What is a Fossil Species..?
What do we currently understand by a ‘species’?
Naming species, also known as alpha taxonomy, forms the fundamental basis and core of systematic analysis (e.g., for biodiversity, macroevolutionary and ecological studies). Since the origin of the species concept, there has been heated and continuous debate as to what exactly constitutes a species. The discovery of DNA as an evolutionary tool sparked a vigorous new line of discussion into what precisely defines a species. Even to this day, despite a wealth of theoretical, empirical and philosophical studies, there is still a lack of consensus in the way of rigorously defining a species unit. This is not to say that there isn’t a general idea of what a species is (ask any biologist or palaeontologist); in fact most people reading this will probably have a pretty good idea of what they define a species as. But there is not total agreement, not by a long shot. Furthermore, most if not all current species concepts are explicitly based on extant organisms which can be directly observed in their every day life, and also just happen to provide a near-endless supply of DNA. But what about fossils? I’ve outlined the critical importance of using fossils in conjunction with pretty much any systematic analysis before (here), but how do palaeontologists actually recognise and delimit fossil species? This is a pretty serious issue, considering the DNA of fossil organisms has always decayed long before exhumation (except in exceptional circumstances), and fossil remains typically only represent a biased sample of the organism it once was.
What are the current species concepts?
For biologists, the species problem can be framed as: “What level of divergence (morphological, genetic, etc.) between populations constitutes species diagnosis?” This can be modified slightly according to whichever species concept is being applied (see below). Using DNA as a sole basis for species delimitation is fraught with issues, including but not limited to the concept of paralogy, lateral gene transfer (transfection), arbitrary delimitation protocols, lack of data (e.g., in tropical species), and often a lack of training or instrumentation (in third world countries mainly). The relative issues and benefits of morphological and/or DNA-based analysis is a tale for another time though. Currently, there is no single ‘silver bullet’ technique for species delimitation (although many DNA taxonomists will try and pretend there is..). What we actually have are a series of non-independent concepts that actually apply to different stages of the speciation process (de Quieroz 2007 discusses this in a most brilliant manner). Here are a couple of examples:
Biological Species Concept: This is the one most people will have heard of. Species are defined by reproductive isolation, or the ability to produce fertile offspring. Obvious issues with this are if you’re asexual, and how do you know if two organisms (within reason) can or cannot mate if they are not sympatric. Also, reproductive isolation is not always congruent with morphological divergence, so is inadequate with purely morphological data sets.
Phylogenetic Species Concept: This refers to diagnosability based on the monophyly of a population. This invariably invokes the use of DNA. Genetic population divergence goes through three stages: polyphyly, paraphyly and finally reciprocal monophyly, giving two or more irreducible clusters of diagnosable organisms with a traceable pattern of ancestry and descent.
Genealogical Species Concept: This is the use of multiple gene marker distributions to delimit putative species by identifying periods of complete lineage sorting. Essentially this means that the incongruence from coalescence (the point in time where gene variants unite in a gene genealogy) no longer affects delimitation.
A currently widely used method is DNA barcoding. Some molecular systematists deem this as a powerful enough tool to entirely replace standard Linnaean taxonomy, although (obviously) there are numerous vocal objections. DNA barcoding operates on the assumption that there is a threshold for species delimitation based on a single gene, which is the entirely arbitrary 10 times greater genetic divergence (interspecific) than intraspecificity, leading to the concept of reciprocal monophyly. It works sometimes, but is fraught again with theoretical and empirical problems. (I love the idea that molecular systematists will go to the tropics with the aim of identifying unique or diverse haplotypes in insects etc., by killing as many organisms as possible; “We’ve found a unique haplotype! We must therefore preserve this beetle at all costs!”, as the decapitated beetle floats around the dissection palate..)
How do these concepts relate to fossils?
Every single one of these concepts rely on either direct observational data (e.g., sympatry for the BSC), or the use of DNA. Few modern studies rely solely on morphology to delimit species (annoyingly, seeing as it is directly coupled with behaviour, ecology etc.; DNA is just, well, DNA..). So really, with regards to fossils, in which phenotype is the only aspect preserved (and ecology etc. accordingly inferred), as well as the spatio-temporal context in which it exists, how can these concepts be applied? Well, they can’t really. So what can palaeontologists do..?
How are fossil species delimited?
In principle, there are two different methods of species delimitation: a discovery-based approach, and a hypothesis-based approach. The former makes no a priori assumptions regarding the putative species in a sample, only delimiting subsequent to analysis (e.g., DNA barcoding/taxonomy, cladistics). The latter requires an a priori assumption of what species already exist within a sample, with the analysis being a validation test. It varies in papers as to whether a full or partial cladistic analysis is carried out (if at all) when the focus if the paper is the erection and description of a new species. By partial analysis, I simply mean that the authors observe the synapomorphies of a specific clade and see if their specimen(s) match or not. This is a pretty horrendous breach of taxonomy and cladistic methodology, as it ignores the fact the every single character placement and it’s polarity is influenced by the addition of new species (in fact, this is the principal method by which cladograms are initially constructed). Full analysis is the dominantly used method, thankfully, given the accessibility of free software and relative simplicity in executing cladistic analysis (although there may be issues in obtaining and extracting previous data sets, but that’s another tale too. For someone else.) This leads us on to the next part.
