Journal of Archaeological Science 53 (2015) 291e296 Contents lists available at ScienceDirect Journal of Archaeological Science journal homepage: http://www.elsevier.com/locate/jas On the variable relationship between NISP and NTAXA in bird remains and in mammal remains R. Lee Lyman Department of Anthropology, University of Missouri, Columbia, MO 65211, USA a r t i c l e i n f o a b s t r a c t Article history: Received 23 September 2014 Received in revised form 28 October 2014 Accepted 29 October 2014 It has long been recognized that the minimum number of individuals (MNI) and the number of taxa identified (NTAXA) are both often tightly related to the number of identified specimens (NISP) in a collection. The relationship between NISP and NTAXA has been suggested to vary between bird remains and mammal remains for three reasons that concern the rate at which identifiable skeletal parts of each are input to the zooarchaeological record. Rigorous testing of the relationship using 59 pairs of assemblages of bird and mammal remains confirms that the NTAXA of birds increases more rapidly per NISP than does the NTAXA of mammals per NISP. Data also indicate that two of the three proposed reasons (bird taxa outnumber mammal taxa on the landscape; each mammalian individual contributes more NISP than each avian individual) are the likely causes for intertaxonomic variability in the relationship between NISP and NTAXA. The third reason (fragmentation reduces identifiability of bird remains more rapidly than it does mammal remains) has yet to be empirically evaluated but is logical. © 2014 Elsevier Ltd. All rights reserved. Keywords: Bird remains Mammal remains Number of identified specimens (NISP) Number of taxa (NTAXA) Zooarchaeology 1. Introduction The relationship between the number of identified specimens (NISP) of faunal remains and more derived measures such as the minimum number of individuals (MNI) or number of taxa identified (NTAXA) (also referred to as taxonomic richness) in zooarchaeological collections has been studied for some time (Casteel, 1977; Grayson, 1979, 1981, 1984; Grayson and Frey, 2004; Hesse, 1982; Lyman, 2008). The relationship is usually said to be an expression of the speciesearea relationship (see Lyman and Ames (2007) for discussion), meaning that the more identified bones and teeth (the greater the NISP), or the larger the examined geographic space (which typically results in more specimens encountered and more taxa identified), the larger the value of the derived variable, whether MNI, NTAXA, or something else (e.g., Leonard, 1989; Wolff, 1975). The relationship is thus often interpreted to be a causal one (Casteel, 1977; Grayson, 1984; Hesse, 1982; Klein and Cruz-Uribe, 1984; Lyman, 2008; Reitz and Wing, 1999), with sample size (measured as NISP, volume excavated, or amount of geographic space sampled) being the independent variable and the derived variable being the dependent one. But is the size of the sample the only variable that influences the dependent variable? Grayson (1998), for instance, argued that the E-mail address: [email protected]. http://dx.doi.org/10.1016/j.jas.2014.10.027 0305-4403/© 2014 Elsevier Ltd. All rights reserved. variable relationship between NISP and NTAXA (both log transformed) in multiple sets of data was a result of variation in the rate of input of faunal remains. He inferred that the variability in the relationship ultimately represented variation in climate in one case (Grayson, 1998) and variation in human diet breadth in another (Grayson and Delpech, 1998). Although he provided no empirical test demonstrating that the rate of NISP input in fact influenced NTAXA, Grayson's reasoning in both concerned variables that influenced the rate of input of identifiable skeletal parts per taxon. A greater rate meant a less steep relationship in terms of a simple best-fit regression line between NISP and NTAXA. This reasoning in turn suggests that deep understanding of the relationship between the two variables would be valuable in cases in which NTAXA is an analytically important variable. In this paper, I explore several causes for the relationship between the two variables, focusing particularly on why the relationship between NISP and NTAXA in avian remains tends to be different than that relationship in mammalian remains. 