: 4674:Probable misidentified genera 4645:Earliest coiled cephalopods: 3959:Renaissance and Enlightenment 1283:10.1144/GSL.SP.1989.047.01.04 737: 449: 421: 4286:(listed by first occurrence) 4170:Missing heritability problem 3797:Gamete differentiation/sexes 2773:(1): 105–132. Archived from 2407:10.1016/j.palaeo.2012.06.023 1603:10.1371/journal.pone.0007262 814:10.1016/j.palaeo.2008.12.015 700: 573:ultimately the ancestors of 559: 511: 178: 7: 1825:a stem-group cephalopod?". 1005:Evolution & Development 755:"Origin of the cephalopoda" 697:have also been documented. 547: 357:(with wide siphuncles) and 158: 142:; an internal mold showing 80:Traditional views of origin 10: 4761: 4559:Probable coleoid ancestor 3802:Life cycles/nuclear phases 3354:Trivers–Willard hypothesis 2667:10.1038/s41467-023-42842-x 2540:10.2989/025776198784126287 2304:10.1038/s41467-022-28333-5 2033:10.1038/s42003-022-04383-9 1984:10.1038/s42003-021-01885-w 1926:10.1186/s12915-022-01284-5 1517:Bulletin of Marine Science 1227:Majewske, Otto P. (1974). 361:(with narrow siphuncles). 344:Early Ordovician diversity 4667: 4608: 4514: 4505: 4445: 4425: 4365: 4338: 4329: 4311: 4292: 4220: 4120: 4045: 3949: 3876: 3832: 3687: 3591: 3408: 3367: 3300:Parent–offspring conflict 3236: 3105:Earliest known life forms 3026: 2993: 2602:10.1038/s42003-019-0523-2 2504:10.1080/00241160600623749 1546:10.1002/9780470995310.ch2 1540:. Ames, Iowa: Blackwell. 1139:10.1002/9780470995310.ch3 1092:Wingstrand, K.G. (1985). 685:known from the Paleozoic 4740:Evolution of protostomes 4153:Cultural group selection 4017:The eclipse of Darwinism 3989:On the Origin of Species 3964:Transmutation of species 2821:10.1144/gsjgs.150.6.1035 2715:embryonic development". 1494:10.1144/gsjgs.144.1.0001 762:Acta Palaeontologica Toe 680:Exceptional preservation 4158:Dual inheritance theory 3997:History of paleontology 2259:10.1111/1475-4983.00155 2202:Journal of Paleontology 2078:Journal of Paleontology 970:10.1073/pnas.0602578103 868:Journal of Paleontology 195: million years ago 4318: 3846:Punctuated equilibrium 3167:Non-adaptive radiation 3115:Evolutionary arms race 2842:Allison, P.A. (1987). 2590:Communications Biology 2478:Kröger, Björn (2006). 2021:Communications Biology 1972:Communications Biology 1878:10.1002/bies.201100001 1364:10.1002/bies.201100001 1167:Kröger, Björn (2007). 695:cephalopod egg fossils 569: 415: 321: 254: 151: 4317: 4138:Evolutionary medicine 4012:Mendelian inheritance 3720:Biological complexity 3708:Programmed cell death 3400:Phenotypic plasticity 3120:Evolutionary pressure 3110:Evidence of evolution 3008:Timeline of evolution 2717:Journal of Morphology 2647:Nature Communications 2284:Nature Communications 567: 409: 319: 249: 133: 4112:Teleology in biology 4007:Blending inheritance 3385:Genetic assimilation 3248:Artificial selection 2987:Evolutionary biology 2780:on 28 September 2011 2364:10.4002/040.052.0107 2343:Dzik, Jerzy (2010). 