2. A bit of sensational science

In 1980, half of an archaic hominin mandible was discovered by a local (Xiahe county) monk in Baishiya Karst Cave (altitude 3,280 meters high, located on the Tibetan Plateau).Footnote ⁹ Later that decade, the bone was transferred to nearby Lanzhou University by a regional religious leader (Jigme Tenpai Wangchuk, the Sixth Gung-Thang Lama, a Living Buddha).Footnote ¹⁰ The partial humanoid jawbone included two molars of unusual shape and size. Because teeth are often preserved when other animal body parts are not, there is a relatively extensive paleontological record of fossil dentition, and fossil experts (paleontologists and paleoanthropologists alike) tend to recognize teeth. It is notable when they do not, so, this particular specimen was neither filed as familiar nor discarded, but rather sat unclassifiable in an ancillary collection at Lanzhou University for nearly thirty years.

In 2008, a fragment of the tip of an archaic juvenile hominin pinky finger bone (in technical terms, a fifth digit distal manual phalanx) was uncovered in Denisova Cave (altitude 700 meters high, located in the Altai mountains of Siberia). Researchers from the Institute of Archeology and Ethnography of the Siberian Division of the Russian Academy of Sciences in Novosibirsk have been excavating at Denisova Cave annually since the early 1980s (Serdyuk Reference Serdyuk2001). The presence of both Levallois and Mousterian stone tools, evidence of butchery and fire use, plus the excavation of human and nonhuman animal fossils all indicate that hominin use and perhaps occupancy of the cave might have begun by the end of the Middle Pleistocene, but was certainly in place by the beginning of the Late Pleistocene (Derevianko et al. Reference Derevianko, Postnov, Rybin, Kuzmin and Keates2005). In other words, Denisova Cave has likely been a site of hominin activity since sometime between 282,000 and 126,000 years ago.

The cave has an entrance zone, a large main chamber, and two narrow offshoots dubbed the East and South Galleries.Footnote ¹¹ Until 1999, excavations were performed only in the central part of the cave (Serdyuk Reference Serdyuk2001) and occasionally the entrance zone (Malaeva Reference Malaeva1998, cited in Rossina Reference Rossina2006). Published descriptions of hominin remains discovered in the cave began to appear by the early 2000s (i.e., Shpakova and Derevianko Reference Shpakova and Derevianko2000, but it was not until these remains became an object of study by molecular geneticists working on ancient DNA that the site gained the widespread notoriety it has today. Reportedly, it was dig leader Anatoly Derevianko who, in 2008, decided to take the fingertip discovered at the site, split it, and send the pieces to two competing ancient DNA labs “to see whether DNA could be extracted from either half” (Callaway Reference Callaway2019, 176).Footnote ¹²

Some biological molecules last longer and age better than others. Certain pigments can apparently last for hundreds of millions of years (e.g., Tanaka et al. Reference Tanaka, Parker, Hasegawa, Siveter, Yamamoto, Miyashita, Takahashi, Ito, Wakamatsu, Mukuda, Matsuura, Tomikawa, Furutani, Suzuki and Maeda2014), but DNA usually degrades within 60,000 years (barring special circumstances, such as low temperatures [Briggs and Summons Reference Briggs and Summons2014]). It is not known why the fragment of pinky finger bone unearthed in 2008 was preserved like a specimen in permafrost,Footnote ¹³ but in April 2010, researchers from the Max Planck Institute for Evolutionary Anthropology in Leipzig, Germany, announced the sequencing (with high coverage—mean 156, low 2, high 602Footnote ¹⁴ ) of a complete mitochondrial genome from “the Denisova hominin” (Krause et al. Reference Krause, Fu, Good, Viola, Shunkov, Derevianko and Pääbo2010).Footnote ¹⁵ By December 2010, a full-length article in Nature Footnote ¹⁶ announced the draft sequencing (with much lower 1.9-fold coverage) of a Denisovan nuclear genome, as well as the complete sequencing (mean 58-fold coverage) of another Denisovan mitochondrial genome (Reich et al. Reference Reich, Green, Kircher, Krause, Patterson, Durand, Viola, Briggs, Stenzel, Johnson, Maricic, Good, Marques-Bonet, Alkan, Fu, Mallick, Li, Meyer, Eichler, Stoneking, Richards, Talamo, Shunkov, Derevianko, Hublin, Kelso, Slatkin and Pääbo2010).Footnote ¹⁷ On this basis, a new population of archaic hominins was declared discovered—a population that might have lived contemporaneously with both Neanderthals and anatomically modern humans, in some parts of Eurasia at least.