2. Background l (2007) examined the Some years ago Bartosiewicz and Ga statistical relationship between NISP and NTAXA among 35 assemblages of archaeological mammal bones, and 29 assemblages of archaeological bird bones (see also Bartosiewicz et al., 2013). They found that the relationship between NISP and NTAXA differed 292 R.L. Lyman / Journal of Archaeological Science 53 (2015) 291e296 significantly between the two taxonomic groups; the best-fit regression line between the two was steeper for the bird assemblages than it was for the mammal assemblages. They suggested three reasons for that difference, all of which concern the rate of input of NISP to the paleozoological record. First, they observed that there were more avian than mammalian taxa on the landscape for prehistoric people to exploit. They argued that the slope of a regression line between NISP (independent variable) and NTAXA (dependent variable) has the potential to be greater in birds than in mammals because NTAXA is greater in birds than in mammals. l (2007) did not identify a more Although Bartosiewicz and Ga proximate cause for the relationship, such is readily apparent. The greater the number of taxa available, the greater the likely value of the dependent variable (NTAXA) and thus the greater the potential steepness of the relationship between NISP and NTAXA. And, the fewer taxa available, the more constrained and limited the maximum possible NTAXA is and the less steep the possible relationship between NISP and NTAXA. l (2007) observed that birds Second, Bartosiewicz and Ga generally have fewer bones per individual than mammals; in particular, a bird's skeleton includes fewer identifiable bones than does a mammal's skeleton. Thus they argued that it takes fewer bones (less NISP) to make up an individual bird than a mammal in a collection of skeletal remains, so individual bird taxa will be added to the NTAXA of what is in a paleozoological collection more rapidly than mammal taxa will be added. Thus the slope of the relationship between the pair of variables for birds will be steeper than the slope of the relationship between the pair of variables for mammals. And l (2007) suggested that bird bones are third, Bartosiewicz and Ga less likely to break into taxonomically identifiable pieces than mammal bones. More identifiable specimens (bone fragments) per individual mammal therefore means that more skeletal specimens will have to be added to find an additional taxon of mammal than an additional taxon of bird. Whereas the second cause for the difference in the relationship between NISP and NTAXA for birds and that relationship for mammals concerns fewer identifiable skeletal elements in birds, the third cause concerns the fact that fragmentation increases the NISP of mammals more than it does for birds (and may decrease the NISP of birds if bird bones are sufficiently fragmented so as to be unidentifiable (Cannon, 2013)). l (2007) made Twenty-five years before Bartosiewicz and Ga their observations, Hesse (1982) observed that a regression line describing the relationship between NISP and MNI would be steeper the fewer the bone types for a taxon; the regression line would decrease in steepness as the number of identifiable bone l (2007) do types per taxon increased. Although Bartosiewicz and Ga not cite Hesse (1982), Hesse's observation is the same as theirs and concerns the fact that birds have fewer identifiable bones per individual (what Hesse termed the “effective number of elements”) than mammals, and thus the regression line between NISP and MNI (or NTAXA) for birds will be steeper than for mammals. Hesse (1982) used Parmalee's (1977) data for prehistoric avian remains from the North American Great Plains to show the steep relationship between the NISP per bird taxon and the MNI per taxon. The relationship between the log10 values of NISP and MNI making up Parmalee's (1977) data is graphed in Fig. 1 where it can be seen that the relationship is strongly linear (Pearson's r ¼ 0.983) and there are few outliers. The slope of the best-fit linear regression line is relatively steep (slope ¼ 0.84). The same tight linear relationship (Pearson's r ¼ 0.974) is apparent in another set of zooarchaeological collections of avian remains, this one from the North American Great Basin, also identified by Parmalee (1980) (Table 1). The slope of the best-fit regression line (¼ 0.72) is nearly as steep as that for the Great Plains collection, suggesting Hesse's argument is correct. To insure that the relationship between the NISP and MNI of birds is not a function of the individual who did the identifications of the two sets of remains (Parmalee), and not a function of the fact that both collections include remains from multiple sites, consider the NISP and MNI values for the bird remains identified by Emslie (1981) and recovered from the Pottery Mound site in New Mexico (part of the North American Southwest). This collection shows the same tight relationship (Table 1; Pearson's r ¼ 0.928) as the first two and the slope of the best-fit line is steep (¼ 0.537), though not as steep as the first two. In sum the relationship between bird NISP and bird MNI seems to not be a function of who did the identifications, where the remains originated geographically, or whether the collection is made up of remains from multiple sites or from one site. The key question therefore is: Is the relationshipdthe slope of the best-fit regression linedbetween NISP and MNI steeper in birds