633:Bear Gulch Limestone 48:Small shelly fossils 4175:Molecular evolution 4133:Ecological genetics 4002:Transitional fossil 3792:Sexual reproduction 3632:endomembrane system 3561:pollinator-mediated 3517:dolphins and whales 3295:Parental investment 2933:1983Geo....11..647J 2895:2009Letha..42..204E 2860:1987Letha..20..117A 2813:1993JGSoc.150.1035B 2659:2023NatCo..14.8094K 2496:2006Letha..39..129K 2449:10.1038/nature20804 2441:2017Natur.541..394M 2399:2012PPP...353...21L 2296:2022NatCo..13.1107W 2250:2000Palgy..43..919K 2129:1993Geo....21..805S 1839:2011Letha..44..373R 1800:2011Letha..44....2M 1753:2013Pbio...39..297S 1718:2011Letha..44....2M 1661:10.1038/nature09068 1653:2010Natur.465..469S 1594:2009PLoSO...4.7262K 1486:1987JGSoc.144....1H 1446:1973Letha...6..275Y 1321:1983Geo....11..647J 1275:1989GSLSP..47...29W 1201:2007Palgy..50..565K 1050:Neopilina galatheae 961:2006PNAS..103.7723G 880:2009JPal...83..123L 845:1970Letha...3..363B 806:2009PPP...273..174K 691:Francis Creek shale 601:The Early Devonian 4319: 4148:Cultural evolution 3263:Fisher's principle 3192:Handicap principle 3182:Parallel evolution 3046:Adaptive radiation 2729:10.1002/jmor.10564 2393:. 353–355: 21–30. 570: 416: 410:Reconstruction of 322: 268:Fengshan Formation 255: 250:Reconstruction of 152: 126:Early shell record 4727: 4726: 4663: 4662: 4501: 4500: 4409:Paleocirroteuthis 4248: 4247: 3864:Uniformitarianism 3817:Sex-determination 3322:Sexual dimorphism 3317:Natural selection 3221:Unit of selection 3187:Signalling theory 2435:(7637): 394–397. 2387:Allatheca degeeri 2170:on 1 October 2008 1823:Nectocaris pteryx 1784:Nectocaris pteryx 1702:Nectocaris pteryx 1647:(7297): 469–472. 1555:978-0-632-06048-1 1148:978-0-470-99531-0 1054: 1017:10.1111/ede.12164 955:(20): 7723–7728. 929:978-0-12-751412-3 888:10.1666/08-078R.1 753:Dzik, J. (1981). 615:biota contains a 552:Hyoliths such as 430:Nectocaris pteryx 150:, both encrusted. 74:mollusc phylogeny 4752: 4512: 4511: 4375:Muensterelloidea 4336: 4335: 4287: 4275: 4268: 4261: 4252: 4251: 4238: 4228: 4227: 4027:Modern synthesis 3787:Multicellularity 3782:Mosaic evolution 3667:auditory ossicle 3349:Social selection 3332:Flowering plants 3327:Sexual selection 2980: 2973: 2966: 2957: 2956: 2952: 2907: 2906: 2878: 2872: 2871: 2839: 2833: 2832: 2807:(6): 1035–1038. 