Over the next decade, additional details about Denisovan genetic characteristics and evolutionary history were frequently published in high-impact scientific venues and were usually accompanied by significant press coverage. A follow-up piece on the same Denisovan nuclear genome (but with better 31-fold coverage) was published in Science in October 2012 (Meyer et al. Reference Meyer, Kircher, Gansauge, Li, Racimo, Mallick, Schraiber, Jay, Prüfer, de Filippo, Sudmant, Alkan, Fu, Do, Rohland, Tandon, Siebauer, Green, Bryc, Briggs, Stenzel, Dabney, Shendure, Kitzman, Hammer, Shunkov, Derevianko, Patterson, Andrés, Eichler, Slatkin, Reich, Kelso and Pääbo2012). In January 2014, another paper was published in Nature about the sequencing of a bone fragment which was initially thought to be Denisovan, but then turned out to be Neanderthal instead (Prüfer et al. Reference Prüfer, Racimo, Patterson, Jay, Sankararaman, Sawyer, Heinze, Renaud, Sudmant, Filippo, Li, Mallick, Dannemann, Fu, Kircher, Kuhlwilm, Lachman, Meyer, Ongyerth, Siebauer, Theunert, Tandon, Moorjani, Pickrell, Mullikin, Vohr, Green, Hellmann, Phillip, Blanche, Cann, Kitzman, Shendure, Eichler, Lein, Bakken, Golovanova, Doronichev, Shunkov, Derevianko, Viola, Slatkin, Reich, Kelso and Pääbo2014).Footnote ¹⁸ A rather comprehensive article comparing sequenced mitochondrial and nuclear genomes from multiple Denisovan and other archaic hominin individuals was published in PNAS in December 2015 (Sawyer et al. Reference Sawyer, Renaud, Viola, Hublin, Gansuage, Shunkov, Derevianko, Prüfer, Kelso and Pääbo2015).Footnote ¹⁹ In March 2016, it was announced that 2,315 previously unidentifiable bone fragments from Denisova Cave had been analyzed for species membership via the method of collagen peptide mass fingerprinting (known as ZooMS)—revealing one hominin sample (DC 1227) tagged as Neanderthal via mitochondrial DNA analysis (Brown et al. Reference Brown, Higham, Slon, Pääbo, Meyer, Douka, Brock, Comeskey, Procopio, Shunkov, Derevianko and Buckley2016).Footnote ²⁰ But in September 2018, another Nature paper announced that the nuclear genome sequenced from this individual revealed a significant share of Denisovan ancestry, thereby revealing that a hybrid offspring with a Neanderthal mother and a Denisovan father had been discovered (Slon et al. Reference Slon, Majessoni, Vernot, de Filippo, Grote, Viola, Hajdinjak, Peyrégne, Nagel, Brown, Douka, Higham, Kozlikin, Shunkov, Derevianko, Kelso, Meyer, Prüfer and Pääbo2018). This individual is frequently called “Denny” in the press. Denny is a sliver of bone about two and a half centimeters long and less than a centimeter wide.

In July 2017, in between publication of these two papers on the hybrid specimen, another relevant report was published: one announcing the sequencing of the mitochondrial genome plus nuclear DNA fragments from what was at that point in time only the fourth Denisovan individual known to science (Slon et al. Reference Slon, Viola, Renaud, Gansauge, Benazzi, Sawyer, Hublin, Shunkov, Derevianko, Kelso, Prüfer, Meyer and Pääbo2017).Footnote ²¹ Until early 2019, all known samples of purportedly Denisovan remains came from just the one spot in the Altai Mountains of southern Siberia. But in May 2019, what is now known as the Xiahe Mandible—that partial jawbone discovered in 1980 on the Tibetan Plateau in Baishiya Karst Cave—was declared, on the basis of ancient protein analysis, to be Denisovan as well, or “closely related” (Chen et al. Reference Chen, Welker, Shen, Bailey, Bermann, Davis, Xia, Wang, Fischer, Freidline, Yu, Skinner, Stelzer, Dong, Fu, Dong, Want, Zhang and Hublin2019).Footnote ²²

Please see Table 1 for a detailed list of the Denisovan specimens, with associated archaeological and genetic information.

Table 1. Each specimen name is accompanied by citation of the article in which that specimen is first declared Denisovan. Citations in other columns indicate the source of information being given.

Sources are as follows: a = Krause et al. (Reference Krause, Fu, Good, Viola, Shunkov, Derevianko and Pääbo2010); b = Reich et al. (Reference Reich, Green, Kircher, Krause, Patterson, Durand, Viola, Briggs, Stenzel, Johnson, Maricic, Good, Marques-Bonet, Alkan, Fu, Mallick, Li, Meyer, Eichler, Stoneking, Richards, Talamo, Shunkov, Derevianko, Hublin, Kelso, Slatkin and Pääbo2010); c = Meyer et al. (Reference Meyer, Kircher, Gansauge, Li, Racimo, Mallick, Schraiber, Jay, Prüfer, de Filippo, Sudmant, Alkan, Fu, Do, Rohland, Tandon, Siebauer, Green, Bryc, Briggs, Stenzel, Dabney, Shendure, Kitzman, Hammer, Shunkov, Derevianko, Patterson, Andrés, Eichler, Slatkin, Reich, Kelso and Pääbo2012); d = Sawyer et al. (Reference Sawyer, Renaud, Viola, Hublin, Gansuage, Shunkov, Derevianko, Prüfer, Kelso and Pääbo2015); e = Brown et al. (Reference Brown, Higham, Slon, Pääbo, Meyer, Douka, Brock, Comeskey, Procopio, Shunkov, Derevianko and Buckley2016); f = Slon et al. (Reference Slon, Viola, Renaud, Gansauge, Benazzi, Sawyer, Hublin, Shunkov, Derevianko, Kelso, Prüfer, Meyer and Pääbo2017); g = Slon et al. (Reference Slon, Majessoni, Vernot, de Filippo, Grote, Viola, Hajdinjak, Peyrégne, Nagel, Brown, Douka, Higham, Kozlikin, Shunkov, Derevianko, Kelso, Meyer, Prüfer and Pääbo2018); h = Chen et al. (Reference Chen, Welker, Shen, Bailey, Bermann, Davis, Xia, Wang, Fischer, Freidline, Yu, Skinner, Stelzer, Dong, Fu, Dong, Want, Zhang and Hublin2019); i = Jacobs et al. (Reference Jacobs, Li, Shunkov, Kozlikin, Bolikhovskaya, Agadjanian, Uliyanov, Vasiliev, O’Gorman, Derevianko and Roberts2019). Abbreviations are as follows: E = East Gallery; EQV = equivalent; INC = incomplete; ka = thousand years ago; kyr = thousand years; M = Main Chamber; Mb = million base pairs; mt = mitochondrial; n = nuclear; N/A = no such information available; S = South Gallery.

