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A collection of fossil remains associated in a specified deposit or sample. Its members may have different original habitats or ages; transport of fossil remains and time averaging affect its interpretation.

taphonomy studies the transformation of biological remains from death or production into the material ultimately recovered and interpreted. It explains how a living organism or community becomes an incomplete geological sample. For shed structures or trace fossils, production of the evidence need not involve the death of the producer. Its relevance therefore extends beyond asking whether a skeleton was buried intact.

Three primary process classes are decay; physical disarticulation and transport; and burial alteration, including diagenetic mineralization. The boundaries are operational and the mechanisms interact: post-mortem decay can continue after burial, and previously buried remains can be reworked and transported again. biostratinomy groups events before final burial, whereas diagenesis groups subsequent physical and chemical changes. Those are stages or settings, rather than three mutually exclusive mechanisms.

First, post-mortem decay transforms tissues by autolysis, microbial decomposition and associated chemical reactions. Soft tissues, connective tissues and different phylogenetic characters disappear at different rates. The important result is not simply that hard parts survive longer: a partly decayed organism can acquire a misleading anatomical combination. Experiments on amphioxus and lamprey larvae followed recognizable characters through decomposition. Derived diagnostic features tended to disappear before some more general chordate features, producing a directional bias. Coding every unobserved diagnostic character as ancestrally absent can push a genuinely derived fossil toward an earlier position on a phylogenetic tree, the effect called stemward slippage.^[ref]

Experiments on adult hagfish and lampreys extended the comparison beyond larvae. They documented transformations as well as disappearance, so a residual stain or collapsed structure should not automatically be identified as an intact organ. Replicate specimens sampled through time are needed because destructive observations cannot follow every internal character in the same individual. For a new experimental test, temperature, water chemistry, microbial conditions and starting condition should be recorded and, where tested, varied independently. A laboratory sequence supplies constraints on interpretations; it is not a universal clock assigning an exact post-mortem duration to every fossil.^[ref]

Second, disarticulation, fragmentation and taphonomic transport alter which elements occur together and where they accumulate. Loss of ligaments releases bones, while currents or scavengers can move them. Shape, density, size, articulation and orientation influence transportability, so a concentration of robust elements need not represent the most abundant living species or the original place of death. Flow experiments and comparison of element representation, as developed in Michael R. Voorhies's vertebrate assemblage study, provide a basis for testing such alternatives. A useful comparison measures elements under specified flow and sediment conditions, with articulated versus disarticulated material distinguished. hydraulic sorting cannot be transferred unchanged between all animals and environments.^[ref]

The consequences include mixing habitats and ages. An apparently coherent bone bed may combine local and transported animals; reworking of fossils can place older remains in younger sediment; time averaging can combine successive communities into one assemblage. None implies that every fossil assemblage is hopelessly mixed. Articulation, abrasion, orientation, size distributions, sedimentary context and independent age information can instead delimit the plausible history. Abrasion alone is an imperfect transport-distance meter because material properties and the transport medium also matter.

Third, burial changes both preservation and geometry. Rapid isolation can reduce scavenging, but burial does not halt all decomposition. sedimentary compaction flattens and fractures remains; dissolution removes mineralized tissues; precipitation can infill pores or replicate tissues; fossil recrystallization can erase original microscopic detail. A fossil can therefore retain an excellent outline but lack its original chemistry, or preserve histology while its overall shape has been distorted. Mineralized replacement is not the only route to fossilization, and surviving original hard parts need not have undergone complete replacement.

Experiments by Derek E. G. Briggs and Amanda J. Kear illustrate constructive as well as destructive diagenesis. Decaying shrimps developed diagenetic mineralization by calcium phosphate preserving muscle detail, particularly in oxygen-restricted systems, with the animal itself supplying phosphate. diagenetic mineralization began on a timescale of weeks. This demonstrates a mechanism by which decay-associated chemistry can stabilize fine structures before they disappear. It does not show that low oxygen guarantees preservation: chemical availability, acidity, tissue composition and the relative rates of destruction and precipitation still control the outcome.^[ref]

These mechanisms are indispensable for reconstructing the history of life. A fossil's first occurrence is a minimum observation of a lineage, not automatically its evolutionary origin. A sudden appearance of soft-bodied organisms can reflect a new window of exceptional preservation, while disappearance of a phylogenetic character can reflect its destruction rather than evolutionary loss. Relative fossil abundance reflects both biological abundance and the probabilities of production, preservation, exposure and recovery. Comparisons of diversity through time must therefore consider changes in environments, preservational pathways and sampling. The fossil record is filtered evidence whose reliability can be tested; taphonomy identifies which biological conclusions that evidence can support.

taphonomic bias is systematic distortion of biological information between a living community and the fossil record. Death, carcass decay, scavenging, transport, burial, chemical alteration, exposure and collection all filter what is observed. A deposit therefore samples organisms, body parts and environments unequally. This is more than incompleteness: preferential preservation of a particular tissue or habitat can produce a misleading pattern of abundance, anatomy or evolutionary timing.