2796: 2790: 2789: 2787: 2785: 2779: 2764: 2755: 2749: 2748: 2708: 2697: 2696: 2686: 2638: 2632: 2631: 2621: 2581: 2575: 2574: 2557: 2544: 2543: 2523: 2512: 2511: 2506:. Archived from 2475: 2469: 2468: 2426: 2417: 2411: 2410: 2382: 2376: 2375: 2349: 2340: 2334: 2333: 2323: 2275: 2264: 2263: 2261: 2229: 2218: 2217: 2189: 2180: 2179: 2177: 2175: 2169: 2162: 2147: 2141: 2140: 2108: 2102: 2101: 2069: 2063: 2062: 2052: 2012: 2006: 2005: 1995: 1963: 1957: 1956: 1946: 1928: 1904: 1898: 1897: 1857: 1851: 1850: 1818: 1812: 1811: 1786:a cephalopod?". 1779: 1773: 1772: 1736: 1730: 1729: 1704:a cephalopod?". 1697: 1691: 1690: 1672: 1632: 1626: 1625: 1615: 1605: 1573: 1560: 1559: 1531: 1525: 1524: 1512: 1506: 1505: 1469: 1458: 1457: 1429: 1423: 1422: 1390: 1384: 1383: 1347: 1341: 1340: 1304: 1295: 1294: 1258: 1235: 1234: 1224: 1215: 1214: 1212: 1164: 1153: 1152: 1126: 1113: 1112: 1102: 1089: 1078: 1077: 1067: 1052: 1048:"The anatomy of 1043: 1037: 1036: 999: 993: 992: 982: 972: 940: 934: 933: 915: 900: 899: 863: 857: 856: 824: 818: 817: 800:(3–4): 174–201. 789: 770: 769: 759: 750: 732: 729: 723: 713: 377:wide-siphuncled 301:Yochelcionellids 295:Yochelcionellids 196: 146:and half-filled 115:monoplacophorans 4760: 4759: 4755: 4754: 4753: 4751: 4750: 4749: 4730: 4729: 4728: 4723: 4659: 4617:Ellesmerocerida 4604: 4600:Phragmoteuthids 4523:Plectronocerida 4497: 4441: 4421: 4361: 4325: 4322: 4309: 4288: 4285: 4281:Notable fossil 4279: 4249: 4244: 4216: 4143:Group selection 4116: 4041: 3945: 3872: 3834:Tempo and modes 3828: 3683: 3587: 3404: 3363: 3239: 3232: 3209:Species complex 3022: 3013:History of life 2989: 2984: 2927:(11): 647–650. 2915: 2913:Further reading 2910: 2879: 2875: 2854:(78): 117–121. 2840: 2836: 2797: 2793: 2783: 2781: 2777: 2762: 2756: 2752: 2709: 2700: 2639: 2635: 2582: 2578: 2572: 2558: 2547: 2524: 2515: 2476: 2472: 2424: 2418: 2414: 2383: 2379: 2347: 2341: 2337: 2276: 2267: 2230: 2221: 2190: 2183: 2173: 2171: 2167: 2160: 2148: 2144: 2109: 2105: 2070: 2066: 2013: 2009: 1964: 1960: 1905: 1901: 1858: 1854: 1819: 1815: 1780: 1776: 1737: 1733: 1698: 1694: 1633: 1629: 1574: 1563: 1556: 1532: 1528: 1513: 1509: 1470: 1461: 1430: 1426: 1391: 1387: 1348: 1344: 1315:(11): 647–650. 1305: 1298: 1259: 1238: 1225: 1218: 1175:Ellesmerocerida 1165: 1156: 1149: 1127: 1116: 1100: 1090: 1081: 1065: 1044: 1040: 1000: 996: 941: 937: 930: 916: 903: 864: 860: 825: 821: 790: 773: 757: 751: 744: 740: 735: 730: 726: 714: 707: 703: 682: 665: 599: 562: 550: 534: 516: 494: 480:silicon dioxide 466: 452: 426: 404: 346: 326:Ellesmerocerida 314: 312:Ellesmerocerida 297: 289:Ellesmerocerids 285:Plectronocerida 244: 221:monoplacophoran 209: 191: 183: 161: 128: 111:Plectronocerida 86:monoplacophoran 82: 66:monoplacophoran 17: 12: 11: 5: 4758: 4748: 4747: 4742: 4725: 4724: 4722: 4721: 4714: 4707: 4700: 4695: 4680:Nectocarididae 4677: 4675: 4671: 4669: 4665: 4664: 4661: 4660: 4658: 4657: 4649: 4643: 4633: 4619: 4613: 4609: 4606: 4605: 