than in mammals, as predicted by Hesse (1982)? The relationships between NISP and MNI of mammals in three collections are summarized in Table 1, along with those for the three bird collections discussed in the two preceding paragraphs. A graph of one of the mammal assemblages is shown in Fig. 2. In all three cases for mammals, the relationship between NISP and MNI is strong (r 0.86). More importantly, although the range of the slopes of the best-fit regression lines for the three mammal collections overlap slightly with that range for the three bird assemblages (0.607e0.472, and 0.840e0.537, respectively), the average Table 1 Relationships between log10 NISP and log10 MNI in three collections of bird remains, and in three collections of mammal remains. Pearson's r and slope refer to relationship between the log10 of NISP and MNI in each of the six assemblages. Taxa NISP/MNI a Birds Birdsc Birds Mammals Mammals Mammals a Fig. 1. Relationship between NISP and MNI of birds in a set of summed archaeological collections. Data from Parmalee (1977). b c 3029/871 3136/863 3209/236 1822/178 5901/232 6190/209 NTAXA 23 72 53 18 25 22 b Pearson's r Slope Reference 0.981 0.969 0.928 0.961 0.867 0.920 0.840 0.720 0.537 0.607 0.492 0.472 Parmalee 1977 Parmalee 1980 Emslie 1981 Pollock and Ray 1957 Lyman 2008 Lyman 2008 Sum of nine sites. Taxonomic family (not genus/species). Sum of 16 sites. R.L. Lyman / Journal of Archaeological Science 53 (2015) 291e296 293 geographic area. I perform this test because if their reasons for the variable relationship between NISP and NTAXA across taxa hold true (they do), it will be important to understand the implications of those reasons for future analyses and interpretations of zooarchaeological collections. 3. Materials and methods Fig. 2. Relationship between NISP and MNI of mammals in an archaeological site. Data from Lyman (2008). slope for mammals is less than that for birds (0.524 vs 0.699, respectively). This suggests that Hesse (1982) was in fact correct. On average, individuals will be added more quicklydMNI will increase more rapidlydamong collections of bird remains than among collections of mammal remains. But is this in fact because, as Hesse hypothesized, each bird skeleton produces fewer taxonomically identifiable bones than each mammal skeleton? Logic suggests Hesse (1982) is correct. Recall that MNI is defined as the most common skeletal element of a taxon in a collection (Grayson, 1984; Lyman, 2008). MNI will increase more rapidly as the number of kinds of bones that can be identified per individual decreases simply because there are fewer kinds of potentially most abundant elements that might define MNI. If one can identify humeri, radii, femora, and tibiae of taxon A, then there are eight (assuming each element is bilaterally paired as a left and a right) possible kinds of most abundant elements (and each individual animal can contribute eight elements); if one can only identify humeri and femora of taxon B, then there are only four possible kinds of most abundant elements (and each individual animal can contribute only four elements). A random sample of 40 NISP of taxon A is likely to have fewer individuals represented than a random sample of 40 NISP of taxon B simply because there could be 5 of each kind of element of taxon A but 10 of each kind of element of taxon B. Taxon B would thus likely have a higher MNI (per NISP) value than Taxon A. Although Hesse (1982) was concerned with the relationship between NISP and MNI, the logic behind his discussion is the same l (2007) with respect to the as that used by Bartosiewicz and Ga relationship between NISP and NTAXA. The similarity between the two resides in the fact that both concern the potential (and likely) rate of input of identifiable specimens (partially dependent on the number in an individual skeleton) to the paleozoological record. As l (2007) suggested three reasons noted earlier, Bartosiewicz and Ga why the relationship between NISP and NTAXA would differ between birds and mammals, and they presented data suggesting each reason was valid. Below I use another data set to test the validity of two of the reasons. I examine the relationship between NISP and NTAXA in birds and in mammals by performing a more l's observations than they rigorous test of Bartosiewicz and Ga originally provided. Greater rigor comes from my use of a greater number of samples for each taxon, greater taphonomic control of the samples, and my samples originate in a different and larger Bartosiewicz and G al (2007) used 35 prehistoric assemblages of mammal remains and 29 prehistoric avian assemblages. All of the assemblages they included originated in Hungary, but apparently at least some of the collections of birds and mammals did not originate in the same site or deposit. That is, each assemblage of bird remains did not necessarily have an associated assemblage of mammal remains