3. The state of uncertain play

Already, this is an exciting story. Forty years ago, a monk finds a jawbone in a cave high up on the Tibetan Plateau. A long way away, in Siberia, another cave is painstakingly excavated for decades before a striking discovery is made. A pinky bone is preserved as though in permafrost and pristine DNA is unexpectedly extracted. A new group of archaic hominins is announced, one that potentially co-existed and even bred with us deep in our evolutionary past. And the link between the specimens from the two quite-distant caves implies that a previously unknown but surprisingly pervasive and far-flung population of these archaic hominins once existed. Not just the narrative but the science is exciting, too: after a tumultuous origin mired in technical difficulties, the field of ancient DNA re-emerges triumphant and with a focus on human evolutionary history (see Stoneking and Krause [Reference Stoneking and Krause2011] for a scientific review; Jones [Reference Jones2019] for an historical one; or Lewis-Kraus [Reference Lewis-Kraus2019] for a journalistic one). Not every subject of scientific study produces a rapid succession of papers so frequently published in the likes of Nature, PNAS, and Science. In short, this is science on the edge—the technical cutting edge, putting us on the edge of our seats, and peering over the edge of what is known into the unknown.

With such excitement and innovation comes speculation and uncertainty. In 2011, Ewen Callaway writes a news item for Nature called “Ancient DNA Reveals Secrets of Human History” (Reference Callaway2011). Callaway gushes that “scientists are racing to apply the work to answer questions about human evolution and history that would have been unfathomable just a few years ago” (136), and Svante Pääbo is quoted at the end of the article: “Maybe we should write a little booklet called archaic genomics for dummies” (137). A little over two years later, however, Callaway writes another news item for Nature, this one entitled “Hominin DNA Baffles Experts” (Reference Callaway2013). It begins “another ancient genome, another mystery” (16) and ends “[e]ven Pääbo admits that he was befuddled by his team’s latest discovery. ‘My hope is, of course, eventually we will not bring turmoil but clarity to this world’, he says” (17).

Here are some scientific facts about the Denisova. One reconstructed molar, one partial molar, one extremely partial molar, one partial mandible, one fragment of the tip of a pinky finger, and one morphologically unidentifiable sliver of bone have all been labeled as Denisovan (or partly so).Footnote ²³ Five of these six samples come from Denisova Cave in Southern Siberia; the sixth comes from Baishiya Karst Cave in Tibet. The difference in altitude between these two caves is approximately 2,500 meters and the caves are located approximately 2,500 kilometers apart. (Geologically speaking, these are big differences.) The teeth identified as Denisovan are bigger in size and irregular in shape when compared to those typically identified as Neanderthal, but they are somewhat similar in size and shape to some other Middle Pleistocene hominin specimens as well as to some Homo erectus specimens (Sawyer et al. Reference Sawyer, Renaud, Viola, Hublin, Gansuage, Shunkov, Derevianko, Prüfer, Kelso and Pääbo2015). The bone fragments are generally insufficient for meaningful analysis in terms of comparative morphology, except for the jaw fragment, which clusters within the known range of Homo erectus specimens along some dimensions (such as mandibular shape), but totally outside all known clusters along others (such as dental arcade; Chen et al. Reference Chen, Welker, Shen, Bailey, Bermann, Davis, Xia, Wang, Fischer, Freidline, Yu, Skinner, Stelzer, Dong, Fu, Dong, Want, Zhang and Hublin2019). Denisova 3, the pinky finger fragment discovered in 2008, is stratigraphically estimated to be 69,000–48,000 years old (Jacobs et al. Reference Jacobs, Li, Shunkov, Kozlikin, Bolikhovskaya, Agadjanian, Uliyanov, Vasiliev, O’Gorman, Derevianko and Roberts2019); or 82,000–74,000 years old on the basis of DNA (Meyer et al. Reference Meyer, Kircher, Gansauge, Li, Racimo, Mallick, Schraiber, Jay, