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59-400: A biostratigraphic unit is defined by the zone fossils it contains. These may be a single taxon or combinations of taxa if the taxa are relatively abundant, or variations in features related to the distribution of fossils. The same strata may be zoned differently depending on the diagnostic criteria or fossil group chosen, so there may be several, sometimes overlapping, biostratigraphic units in

118-455: A superbiozone in which the grouped biozones usually have a related characteristic. A succession of biozones is called biozonation . The length of time represented by a biostratigraphic zone is called a biochron . The concept of a biozone was first established by the 19th century paleontologist Albert Oppel , who characterized rock strata by the species of the fossilized animals found in them, which he called zone fossils. Oppel's biozonation

177-411: A flat plane. The most fundamental difference in spiral form is how strongly successive whorls expand and overlap their predecessors. This can be inferred by the size of the umbilicus, the sunken-in inner part of the coil, exposing older and smaller whorls. Evolute shells have very little overlap, a large umbilicus, and many exposed whorls. Involute shells have strong overlap, a small umbilicus, and only

236-526: A general shape to ammonite tentacles. A contemporary study found an ammonite isolated body, offering for the first time a glimpse into these animals' organs. The smallest ammonoid was Maximites from the Upper Carboniferous . Adult specimens reached only 10 mm (0.39 in) in shell diameter. Few of the ammonites occurring in the lower and middle part of the Jurassic period reached

295-524: A group continued through several major extinction events , although often only a few species survived. Each time, however, this handful of species diversified into a multitude of forms. Ammonite fossils became less abundant during the latter part of the Mesozoic , and although they seemingly survived the Cretaceous–Paleogene extinction event , all known Paleocene ammonite lineages are restricted to

354-411: A result of limpets attaching themselves to the shells. However, the triangular formation of the holes, their size and shape, and their presence on both sides of the shells, corresponding to the upper and lower jaws, is more likely evidence of the bite of a medium-sized mosasaur preying upon ammonites. Some ammonites appear to have lived in cold seeps and even reproduced there. The chambered part of

413-1989: A series on Paleontology [REDACTED] Fossils Fossilization Trace fossil Microfossil Fossil preparation Index fossil List of fossils List of fossil sites Lagerstätte fossil beds List of transitional fossils List of human evolution fossils Natural history Biogeography Extinction event Geochronology Geologic time scale Geologic record History of life Origin of life Paleoclimatology Timeline of evolution Transitional fossil Organs and processes Avian flight Cells Multicells Eyes Flagella Hair Mammalian auditory ossicles Mosaic evolution Nervous systems Sex Evolution of various taxa Birds Butterflies Cephalopods Cetaceans Dinosaurs Fishes Fungi Humans Insects Mammals Molluscs Plants Reptiles Sea cows Spiders Tetrapods Evolution Introduction to evolution Common descent Phylogeny Cladistics Biological classification History of paleontology History of paleontology Timeline of paleontology Branches of paleontology Biostratigraphy Ichnology Invertebrate paleontology Micropaleontology Molecular paleontology Palaeoxylology Paleobiology Paleobotany Paleoecology Paleogenetics Paleolimnology Paleomycology Paleoneurobiology Paleopathology Paleopedology Paleotempestology Paleozoology Palynology Sclerochronology Taphonomy Vertebrate paleontology Paleontology Portal Category v t e Index fossils (also known as guide fossils or indicator fossils) are fossils used to define and identify geologic periods (or faunal stages). Index fossils must have

472-2365: A short vertical range, wide geographic distribution and rapid evolutionary trends. Another term, "zone fossil", is used when the fossil has all the characters stated above except wide geographical distribution; thus, they correlate the surrounding rock to a biozone rather than a specific time period. Fossil Scientific Name Geological time interval Million Years Ago [REDACTED] Calico scallop Argopecten gibbus Quaternary 1.8  million years ago Neptunea tabulata Quaternary 1.8  million years ago [REDACTED] Viviparus glacialis Tiglian ( Early Pleistocene ) 0.5  million years ago Calyptraphorus velatus Tertiary Venericardia planicosta Eocene [REDACTED] Scaphites Scaphites hippocrepis Cretaceous 145 to 66 million years ago [REDACTED] Inoceramus Inoceramus labiatus Cretaceous [REDACTED] Perisphinctes Perisphinctes tiziani Jurassic 201.3 to 145 million years ago Nerinea trinodosa Jurassic Tropites subbullatus Triassic [REDACTED] Monotis subcircularis Triassic [REDACTED] Leptodus Leptodus americanus Permian Parafusulina Parafusulina bosei Permian Dictyoclostus americanus Pennsylvanian Lophophyllidium proliferum Pennsylvanian Cactocrinus multibrachiatus Mississippian Prolecanites gurleyi Mississippian [REDACTED] Mucrospirifer Mucrospirifer mucronatus Devonian 416 to 359 million years ago Palmatolepis unicornis Devonian Tetragraptus fructicosus Ordovician [REDACTED] Paradoxides Cambrian 509 to 500 million years ago Billingsella corrugata Cambrian [REDACTED] Archaocyathids Cambrian 529 to 509 million years ago See also [ edit ] Biostratigraphy#Index fossils References [ edit ] ^ Index Fossils , from

531-558: A single horny plate or a pair of calcitic plates. In the past, these plates were assumed to serve in closing the opening of the shell in much the same way as an operculum , but more recently they are postulated to have been a jaw apparatus. The plates are collectively termed the aptychus or aptychi in the case of a pair of plates, and anaptychus in the case of a single plate. The paired aptychi were symmetric to one another and equal in size and appearance. Anaptychi are relatively rare as fossils. They are found representing ammonites from

590-650: A size exceeding 23 cm (9.1 in) in diameter. Much larger forms are found in the later rocks of the upper part of the Jurassic and the lower part of the Cretaceous, such as Titanites from the Portland Stone of Jurassic of southern England, which is often 53 cm (1.74 ft) in diameter, and Parapuzosia seppenradensis of the Cretaceous period of Germany, which is one of the largest-known ammonites, sometimes reaching 2 m (6.6 ft) in diameter. The largest-documented North American ammonite

649-573: A small portion of fossils are preserved, a biozone does not represent the true range of that species in time. Moreover, ranges can be influenced by the Signor-Lipps effect , meaning that the last "disappearance" of a species tends to be observed further back in time than was actually the case. Zone fossils (Redirected from Zone fossils ) Fossils used to define and identity geologic periods [REDACTED] Examples of index fossils Part of

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708-465: Is Baculites , which has a nearly straight shell convergent with the older orthocone nautiloids. Still other species' shells are coiled helically (in two dimensions), similar in appearance to some gastropods (e.g., Turrilites and Bostrychoceras ). Some species' shells are even initially uncoiled, then partially coiled, and finally straight at maturity (as in Australiceras ). Perhaps

767-506: Is Parapuzosia bradyi from the Cretaceous, with specimens measuring 137 cm (4.5 ft) in diameter. Starting from the mid-Devonian, ammonoids were extremely abundant, especially as ammonites during the Mesozoic era. Many genera evolved and ran their course quickly, becoming extinct in a few million years. Due to their rapid evolution and widespread distribution, ammonoids are used by geologists and paleontologists for biostratigraphy . They are excellent index fossils , and it

826-407: Is a biozone that is defined by the range in which the abundance of a particular taxon is highest. Because an abundance zone requires a statistically high proportion of a particular taxon, the only way to define them is to trace the abundance of the taxon through time. As local environmental factors influence abundance, this can be an unreliable way of defining a biozone. Abundance zones are named after

885-432: Is a biozone with the upper boundary being the appearance of one taxon, and the lower boundary the appearance of another taxon. A lineage zone, also called a consecutive range zone , are biozones which are defined by being a specific segment of an evolutionary lineage. For example, a zone can be bounded by the highest occurrence of the ancestor of a particular of a taxon and the lowest occurrence of its descendant, or between

944-626: Is a narrow tubular structure that runs along the shell's outer rim, known as the venter, connecting the chambers of the phragmocone to the body or living chamber. This distinguishes them from living nautiloides ( Nautilus and Allonautilus ) and typical Nautilida , in which the siphuncle runs through the center of each chamber. However the very earliest nautiloids from the Late Cambrian and Ordovician typically had ventral siphuncles like ammonites, although often proportionally larger and more internally structured. The word "siphuncle" comes from