Bring on Cladistics
Cladistics is the method that sytematists use to forge a hierarchical grouping of taxa into discrete subsets, or clades, for the inference of common ancestry between species and groups. A clade is defined by a node (or sometimes a branch) – the point of intersection of two or more branches – that represents the common ancestry and speciation of all subsequent taxa. Each node is represented by one or more shared derived characters (synapomorphies) between all branches, and hence taxa, emanating from the node. If the taxa in question are species (i.e., terminal branches), then the minimum required number of synapomorphies to give a sister taxa relationship is one, and the minimum number of required autapomorphies (unique derived characters) to ‘split’ the branch into two separately recognised entities, is one. That is, cladistics can recognise discrete units, including species, on the basis of a single unique character, regardless of the size of the initial character set. There are statistical methods of assessing the strength or support of this (e.g., pseudo-replication analyses, branch decay tests), but the point remains that a species can be delimited through cladistic analysis based on the possession of a single unique character. [this is a really simple overview, there are numerous web-pages and texts out there that describe cladistic methodology in more detail; just search.]
It seems that there are two main methods of delimiting fossil species: qualitatively, whereby the fossil simply looks different but the differences are not broken down into discrete characters; and quantitatively, where the species name is supported by x number of autapomorphies, and the strength or support of the diagnosis is a function of x, and is testable through cladistic methods. This is pretty much the only method available to palaeontologists given the relative paucity of fossil data. But then how many autapomorphies are required to be interpreted as a ‘strong’, or valid, diagnosis? And to what extent are species therefore comparable? It’s a problematic issue, that I haven’t actually came across much at all in the published literature. If I’m mistaken, please do point me in the right direction! What is perhaps required though, is a rigorous species concept that is directly compatible with the full range of fossil diversity, and that extant taxa can be integrated in to.
One thing to consider though is that species are treated as discrete entities when these concepts are applied; is this the correct approach when really a lineage on which an organism sits is by definition, continuous? What do we gain by stamping an arbitrary and highly subjective boundary on this continuum? A method of classification. It has heuristic value in systematics, but it seems that the fundamental treatment of species as discrete units may need some consideration. Furthermore, speciation is a pretty stochastic and deterministic process, and the application of delimitation criteria must be flexible to account for the variation between lineages. Unless someone comes up with something really neat. Like..
Future prospects? Geometric Morphometrics. 3D automated species recognition software, based on robust statistical delimitation procedures. It’s awesome. Watch this space!
Disclaimer: I’ve probably missed out huge amounts here; this is such a massively studied field, that it’s been difficult to even shrink down to these couple of paltry pages! Comments as always are more than welcome! There are simply too many references to list here too. If people would like to read more about the subject, drop me an email (jon.tenannt.2[at]gmail.com), and I’ll happily whizz a few papers [legally..] your way, depending on taste!
Final thought: with respect to all of the work that has gone into validating ‘species’, what has been done to test the validity of higher taxonomic units, such as Family and Order, or even the Genus..?
For reading all that, here’s a snap of the Iguanodon specimen on display at the museum in Oxford, England.
Higher taxonomic ranks are never comparable between different groups and therefore don’t exist; the only real biological unit is the species. Grab a copy of the Wiley and Lieberman phylogenetics books for a breakdown on the current thought on this sort of thing.
Glad you said that! I hated all these ‘high-impact’ articles of the last few months talking about a ‘burst of family-level diversity’ or whatever nonsense..
How is a species a real biological unit though? I mean, you’ve done loads wrt eurypterids right? How do you rigorously diagnose one species from another..?
Cheers for the book tip! Any chance you know a link where there’s a free pdf..? *empty wallet*
Absolutely agree about this sudden burst of “fill-in-blank-here level of taxa” studies in recent years: like a flashback to the 1970s and ’80s!
Over the last few years I’ve actually become very partial to Darwin’s (often forgotten) species concept: that species were no more or less than well-differentiated varieties distinguished only by the extinction of the gradations intermediate with their closest relatives. (The oft-repeated trope that “Darwin didn’t talk about the origin of species in the Origin of Species” is hogwash; what people really mean is “Darwin didn’t talk about the origin of Mayrian species in the Origin“.
I like that. So, what is and isn’t a species is dependent on the point in time. Meaning that species are useful in [neontological] ecology (and conservation efforts) but virtually useless in paleontology.
Hear hear!
Maxwell (2012) uses morphometric (although not geometric) analyses to quantify variation among a variety of elements (skull, vertebrae, appendicular elements) in a broad selection of specimens from the Posidonia Shale that have been referred to Stenopterygius and Hauffiopteryx, finding four discreet groups, including neonates through adults. She affirms synonymy of several specimens into four species: tricissus, quadricissus and uniter, in Stenopterygius, and typicus in Hauffiopteryx. I wonder why papers that assess quanitiative measures against systematic results receive less attention than systematic results alone, but oh well.
Maxwell, E. E. 2012. New metrics to differentiate species of Stenopterygius (Reptilia: Ichthyosauria) from the Lower Jurassic of southwestern Germany. Journal of Paleontology 86(1):105-115.
Would you be taken with exchanging links? afgdkebbdaec