4603: 4602: 4597: 4587: 4584:Syllipsimopodi 4563: 4557: 4547: 4543: 4542: 4533:Monoplacophora 4528:Plectronoceras 4515: 4509: 4503: 4502: 4499: 4498: 4496: 4495: 4494: 4493: 4490:Belemnotheutis 4486: 4479: 4466: 4455: 4453: 4446: 4443: 4442: 4440: 4439: 4433: 4426: 4423: 4422: 4420: 4419: 4412: 4405: 4398: 4391: 4384: 4377: 4372: 4370: 4369:Early coleoids 4366: 4363: 4362: 4360: 4359: 4353: 4348: 4346: 4339: 4333: 4327: 4326: 4312: 4310: 4308: 4307: 4298: 4296: 4290: 4289: 4278: 4277: 4270: 4263: 4255: 4246: 4245: 4243: 4242: 4232: 4221: 4218: 4217: 4215: 4214: 4209: 4204: 4199: 4194: 4193: 4192: 4182: 4177: 4172: 4167: 4162: 4161: 4160: 4155: 4150: 4140: 4135: 4130: 4124: 4122: 4118: 4117: 4115: 4114: 4109: 4108: 4107: 4102: 4097: 4096: 4095: 4085: 4080: 4075: 4070: 4065: 4055: 4049: 4047: 4043: 4042: 4040: 4039: 4034: 4029: 4024: 4019: 4014: 4009: 4004: 3999: 3994: 3993: 3992: 3983:Charles Darwin 3980: 3979: 3978: 3966: 3961: 3955: 3953: 3947: 3946: 3944: 3943: 3938: 3933: 3928: 3923: 3921:Non-ecological 3918: 3913: 3908: 3903: 3898: 3893: 3888: 3882: 3880: 3874: 3873: 3871: 3870: 3861: 3852: 3838: 3836: 3830: 3829: 3827: 3826: 3821: 3820: 3819: 3814: 3809: 3804: 3799: 3789: 3784: 3779: 3774: 3769: 3764: 3759: 3754: 3749: 3744: 3739: 3738: 3737: 3727: 3722: 3717: 3712: 3711: 3710: 3705: 3694: 3692: 3685: 3684: 3682: 3681: 3680: 3679: 3674: 3672:nervous system 3669: 3664: 3659: 3651: 3650: 3649: 3644: 3639: 3634: 3629: 3624: 3614: 3609: 3604: 3598: 3596: 3589: 3588: 3586: 3585: 3580: 3575: 3570: 3565: 3564: 3563: 3553: 3552: 3551: 3546: 3545: 3544: 3539: 3529: 3524: 3519: 3514: 3509: 3508: 3507: 3502: 3492: 3482: 3477: 3476: 3475: 3465: 3460: 3455: 3450: 3449: 3448: 3438: 3433: 3432: 3431: 3421: 3415: 3413: 3406: 3405: 3403: 3402: 3397: 3392: 3387: 3382: 3377: 3371: 3369: 3365: 3364: 3362: 3361: 3356: 3351: 3346: 3345: 3344: 3339: 3334: 3324: 3319: 3314: 3309: 3304: 3303: 3302: 3297: 3287: 3282: 3277: 3276: 3275: 3265: 3260: 3255: 3250: 3244: 3242: 3234: 3233: 3231: 3230: 3229: 3228: 3218: 3213: 3212: 3211: 3206: 3196: 3195: 3194: 3184: 3179: 3174: 3172:Origin of life 3169: 3164: 3159: 3157:Microevolution 3154: 3152:Macroevolution 3149: 3144: 3139: 3138: 3137: 3127: 3122: 3117: 3112: 3107: 3102: 3097: 3092: 3090:Common descent 3087: 3086: 3085: 3075: 3070: 3068:Baldwin effect 3065: 3064: 3063: 3058: 3048: 3043: 3038: 3032: 3030: 3024: 3023: 3021: 3020: 3015: 3010: 3005: 3000: 2994: 2991: 2990: 2983: 2982: 2975: 2968: 2960: 2954: 2953: 2914: 2911: 2909: 2908: 2889:(2): 204–217. 2873: 2834: 2791: 2750: 2698: 2633: 2576: 2570: 2545: 2513: 2510:on 2012-10-20. 2490:(2): 129–139. 2470: 2412: 2377: 2335: 2265: 2219: 2181: 2142: 2103: 2084:(2): 329–336. 2064: 2007: 1958: 1899: 1872:(8): 602–613. 