1003-411: Is from κέρας ( kéras ) meaning "horn". Ammonites (subclass Ammonoidea) can be distinguished by their septa, the dividing walls that separate the chambers in the phragmocone, by the nature of their sutures where the septa join the outer shell wall, and in general by their siphuncles . Ammonoid septa characteristically have bulges and indentations and are to varying degrees convex when seen from

1062-422: Is occasionally preserved in fossil specimens. The soft body of the creature occupied the largest segments of the shell at the end of the coil. The smaller earlier segments were walled off and the animal could maintain its buoyancy by filling them with gas. Thus, the smaller sections of the coil would have floated above the larger sections. Many ammonite shells have been found with round holes once interpreted as

1121-467: Is often possible to link the rock layer in which they are found to specific geologic time periods . Due to their free-swimming and/or free-floating habits, ammonites often happened to live directly above seafloor waters so poor in oxygen as to prevent the establishment of animal life on the seafloor. When upon death the ammonites fell to this seafloor and were gradually buried in accumulating sediment, bacterial decomposition of these corpses often tipped

1180-633: Is often preserved. This type of preservation is found in ammonites such as Hoplites from the Cretaceous Gault clay of Folkestone in Kent, England. The Cretaceous Pierre Shale formation of the United States and Canada is well known for the abundant ammonite fauna it yields, including Baculites , Placenticeras , Scaphites , Hoploscaphites and Jeletzkytes , as well as many uncoiled forms. Many of these also have much or all of

1239-538: Is thought to be because the female required a larger body size for egg production. A good example of this sexual variation is found in Bifericeras from the early part of the Jurassic period of Europe . Only recently has sexual variation in the shells of ammonites been recognized. The macroconch and microconch of one species were often previously mistaken for two closely related but different species occurring in

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1298-591: The Neo-Latin siphunculus , meaning "little siphon". Originating from within the bactritoid nautiloids, the ammonoid cephalopods first appeared in the Devonian ( circa 409 million years ago (Mya)) and became extinct shortly after Cretaceous (66 Mya). The classification of ammonoids is based in part on the ornamentation and structure of the septa comprising their shells' gas chambers. The Ammonoidea can be divided into six orders, listed here starting with

1357-768: The Paleocene epoch (65–61 Ma). Goniatites, which were a dominant component of Early and Middle Permian faunas, became rare in the Late Permian, and no goniatite is thought to have crossed into the Triassic. Ceratitida originated during the Middle Permian, likely from the Daraelitidae , and radiated in the Late Permian. In the aftermath of the Permian–Triassic extinction event , Ceratitids represent

1416-638: The Solnhofen Limestone , their soft-part record is surprisingly sparse. Beyond a tentative ink sac and possible digestive organs, no soft parts were known until 2021. When neutron imaging was used on a fossil found in 1998, part of the musculature became visible and showed they were able to retract themselves into the shell for protection, and that the retractor muscles and hyponome that work together to enable jet propulsion in nautilus worked independently in ammonites. The reproductive organs show possible traces of spermatophores, which would support

1475-523: The US Geological Survey . Updated July 31, 1997. Retrieved from " https://en.wikipedia.org/w/index.php?title=List_of_index_fossils&oldid=1229171730 " Category : Index fossils Hidden categories: Pages with non-numeric formatnum arguments Articles with short description Short description is different from Wikidata Ammonites Ammonoids are extinct spiral shelled cephalopods comprising

1534-433: The buoyancy of the shell and thereby rise or descend in the water column. A primary difference between ammonites and nautiloids is the siphuncle of ammonites (excepting Clymeniina ) runs along the ventral periphery of the septa and camerae (i.e., the inner surface of the outer axis of the shell), while the siphuncle of nautiloids runs more or less through the center of the septa and camerae. One feature found in shells of