from the same deposit. This is an important consideration with respect to taphonomic influences on the collections of bones available and also on what could be identified. I control for this here by including an assemblage of bird remains only if it has an associated assemblage of mammal remains on the assumption that bird and mammal remains from the same deposit were subjected to similar diagenetic (if not biostratinomic) histories. In other words, each of the 59 assemblages of bird remains has an associated assemblage of mammal remains; each pair of assemblages was recovered from the same deposit in a site. Of course, taphonomic histories may also vary from site to site and deposit to deposit. To contend with this possibility, I use numerous assemblages from varied depositional settings such that a great deal of variability in taphonomic histories is included. In doing so, I assume the large number of collections will mute any potential taphonomic skewing of results emanating from one or a few assemblages. Taphonomic histories may also vary intertaxonomically given differences between skeletons at the level of taxonomic class (Aves, Mammalia). This is in fact an issue here, particularly with respect to the influence of fragmentation on identifiability. As noted above, l (2007) suggested fragmentationda taphoBartosiewicz and Ga nomic resultdreduced identifiability of bird remains more rapidly than a similar degree of fragmentation reduced the identifiability of mammal remains. If so, this would enhance the differences between the relationship of NISP to NTAXA for bird remains and that relationship for mammal remains. As indicated below, I cannot directly assess the influence of fragmentation among the collections I use in the analyses for want of data. Instead, I assume that the large number of assemblages included will mute any skewing and taphonomic biases. Specifically, I find it unlikely that all the included avian assemblages will be significantly more fragmented (and thus have fewer identifiable specimens per taxon) than all of the included mammalian assemblages. All collections date to the Holocene, and all come from North America (Supplementary Table 1). The assemblages originate in Arizona (2), Arkansas (1), Florida (2), Illinois (9), Indiana (2), Michigan (6), Minnesota (3), Missouri (9), Nevada (3), New Mexico (8), South Carolina (1), South Dakota (1), Tennessee (4), Utah (1), Wisconsin (5), Alberta (1) and Manitoba (1). Twenty-three analysts identified the remains making up one or more of the collections and wrote the reports. In some cases an analyst identified both the bird and the mammal remains; in a few cases one analyst identified the bird remains and another analyst identified the mammal remains. I believe that the analysts involved have not influenced in a consistent or patterned way the relationship between NISP and NTAXA across all 59 assemblages of either the birds or the mammals. My belief rests on the fact that multiple researchers identified the remains, and in some cases the same researcher identified both the bird and mammal remains. Had one set of analysts identified the bird remains and another had identified the mammal remains, 294 R.L. Lyman / Journal of Archaeological Science 53 (2015) 291e296 then there would be cause for concern that any difference in the relationship between NISP and NTAXA for birds relative to that for mammals might be a function of the analysts involved. I tallied NISP and NTAXA for birds and for mammals for each assemblage. Only unique taxa were included; for example, if both the subfamily Anatinae (ducks) and its included genus Anas sp. were listed (not unusual), only data for the latter were recorded. If some specimens were identified as, say, “dog or coyote; Canis familiaris or Canis latrans” and other specimens were identified as either or both of these species, only data for the latter were recorded. This protocol insured that taxa were not counted twice and thus did not artificially increase NTAXA. In some cases, NTAXA of an assemblage might be slightly decreased by tallying, say, only Canis sp. in one assemblage (NTAXA ¼ 1) and tallying C. latrans and C. familiaris in another assemblage (NTAXA ¼ 2). I presume such instances are too few to exert a strong influence on analytical results. The NISP of bird remains across the 59 assemblages ranges from 4 to 4988 and averages 354; the NTAXA of birds per assemblage ranges from 3 to 59 and averages 18.2. The NISP of mammal remains across the 59 assemblages ranges from 23 to 18,376 and averages 2158; the NTAXA of mammals per assemblage ranges from 5 to 45 and averages 18.8. Forty percent (73 of 181 species) of the bird taxa occur in only one assemblage and 63.5% (115 of 181) occur in three or fewer assemblages. This is in stark contrast to mammalian taxa of which only 22.6% (28 of 124 species) occur in only one assemblage and 46.0% (57 of 124) occur in three or fewer assemblages. The turkey (Meleagris gallopavo) and Canada goose (Branta canadensis) are the most ubiquitous bird species, occurring in 43 and 42 assemblages, respectively. Deer (Odocoileus virginianus/hemionus) and domestic dogs (C. familiaris) are the most ubiquitous mammals species, occurring in 56 and 43 assemblages, respectively. 