1852: 1813: 1774: 1747:(2): 291–321. 1731: 1692: 1627: 1561: 1554: 1526: 1507: 1459: 1424: 1385: 1358:(8): 602–613. 1342: 1296: 1236: 1216: 1195:(3): 565–572. 1154: 1147: 1133:. p. 36. 1114: 1096:Monoplacophora 1079: 1038: 1011:(6): 337–346. 994: 935: 928: 901: 874:(1): 123–127. 858: 839:(4): 363–392. 819: 771: 741: 739: 736: 734: 733: 724: 704: 702: 699: 687:Hunsrück Slate 681: 678: 664: 661: 653:Octopodiformes 648:Syllipsimopodi 598: 595: 561: 558: 549: 546: 533: 530: 515: 510: 493: 488: 465: 460: 456:chimera fossil 451: 448: 425: 420: 403: 400: 345: 342: 331:Paradakeoceras 313: 310: 296: 293: 259:Plectronoceras 252:Plectronoceras 243: 241:Plectronoceras 238: 208: 203: 182: 177: 160: 157: 127: 124: 95:Plectronoceras 81: 78: 27:found in late 15: 9: 6: 4: 3: 2: 4757: 4746: 4743: 4741: 4738: 4737: 4735: 4720: 4719: 4715: 4713: 4712: 4708: 4706: 4705: 4701: 4699: 4696: 4693: 4692: 4687: 4686: 4681: 4678: 4676: 4673: 4672: 4670: 4668:Misidentified 4666: 4656: 4655: 4650: 4648: 4644: 4642: 4638: 4634: 4632: 4628: 4624: 4620: 4618: 4614: 4611: 4610: 4607: 4601: 4598: 4596: 4592: 4588: 4586: 4585: 4580: 4579: 4574: 4573: 4568: 4564: 4562: 4558: 4555: 4551: 4548: 4545: 4544: 4540: 4539: 4534: 4530: 4529: 4524: 4520: 4517: 4516: 4513: 4510: 4508: 4504: 4492: 4491: 4487: 4485: 4484: 4480: 4478: 4477: 4473: 4472: 4470: 4467: 4465: 4464: 4459: 4456: 4454: 4452: 4448: 4447: 4444: 4438: 4434: 4431: 4428: 4427: 4424: 4418: 4417: 4413: 4411: 4410: 4406: 4404: 4403: 4399: 4397: 4396: 4392: 4390: 4389: 4388:Styletoctopus 4385: 4383: 4382: 4381:Proteroctopus 4378: 4376: 4373: 4371: 4368: 4367: 4364: 4358: 4354: 4352: 4349: 4347: 4345: 4341: 4340: 4337: 4334: 4332: 4328: 4324: 4316: 4306: 4305: 4300: 4299: 4297: 4295: 4291: 4284: 4276: 4271: 4269: 4264: 4262: 4257: 4256: 4253: 4241: 4237: 4233: 4231: 4223: 4222: 4219: 4213: 4210: 4208: 4205: 4203: 4200: 4198: 4195: 4191: 4188: 4187: 4186: 4185:Phylogenetics 4183: 4181: 4178: 4176: 4173: 4171: 4168: 4166: 4163: 4159: 4156: 4154: 4151: 4149: 4146: 4145: 4144: 4141: 4139: 4136: 4134: 4131: 4129: 4126: 4125: 4123: 4119: 4113: 4110: 4106: 4103: 4101: 4098: 4094: 4091: 4090: 4089: 4088:Structuralism 4086: 4084: 4081: 4079: 4076: 4074: 4071: 4069: 4066: 4064: 4063:Catastrophism 4061: 4060: 4059: 4056: 4054: 4051: 4050: 4048: 4044: 4038: 4035: 4033: 4030: 4028: 4025: 4023: 4022:Neo-Darwinism 4020: 4018: 4015: 4013: 4010: 4008: 4005: 4003: 4000: 3998: 3995: 3991: 3990: 3986: 3985: 3984: 3981: 3977: 3976: 3972: 3971: 3970: 3967: 3965: 3962: 3960: 3957: 3956: 3954: 3952: 3948: 3942: 3939: 3937: 3936:Reinforcement 3934: 3932: 3929: 3927: 3924: 3922: 3919: 3917: 3914: 3912: 3909: 3907: 3904: 3902: 3899: 3897: 3894: 3892: 3889: 3887: 3884: 3883: 3881: 