1593-653: The Ceratitina from the Triassic; and the Ammonitina, Lytoceratina and Phylloceratina from the Jurassic and Cretaceous. In subsequent taxonomies, these are sometimes regarded as orders within the subclass Ammonoidea. Because ammonites and their close relatives are extinct, little is known about their way of life. Their soft body parts are very rarely preserved in any detail. Nonetheless, much has been worked out by examining ammonoid shells and by using models of these shells in water tanks. Many ammonoids probably lived in

1652-540: The Devonian period through those of the Cretaceous period. Calcified aptychi only occur in ammonites from the Mesozoic era. They are almost always found detached from the shell, and are only very rarely preserved in place. Still, sufficient numbers have been found closing the apertures of fossil ammonite shells as to leave no doubt as to their identity as part of the anatomy of an ammonite. Large numbers of detached aptychi occur in certain beds of rock (such as those from

1711-519: The Mesozoic in the Alps ). These rocks are usually accumulated at great depths. The modern Nautilus lacks any calcitic plate for closing its shell, and only one extinct nautiloid genus is known to have borne anything similar. Nautilus does, however, have a leathery head shield (the hood) which it uses to cover the opening when it retreats inside. There are many forms of aptychus, varying in shape and

1770-440: The ammonite shell is called a phragmocone . It contains a series of progressively larger chambers, called camerae (sing. camera) that are divided by thin walls called septa (sing. septum). Only the last and largest chamber, the body chamber , was occupied by the living animal at any given moment. As it grew, it added newer and larger chambers to the open end of the coil. Where the outer whorl of an ammonite shell largely covers

1829-456: The ammonoid suture line (the intersection of the septum with the outer shell) is variably folded, forming saddles ("peaks" that point towards the aperture) and lobes ("valleys" which point away from the aperture). The suture line has four main regions. The external or ventral region refers to sutures along the lower (outer) edge of the shell, where the left and right suture lines meet. The external (or ventral) saddle, when present, lies directly on

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1888-474: The animal's life; additional shell layers covered it. The majority of ammonoid specimens, especially those of the Paleozoic era, are preserved only as internal molds; the outer shell (composed of aragonite ) has been lost during the fossilization process. Only in these internal-mould specimens can the suture lines be observed; in life, the sutures would have been hidden by the outer shell. The ammonoids as

1947-419: The delicate balance of local redox conditions sufficiently to lower the local solubility of minerals dissolved in the seawater, notably phosphates and carbonates . The resulting spontaneous concentric precipitation of minerals around a fossil, a concretion , is responsible for the outstanding preservation of many ammonite fossils. When ammonites are found in clays , their original mother-of-pearl coating

2006-466: The first heteromorph ammonoid fossils belongs to the genus Rhabdoceras. The three other heteromorphic genera were Hannaoceras, Cochloceras and Choristoceras. All of them went extinct at the end of Triassic. In the Jurassic an uncoiled shell was found in the Spiroceratoidea, but by the end of Cretaceous the only heteromorph ammonites remaining belonged to the suborder Ancyloceratina. One example

2065-420: The first saddle and lobe pair past the external region as the suture line extends up the side of the shell. The lateral saddle and lobe are usually larger than the ventral saddle and lobe. Additional lobes developing towards the inner edge of a whorl are labelled umbilical lobes, which increase in number through ammonoid evolution as well as an individual ammonoid's development. In many cases the distinction between

2124-433: The front, distinguishing them from nautiloid septa, which are typically simple concave, dish-shaped structures. The topology of the septa, especially around the rim, results in the various suture patterns found. The septal curvature in nautiloids and ammonoids also differ in that the septa curves towards the opening in nautiloids, and away from the opening in ammоnoids. While nearly all nautiloids show gently curving sutures,

2183-422: The geographic and stratigraphic range of occurrence of a taxon (or taxa). There are two types of range zones: A taxon-range zone is simply the biozone defined by the first ( first appearance datum or FAD ) and last ( last appearance datum or LAD ) occurrence of a single taxon. The boundaries are defined by the lowest and highest stratigraphic occurrence of that particular taxon. Taxon-range zones are named after

2242-503: The hypothesis that the microconchs were males. They likely bore a radula and beak, a marginal siphuncle and ten arms. They operated by direct development with sexual reproduction, were carnivorous, and had a crop for food storage. They are unlikely to have dwelt in fresh or brackish water. Many ammonites were likely filter feeders , so adaptations associated with this lifestyle like sieves probably occurred. A 2021 study found ammonite specimens with preserved hook-like suckers, providing