4. The relationship of NISP to NTAXA in birds and in mammals l (2007) showed that there were more bird Bartosiewicz and Ga than mammal species in the archaeological collections they examined, just as was found on the modern landscape. According to the Audobon Society, today there are more than 800 species of birds in North America north of Mexico (birds.audubon.org/birdid; Table 2 Avian skeletal elements illustrated in osteology guidesa and identified in a zooarchaeological reportb. þ Indicates skeletal element is illustrated or identified. Skeletal element (N) Olsen 1972, 1979a Skull (1) Mandible (1) Coracoid (2) Furculum (1) Sternum (1) Scapula (2) Humerus (2) Radius (2) Ulna (2) Carpometacarpus (2) First phalanx, 2nd digit (2) Pelvis/Synsacrum (1) Femur (2) Fibula (2) Tibiotarsus (2) Tarsometatarsus (2) Terminal foot phalanx (3) SUM þ þ þ þ þ þ þ þ þ þ 17 Gilbert et al. 1981a þ þ þ þ þ þ þ þ þ þ þ þ þ þ 26 Broughton 2004b þ þ þ þ þ þ þ þ þ þ þCarpal digit 2 þ þ þ þ þ 30 accessed Aug. 27, 2014). Today there are 462 species of mammals known in North America north of Mexico (Kays and Wilson, 2009). The number of distinct species identified in the 59 North American samples of archaeological bird remains (N ¼ 181) is greater than the number of distinct species identified in the 59 North American samples of archaeological mammal remains (N ¼ 124). If Bartosiewicz and G al (2007) are correct in their surmise, the difference in taxonomic richness between North American birds and mammals suggests the regression line between bird NISP and bird NTAXA in the 59 North American assemblages should be steeper than the regression line between mammal NISP and mammal NTAXA. l (2007) and Hesse (1982) indicated Both Bartosiewicz and Ga that the number of identifiable bones per individual skeleton is less in a bird than in a mammal. That this is in fact so is easily demonstrated in two ways. First, the number of kinds of skeletal elements illustrated and described in zooarchaeological osteology identification manuals tends to be greater for mammals than for birds. For birds, the number is 17e26 (Table 2). The number is difficult to estimate for mammals given that different taxa have different numbers of teeth, metapodials, and the like. Conservatively, the number of mammal skeletal elements illustrated and described in skeletal guides is 53e83 (Table 3). Second, the number of kinds of skeletal elements (ignoring whether identified specimens are fragments or anatomically complete skeletal elements) identified in a large collection of archaeological bird remains (N ¼ 30) is smaller than the number of kinds of skeletal elements identified in a large collection of archaeological mammal remains (N ¼ 116) (Tables 2 and 3). These two observations suggest, just as l (2007) proposed, that the regression line Bartosiewicz and Ga between bird NISP and bird NTAXA for the 59 North American assemblages will be steeper than the regression line between mammal NISP and mammal NTAXA in those assemblages. l (2007) suggested that the greater Finally, Bartosiewicz and Ga degree of identifiability of fractured (anatomically incomplete) mammal bones relative to the identifiability of fractured bird bones Table 3 Mammalian skeletal elements illustrated in zooarchaeology osteology guidesa and identified in a zooarchaeological reportb. þ Indicates skeletal element is illustrated or identified. Skeletal element Olsen 1964a Gilbert 1990a Grayson 1988b Skull (1) Mandible (2) Teeth (16e40) Atlas (1) Axis (1) Cervical 3e7 (5) Thoracic (13) Lumbar (6e7) Clavicle (2) Sacrum (1) Scapula (2) Humerus (2) Radius (2) Ulna (2) Carpals (12) Metacarpals (2e10) Innominate (2) Femur (2) Tibia (2) Fibula (2) Astragalus (2) Calcaneum (2) Other tarsals (2e4?) Metatarsal (2e10) Phalange (24e60) SUM þ þ þ þ þ þ þ þ þ þ þ þ þ þ þ þ þ þ þ þ þ þ þ þ þ þ þ þ þ þ þ þ þ ~116 þ þ þ þ þ þ þ þ þ þ þ þ þ þ þ þ þ þ þ þ ~53 þ þ ~83 R.L. Lyman / Journal of Archaeological Science 53 (2015) 291e296 results in a generally greater ratio of NISP:NTAXA for mammal remains than for bird remains. This suggestion cannot be empirically evaluated with the 59 North American collections because fragmentation data for them are unavailable. This is not, however, a serious drawback because fragmentation will increase the NISP but not the NTAXA for both birds and mammals. If bird bones more rapidly become less identifiable with greater intensity of fragmentation than mammal bones, as suggested by Bartosiewicz and l (2007), then the effect on the relationship between NISP and Ga NTAXA of mammals