An autochthonous fossil assemblage contains remains preserved where the organisms lived; an allochthonous fossil assemblage contains material transported from elsewhere. These describe provenance, rather than two levels of fidelity. In an allochthonous fossil assemblage, currents can separate elements by size, shape and density, concentrate resistant teeth or scales, remove delicate bodies and mix organisms from different habitats. Erosion and redeposition can also introduce older fossils into younger sediment. Such reworking differs from simple transport of recently dead animals. time averaging mixes deaths from different times even without long-distance transport. A concentration of robust remains consequently need not represent either a locally abundant living population or a single ecological event.

An autochthonous fossil assemblage avoids some transport distortion, but still selects organisms and characters. A bottom-dwelling community rapidly buried in place can be unusually well represented while swimmers above it, unmineralized tissues and organisms living outside that depositional setting are missing. Conversely, an intact carcass can travel before burial, whereas locally decayed remains can become disarticulated without transport. Articulation, abrasion, preferred orientation, sedimentary context and age agreement must therefore be evaluated together. Local preservation does not imply an unbiased biological census.

The contrast between cyclostomes and early members of the gnathostome lineage is particularly revealing. Living cyclostomes, hagfish and lampreys, have no extensive mineralized external skeleton comparable to the armour of many early jawless relatives of gnathostomes. Their bodies are dominated by tissues whose preservation usually requires exceptional conditions. The abundance of isolated mineralized scales, plates or teeth can thus make a hard-bodied lineage conspicuous where a soft-bodied contemporary is virtually invisible. Importantly, the armoured jawless assemblage traditionally called ostracoderms is not simply the ancestral cyclostome record: many of its members belong on the gnathostome stem. Absence of jaws does not by itself establish cyclostome affinity.

There is also a character-level filter. Robert S. Sansom and colleagues followed experimental carcass decay of living chordates, and then examined hagfish and lampreys in detail. Anatomical characters did not disappear at random: loss of diagnostic features could make a derived animal appear more primitive. This produces stemward slippage if investigators mistake an unpreserved feature for a feature absent in life. The result is relevant both to isolated soft-bodied fossils and to the apparently long primitive intervals preceding well-preserved groups.^[ref][ref]

A useful experimental design records fresh anatomy first, samples replicated carcasses through time under stated temperature and chemical conditions, and scores the same characters in each specimen. Comparisons between animals and between preservational conditions test whether the loss order is reproducible. Such experiments identify plausible biases; they do not recreate every burial chemistry or prove that every uncertain fossil has undergone the same sequence. In a phylogenetic character matrix, genuinely unobservable anatomy should normally be coded as unknown rather than automatically absent. Comparison across differently preserved specimens can sometimes recover information that one specimen lacks.

Exceptional discoveries show what the ordinary record omits. The Late Devonian lamprey Priscomyzon from South Africa preserves a recognizable oral apparatus and branchial region without a massive mineralized skeleton. It shows that early lamprey anatomy can be recovered when the appropriate soft-tissue window is available; the gap before such a discovery is not evidence that the lineage had just originated.^[ref] The Cretaceous hagfish Tethymyxine preserves evidence including slime-producing structures, allowing characters unavailable in most older deposits to be brought into an analysis using phylogenetics. It supplies a minimum occurrence and anatomical information, not the date when hagfish originated.^[ref] Conversely, Early Silurian Qianodus is known through mineralized tooth whorls: such durable small remains can establish an early occurrence of a toothed gnathostome even where complete bodies are missing.^[ref]

The defensible comparison concerns preservation probabilities as well as biological histories. First fossil occurrences are minimum ages, and unequal counts need not measure unequal diversity. Independent anatomical characters, comparable depositional settings, searches for small hard parts and exceptional soft-tissue deposits together give a better test of early vertebrate history than a literal reading of the most conspicuous remains.