2301-511: The largest and most recent whorls are exposed. Shell structure can be broken down further by the width of the shell, with implications for hydrodynamic efficiency. Major shell forms include: Ammonites vary greatly in the ornamentation (surface relief) of their shells. Some may be smooth and relatively featureless, except for growth lines, resembling that of the modern Nautilus . In others, various patterns of spiral ridges, ribs, nodes, or spines are presented. This type of complex ornamentation of

2360-510: The lateral and umbilical regions are unclear; new umbilical features can develop from subdivisions of other umbilical features, or from subdivisions of lateral features. Lobes and saddles which are so far towards the center of the whorl that they are covered up by succeeding whorls are labelled internal (or dorsal) lobes and saddles. Three major types of suture patterns are found in the Ammonoidea: The siphuncle in most ammonoids

2419-434: The lower midline of the shell. As a result, it is often called the median saddle. On suture diagrams the median saddle is supplied with an arrow which points towards the aperture. The median saddle is edged by fairly small external (or ventral) lobes. The earliest ammonoids lacked a median saddle and instead had a single midline ventral lobe, which in later forms is split into two or more components. The lateral region involves

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2478-416: The lowest occurrence of a taxon and the lowest occurrence of its descendant. Lineage zones are different from most other biozones because they need that the segments its bounded by are successive segments of an evolutionary lineage. This makes them similar to chronostratigraphical units - however, lineage zones, being a biozone, are restricted by the actual spatial range of fossils. Lineage zones are named for

2537-432: The modern Nautilus is the variation in the shape and size of the shell according to the sex of the animal, the shell of the male being slightly smaller and wider than that of the female. This sexual dimorphism is thought to be an explanation for the variation in size of certain ammonite shells of the same species, the larger shell (the macroconch ) being female, and the smaller shell (the microconch ) being male. This

2596-543: The most extreme and bizarre-looking example of a heteromorph is Nipponites , which appears to be a tangle of irregular whorls lacking any obvious symmetric coiling. Upon closer inspection, though, the shell proves to be a three-dimensional network of connected "U" shapes. Nipponites occurs in rocks of the upper part of the Cretaceous in Japan and the United States. Some ammonites have been found in association with

2655-575: The most primitive and going to the more derived: In some classifications, these are left as suborders, included in only three orders: Goniatitida , Ceratitida and Ammonitida . The Treatise on Invertebrate Paleontology (Part L, 1957) divides the Ammonoidea, regarded simply as an order, into eight suborders, the Anarcestina, Clymeniina, Goniatitina and Prolecanitina from the Paleozoic;

2714-781: The open water of ancient seas, rather than at the sea bottom, because their fossils are often found in rocks laid down under conditions where no bottom-dwelling life is found. In general, they appear to have inhabited the upper 250 meters of the water column. Many of them (such as Oxynoticeras ) are thought to have been good swimmers, with flattened, discus-shaped, streamlined shells, although some ammonoids were less effective swimmers and were likely to have been slow-swimming bottom-dwellers. Synchrotron analysis of an aptychophoran ammonite revealed remains of isopod and mollusc larvae in its buccal cavity, indicating at least this kind of ammonite fed on plankton . They may have avoided predation by squirting ink , much like modern cephalopods; ink

2773-478: The order Ammonitida , the only remaining group of ammonoids from the Jurassic up until their extinction. Ammonites are excellent index fossils , and linking the rock layer in which a particular species or genus is found to specific geologic time periods is often possible. Their fossil shells usually take the form of planispirals , although some helically spiraled and nonspiraled forms (known as heteromorphs ) have been found. The name "ammonite", from which

2832-478: The original shell, as well as the complete body chamber, still intact. Many Pierre Shale ammonites, and indeed many ammonites throughout earth history, are found inside concretions . Other fossils, such as many found in Madagascar and Alberta , Canada display iridescence . These iridescent ammonites are often of gem quality ( ammolite ) when polished. In no case would this iridescence have been visible during