will be to make the regression line steeper for birds than for mammals because there will be a lower rate of input of bird NISP per taxon than that rate for mammals. l's (2007) and Hesse's (1982) In light of Bartosiewicz and Ga reasoning, and given the three reasons for the relationship between NISP and NTAXA, the slope of the best-fit regression line between the NISP and NTAXA of birds should be steeper than the slope of the line between the NISP and NTAXA of mammals. That is in fact precisely what is observed both graphically (Fig. 3) and statistically for the 59 North American assemblages. The slope of the best-fit linear regression line for birds is 0.409, and for mammals is 0.241. In both cases, the correlation of the two variables is high, although it is higher for birds (r ¼ 0.841) than it is for mammals (r ¼ 0.773). Thus variability in bird NISP explains almost 71% of the variability in NTAXA of birds whereas variability in mammal NISP explains only 60% of the variability in NTAXA of mammals. This is not unexpected either given that there are many more kinds of bones that can be identified per individual of a mammal taxon than there are kinds of bones that can be identified per individual of a bird taxon. 5. Discussion The preceding provides a more rigorous test of Bartosiewicz and l's (2007) observations than they originally did for three reasons. Ga First, taphonomy is more tightly controlled by using 59 pairs of bird and mammal assemblages, each pair recovered from the same deposits or sites. Taphonomic, particularly diagenetic, differences between deposits containing bird remains and those containing mammal remains that might influence the relationship of NISP to NTAXA are not possible. Second, the test described here is more rigorous and more statistically powerful because a larger number of assemblages for both taxa is used. And third, the assemblages I have used derive from a larger geographic area and thus provide the potential for a much greater suite of taxa and of taphonomic Fig. 3. Relationship between NISP and NTAXA in 59 zooarchaeological assemblages of bird bones, and in 59 zooarchaeological assemblages of mammal bones. 295 processes to influence both NISP and NTAXA. The analysis presented above therefore lends considerable strength to Bartosiewicz and G al's observations, and it also indicates that those observations are very likely universal. But, one might ask, so what? In particular, l's obserof what analytical significance are Bartosiewicz and Ga vations? There are several responses to these questions. Recall that I began with the observation that NTAXA was (and is) often a function of NISP. The general cause of the relationship is clear: as sample size (NISP) increases, so too does NTAXA. But, l (2007) importantly, Hesse (1982) and Bartosiewicz and Ga observed that the relationship differs inter-taxonomically, at least at the level of taxonomic class. In other words, the precise nature of the relationship between NISP and NTAXA depends in part on sample size and also in part on the particular taxa. One implication of this observation concerns the fact that archaeologists and paleontologists sample deposits (e.g., Krumbein, 1965; Orton, 2000). They are aware of the influences of sample size on derived measures such as NTAXA and sometimes use techniques such as rarefaction to control variability in sample sizes across multiple samples (e.g., Barnosky et al., 2005; Lyman, 2014). Comparison of a rarefaction curve for an assemblage of birds with a rarefaction curve for mammals would, in light of Fig. 3, be unwise. In addition, paleozoologists do not always rarify collections yet continue to determine NTAXA (biodiversity), evenness and heterogeneity as measures of dietary breadth among prehistoric humans (e.g., selected references in Lupo, 2007) or some aspect of paleoecology (e.g., Barnosky et al., 2005; Faith, 2011). The implication of Fig. 3 is that if the taxa included in the analyses vary in such a way as to influence the relationship between NISP and NTAXA (e.g., number of effective elements per taxon), comparing, say, the NTAXA of birds with the NTAXA of mammals would be unwise. Previously, one might argue that the indices could be compared if the samples upon which they were based were similar in size. Fig. 3 indicates that even if the sample of bird remains is the same size as the sample of mammal remains, differences in richness are to be expected simply because fewer bones are required to produce a particular NTAXA value for birds than are required to produce that same NTAXA for mammals. A second implication concerns the influence of the number of kinds of skeletal elements (or fragments thereof) that can be identified per taxon. For example, if all the skeletal elements listed in Table 3 are identified for one collection or taxon but only, say, mandibles, maxillae and teeth are identified for another collection or