3879: 3875: 3869: 3868:Catastrophism 3865: 3862: 3860: 3859:Macromutation 3856: 3855:Micromutation 3853: 3851: 3847: 3843: 3840: 3839: 3837: 3835: 3831: 3825: 3822: 3818: 3815: 3813: 3810: 3808: 3805: 3803: 3800: 3798: 3795: 3794: 3793: 3790: 3788: 3785: 3783: 3780: 3778: 3775: 3773: 3770: 3768: 3765: 3763: 3762:Immune system 3760: 3758: 3755: 3753: 3750: 3748: 3745: 3743: 3740: 3736: 3733: 3732: 3731: 3728: 3726: 3723: 3721: 3718: 3716: 3713: 3709: 3706: 3704: 3701: 3700: 3699: 3696: 3695: 3693: 3691: 3686: 3678: 3675: 3673: 3670: 3668: 3665: 3663: 3660: 3658: 3655: 3654: 3652: 3648: 3645: 3643: 3640: 3638: 3635: 3633: 3630: 3628: 3625: 3623: 3622:symbiogenesis 3620: 3619: 3618: 3615: 3613: 3610: 3608: 3605: 3603: 3600: 3599: 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3375:Canalisation 3253:Biodiversity 2998:Introduction 2924: 2920: 2886: 2882: 2876: 2851: 2847: 2837: 2804: 2800: 2794: 2782:. 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Putative 613:Mazon Creek 542:brachiopods 526:Mazon Creek 524:known from 383:Discocerida 366:Orthocerids 337:Levisoceras 272:Fengshanian 166:Ectenolites 21:cephalopods 4745:Teuthology 4734:Categories 4691:Nectocotis 4685:Nectocaris 4654:Shimanskya 4641:Oncocerida 4637:Ascocerida 4623:Endocerida 4591:belemnoids 4561:Bactritida 4507:Palaeozoic 4476:Belemnites 4469:Belemnites 4463:Diplobelus 4451:belemnoids 4344:nautiloids 4304:Belosaepia 4068:Lamarckism 4046:Philosophy 3969:David Hume 3931:Peripatric 3926:Parapatric 3911:Ecological 3891:Anagenesis 3886:Allopatric 3878:Speciation 3842:Gradualism 3767:Metabolism 3627:chromosome 3617:Eukaryotes 3395:Modularity 3312:Population 3238:Population 3199:Speciation 3177:Panspermia 3130:Extinction 3125:Exaptation 3100:Divergence 3073:Cladistics 3061:Reciprocal 3041:Adaptation 2596:(1): 280. 2244:(5): 919. 2123:(9): 805. 1978:(1): 388. 1833:(4): 373. 1794:(1): 2–4. 1670:1807/32368 1440:(3): 275. 1171:Cephalopod 738:References 720:exogastric 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520:Pohlsepia 513:Pohlsepia 435:arthropod 370:Lituitids 281:siphuncle 236:fossils. 225:siphuncle 187:Tannuella 180:Tannuella 144:siphuncle 100:siphuncle 58:sclerites 40:Paleozoic 4567:coleoids 4554:ceratite 4331:Mesozoic 4294:Cenozoic 4230:Category 4105:Vitalism 4100:Theistic 4093:Spandrel 3777:Morality 3772:Monogamy 3647:plastids 3612:Flagella 3568:Reptiles 3549:sea cows 3532:primates 3441:Molluscs 3419:Bacteria 3307:Mutation 3240:genetics 3216:Taxonomy 3162:Mismatch 3142:Homology 3056:Cheating 3051:Altruism 2784:21 April 2745:13109195 2737:17654542 2713:Nautilus 2693:38062003 2684:10703834 2628:31372519 2457:28077871 2372:85622212 2330:35260548 2059:36635404 2002:33758350 1953:35421982 1886:21681989 1769:85744624 1687:20505727 1622:19789709 1582:PLOS ONE 1372:21681989 1057:Mollusca 1033:37343813 1025:26487042 989:16675549 829:Tommotia 673:Nautilus 586:nautilus 548:Hyoliths 444:molluscs 381:and the 218:Cambrian 159:Cambrian 140:Kentucky 53:Tommotia 50:such as 44:Mesozoic 31:strata. 