2891-461: The preceding whorls, the specimen is said to be involute (e.g., Anahoplites ). Where it does not cover those preceding, the specimen is said to be evolute (e.g., Dactylioceras ). A thin living tube called a siphuncle passed through the septa, extending from the ammonite's body into the empty shell chambers. Through a hyperosmotic active transport process, the ammonite emptied water out of these shell chambers. This enabled it to control

2950-411: The same interval. Like lithostratigraphic units, biozones must have a type section designated as a stratotype . These stratotypes are named according to the typical taxon (or taxa) that are found in that particular biozone. The boundary of two distinct biostratigraphic units is called a biohorizon . Biozones can be further subdivided into subbiozones , and multiple biozones can be grouped together in

3009-494: The same rocks. However, because the dimorphic sizes are so consistently found together, they are more likely an example of sexual dimorphism within the same species. Whorl width in the body chamber of many groups of ammonites, as expressed by the width:diameter ratio, is another sign of dimorphism. This character has been used to separate "male" (Largiventer conch "L") from "female" (Leviventer conch "l"). The majority of ammonite species feature planispiral shells, tightly coiled in

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3068-519: The scientific term is derived, was inspired by the spiral shape of their fossilized shells, which somewhat resemble tightly coiled rams ' horns. Pliny the Elder ( d. 79 AD near Pompeii) called fossils of these animals ammonis cornua (" horns of Ammon ") because the Egyptian god Ammon ( Amun ) was typically depicted wearing rams' horns. Often, the name of an ammonite genus ends in - ceras , which

3127-479: The sculpture of the inner and outer surfaces, but because they are so rarely found in position within the shell of the ammonite it is often unclear to which species of ammonite one kind of aptychus belongs. A number of aptychi have been given their own genus and even species names independent of their unknown owners' genus and species, pending future discovery of verified occurrences within ammonite shells. Although ammonites do occur in exceptional lagerstatten such as

3186-415: The shell is especially evident in the later ammonites of the Cretaceous. Ammonoids with a shell shape diverging from the typical planispiral form are known as heteromorphs , instead forming a conch with detached whorls (open coiling) or non-planispiral coiling. These types of shells evolved four times in ammonoids, with the first forms appearing already in the Devonian period. In late Norian age in Triassic

3245-459: The specific taxon they represent. An assemblage zone is a biozone defined by three or more different taxa, which may or may not be related. The boundaries of an assemblage zone are defined by the typical, specified fossil assemblage's occurrence: this can include the appearance, but also the disappearance of certain taxa. Assemblage zones are named for the most characteristic or diagnostic fossils in its assemblage. An abundance zone, or acme zone ,

3304-432: The subclass Ammonoidea . They are more closely related to living coleoids (i.e., octopuses , squid and cuttlefish ) than they are to shelled nautiloids (such as the living Nautilus ). The earliest ammonoids appeared during the Devonian , with the last species vanishing during or soon after the Cretaceous–Paleogene extinction event . They are often called ammonites , which is most frequently used for members of

3363-417: The taxon in it. A concurrent-range zone uses the overlapping range of two taxa, with low boundary defined by the appearance of one taxon and high boundary defined by the disappearance of the other taxon. Concurrent-range zones are named after both of the taxa in it. An interval zone is defined as the body of strata between two bio-horizons, which are arbitrarily chosen. For example, a highest-occurrence zone

3422-580: The taxon that is the most abundant within its range. A great variety of species can be used in establishing biozonation. Graptolites and ammonites are some of the most useful as zone fossils, as they preserve well and often have relatively short biozones. Microfossils , such as dinoflagellates , foraminiferans , or plant pollen are also good candidates because they tend to be present even in very small samples and evolve relatively rapidly. Fossils of pigs and cannabis can be used for biozonation of Quaternary rocks as they were used by hominids . As only

3481-458: Was mainly based on Jurassic ammonites he found throughout Europe, which he used to classify the period into 33 zones (now 60). Alcide d'Orbigny would further reinforce the concept in his Prodrome de Paléontologie Stratigraphique , in which he established comparisons between geological stages and their biostratigraphy. The International Commission on Stratigraphy defines the following types of biozones: Range zones are biozones defined by

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