taxon, then, as noted in the immediately preceding paragraph, indices of faunal structure such as NTAXA, evenness, and heterogeneity for those two faunas can only be compared with explicit recognition that those taxon free indices will be differentially influenced by the rate of skeletal part input. Paleozoologists have long been aware of this pitfall, expressing it as the lack of comparability of taxonomic abundances determined on the basis of taxa with different numbers of identifiable bones per taxon or different degrees of fragmentation of bones per taxon (e.g., Chaplin, 1971; Holtzman, 1979; Shotwell, 1955, 1958). The potential magnitude of the effect is clearly demonstrated in Fig. 3. A potentially important follow-up study along lines similar to the study reported here would involve generating a graph like that in Fig. 3 comparing the relationships between the NISP and NTAXA of rodentsdof which teeth, skulls, and mandibles are typically the elements identifieddwith that for artiodactylsdof which nearly all teeth and bones, cranial and post-cranial, are identified. Finally, given the variable relationships shown in Fig. 3 both between birds and mammals and within birds and mammals, the issue of how large a representative sample must be is underscored. The scatterplots in Fig. 3 emphasize that the relationship of NISP and NTAXA varies considerably (the data points fall various 296 R.L. Lyman / Journal of Archaeological Science 53 (2015) 291e296 distances from the best-fit regression line) for a number of reasons. This makes a standard representative sample size for all collections impossible to determine because it is quite improbable. Sampling to redundancy (Lyman and Ames, 2004, 2007) is a logical technique for monitoring sample adequacy or representativeness because it is case specific and can (and should) be empirically determined on a case-by-case basis. 6. Conclusion In the few studies of which I am aware wherein the varied relationships between NISP and NTAXA across multiple assemblages are interpreted to signify changes in climate (Faith, 2011; Grayson, 1998; Lyman, 2012, 2014) or changes in human diet breadth (Grayson and Delpech, 1998), the variable relationship is said to be a function of varied rates of skeletal part input. Those interpretations have a firm foundation because data and analyses presented here show that the relationship between NISP and NTAXA is indeed influenced by the rate of skeletal part input. And we now know that rate is determined by such things as taxonomic richness on the landscape and the effective number of elements (to borrow Hesse's (1982) term) per taxon, both the number of identifiable bones in an individual and the number of identifiable fragments into which the bones of a skeleton can be broken. The rarity with which knowledge of the varied relationship between NISP and NTAXA has been used to solve analytical problems suggests that we still have a lot to learn about the basic quantitative units that underpin much zooarchaeological analysis (Grayson, 1984; Lyman, 2008). Increased computing power and greater access to large data sets will facilitate meta-analyses that should be directed toward revealing new aspects of the relationships between zooarchaeological variables as well as enhancing our understanding of known relationships. Greater knowledge and understanding should result in more refined and insightful analyses and interpretations. Acknowledgments This analysis grew from my chance reading of the thoughtful 2007 paper by Bartosiewicz and G al. The comments of two anonymous reviewers were helpful. Appendix A. Supplementary data Supplementary data related to this article can be found at http:// dx.doi.org/10.1016/j.jas.2014.10.027. References Barnosky, A.D., Carrasco, M.A., Davis, E.B., 2005. The impact of the species-area relationship on estimates of biodiversity. PLoS Biol. 3, 1356e1361. l, E., 2007. Sample size and taxonomic richness in mammalian Bartosiewicz, L., Ga and avian bone assemblages from archaeological sites. Archeometriai Mühely 2007 (1), 37e44. Bartosiewicz, L., G al, E., Kov acs, Z.E., 2013. Domesticating mathematics: taxonomic diversity in archaeozoological assemblages. In: Anders, A., Kulcs ar, B. (Eds.), l Raczky on His 60th Birthday. Moments in Time: Papers Presented to Pa € e ge szeti Ta rsas € tvo €s Lora nd University, Budapest, Osr ag (Prehistoric Society), Eo pp. 853e862. Broughton, J.M., 2004. Prehistoric Human Impacts on California Birds: Evidence from the Emeryville Shellmound Avifauna. Ornithological Monographs No. 56. American Ornithologists' Union, Washington, DC. Cannon, M.D., 2013. NISP, bone fragmentation, and the measurement of taxonomic abundance. J. Archaeol. Method Theory 20, 397e419. Casteel, R.W., 1977. A consideration of the behavior of the minimum number of individuals index: a problem in faunal characterization. Ossa 3 (4), 141e151. Chaplin, R.E., 1971. The Study of Animal Bones from Archaeological Sites. Seminar Press, London. Emslie, S.D., 1981. Prehistoric agricultural ecosystems: avifauna from Pottery Mound. N. M. Am. Antiq. 