29:Cambrian 4395:Keuppia 4121:Related 3951:History 3812:Meiosis 3747:Empathy 3742:Emotion 3642:nucleus 3583:Viruses 3573:Spiders 3485:Mammals 3468:Insects 3268:Fitness 3204:Species 3003:Outline 2929:Bibcode 2921:Geology 2891:Bibcode 2883:Lethaia 2856:Bibcode 2848:Lethaia 2809:Bibcode 2655:Bibcode 2619:6668408 2492:Bibcode 2484:Lethaia 2465:4409157 2437:Bibcode 2395:Bibcode 2321:8904582 2292:Bibcode 2246:Bibcode 2214:1304159 2125:Bibcode 2117:Geology 2098:1302218 2050:9837193 1993:7987959 1944:9008929 1894:2767810 1835:Bibcode 1827:Lethaia 1796:Bibcode 1788:Lethaia 1749:Bibcode 1714:Bibcode 1712:: 2–4. 1706:Lethaia 1649:Bibcode 1613:2749442 1590:Bibcode 1482:Bibcode 1442:Bibcode 1434:Lethaia 1380:2767810 1317:Bibcode 1309:Geology 1271:Bibcode 1197:Bibcode 1111:: 7–94. 1076:: 9–73. 980:1472512 957:Bibcode 876:Bibcode 841:Bibcode 833:Lethaia 802:Bibcode 617:decapod 148:camerae 4565:Early 4240:Portal 3916:Hybrid 3752:Ethics 3594:organs 3556:Plants 3542:lemurs 3537:humans 3522:horses 3512:hyenas 3500:wolves 3495:canids 3429:origin 2947:  2827:  2743:  2735:  2691:  2681:  2673:  2626:  2616:  2608:  2568:  2463:  2455:  2429:Nature 2370:  2328:  2318:  2310:  2212:  2174:1 June 2096:  2088:  2057:  2047:  2039:  2000:  1990:  1951:  1941:  1933:  1892:  1884:  1767:  1685:  1677:  1641:Nature 1620:  1610:  1552:  1500:  1417:  1378:  1370:  1335:  1289:  1173:order 1145:  1031:  1023:  987:  977:  926:  894:  46:seas. 4435:late 4355:True 3703:Death 3698:Aging 3677:brain 3463:Fungi 3424:Birds 3337:Fungi 3135:Event 3018:Index 2825:S2CID 2778:(PDF) 2763:(PDF) 2741:S2CID 2461:S2CID 2425:(PDF) 2368:S2CID 2348:(PDF) 2210:JSTOR 2168:(PDF) 2161:(PDF) 2094:JSTOR 1890:S2CID 1765:S2CID 1498:S2CID 1376:S2CID 1287:S2CID 1029:S2CID 892:S2CID 758:(PDF) 277:septa 155:age. 4552:and 4190:Tree 3662:hair 3602:Cell 3505:dogs 3490:cats 3480:Life 3458:Fish 3411:taxa 2945:ISSN 2786:2009 2733:PMID 2689:PMID 2671:ISSN 2624:PMID 2606:ISSN 2566:ISBN 2453:PMID 2326:PMID 2308:ISSN 2196:and 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Index

cephalopods
nautiloids
Cambrian
Ordovician
Paleozoic
Mesozoic
Small shelly fossils
Tommotia
sclerites
tryblidiid
monoplacophoran
Scaphopoda
mollusc phylogeny
monoplacophoran
gastropods
Plectronoceras
siphuncle
Knightoconus
Plectronocerida
monoplacophorans
gastropods

Ordovician
Kentucky
siphuncle
camerae
Ectenolites
Eoclarkoceras
Tannuella
522

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