46, 853e861. Faith, J.T., 2011. Ungulate community richness, grazer extinctions, and human subsistence behavior in southern Africa's cape floral region. Palaeogeog. Palaeoclimatol. Palaeoecol. 306, 219e227. Gilbert, B.M., 1990. Mammalian Osteology. Missouri Archaeological Society, Columbia. Gilbert, B.M., Martin, L.D., Savage, H.G., 1981. Avian Osteology. Privately published, Laramie, Wyoming. Grayson, D.K., 1979. On the quantification of vertebrate archaeofaunas. In: Schiffer, M.B. (Ed.), Advances in Archaeological Method and Theory, vol. 2. Academic Press, New York, pp. 199e237. Grayson, D.K., 1981. The effects of sample size on some derived measures vertebrate faunal analysis. J. Archaeol. Sci. 8, 77e88. Grayson, D.K., 1984. Quantitative Zooarchaeology: Topics in the Analysis of Archaeological Faunas. Academic Press, Orlando, FL. Grayson, D.K., 1988. Danger cave, last supper cave, and hanging rock shelter: the faunas. Am. Mus. Nat. Hist. Anthropol. Pap. 66 (1). Grayson, D.K., 1998. Moisture history and small mammal community richness during the latest Pleistocene and Holocene, northern Bonneville Basin, Utah. Quat. Res. 49, 330e334. Grayson, D.K., Delpech, F., 1998. Changing diet breadth in the early Upper Paloelithic of southwestern France. J. Archaeol. Sci. 25, 1119e1129. Grayson, D.K., Frey, C.J., 2004. Measuring skeletal part representation in archaeological faunas. J. Taphon. 2, 27e42. Hesse, B., 1982. Bias in the zooarchaeological record: suggestions for interpretation of bone counts in faunal samples from the Plains. In: Ubelaker, D.H., Viola, H.J. (Eds.), Plains Indian Studies: a Collection of Essays in Honor of John C. Ewers and Waldo R. Wedel, pp. 157e172. Smithsonian Contributions to Anthropology No. 20. Holtzman, R.C., 1979. Maximum likelihood estimation of fossil assemblage composition. Paleobiol 5, 77e90. Kays, R.W., Wilson, D.E., 2009. Mammals of North America, second ed. Princeton University Press, Princeton, NJ. Klein, R.G., Cruz-Uribe, K., 1984. The Analysis of Animal Bones from Archeological Sites. University of Chicago Press, Chicago. Krumbein, W.C., 1965. Sampling in paleontology. In: Kummel, B., Raup, D. (Eds.), Handbook of Paleontological Techniques. W.H. Freeman and Co., San Francisco, pp. 137e150. Leonard, R.D., 1989. Anasazi Faunal Exploitation: Prehistoric Subsistence on Northern Black Mesa, Arizona. Center for Archaeological Investigations Occasional Paper No. 13. Southern Illinois University, Carbondale. Lupo, K.D., 2007. Evolutionary foraging models in zooarchaeological analysis: recent applications and future challenges. J. Archaeol. Res. 15, 143e189. Lyman, R.L., 2008. Quantitative Paleozoology. Cambridge University Press, Cambridge. Lyman, R.L., 2012. Biodiversity, paleozoology, and conservation biology. In: Louys, J. (Ed.), Paleontology in Ecology and Conservation. Springer-Verlag, Berlin, pp. 147e169. Lyman, R.L., 2014. Terminal Pleistocene change in mammal communities in southeastern Washington State, USA. Quat. Res. 81, 295e304. Lyman, R.L., Ames, K.M., 2004. Sampling to redundancy in zooarchaeology: lessons from the Portland Basin, northwestern Oregon and southwestern Washington. J. Ethnobiol. 24, 329e346. Lyman, R.L., Ames, K.M., 2007. On the use of species-area curves to detect the effects of sample size. J. Archaeol. Sci. 34, 1985e1990. Olsen, S.J., 1964. Mammal remains from archaeological sites, Part IdSoutheastern and southwestern United States. Pap. Peabody Mus. Archaeol. Ethnol. 56 (1). Olsen, S.J., 1972. Osteology for the archaeologist: North American birds: skulls and mandibles. Pap. Peabody Mus. Archaeol. Ethnol. 56 (4). Olsen, S.J., 1979. Osteology for the archaeologist: North American birds: postcranial skeletons. Pap. Peabody Mus. Archaeol. Ethnol. 56 (5). Orton, C., 2000. Sampling in Archaeology. Cambridge University Press, Cambridge. Parmalee, P.W., 1977. The avifauna from prehistoric Arikara sites in South Dakota. Plains Anthropol. 22, 189e222. Parmalee, P.W., 1980. Utilization of birds by the Archaic and Fremont cultural groups of Utah. Natural history museum of Los Angeles County. Contributions Sci. 330, 237e250. Pollock, H.E.D., Ray, C.E., 1957. Notes on Vertebrate Remains from Mayapan. Current Reports 41. Carnegie Institute, Department of Archaeology, Washington, pp. 633e656. Reitz, E.J., Wing, E.S., 1999. Zooarchaeology. Cambridge University Press, Cambridge. Shotwell, J.A., 1955. An approach to the paleoecology of mammals. Ecology 36, 327e337. Shotwell, J.A., 1958. Inter-community relationships in Hemphillian (mid-Pliocene) mammals. Ecology 39, 271e282. Wolff, R.G., 1975. Sampling and sample size in ecological analyses of fossil mammals. Paleobiology 1, 195e204.
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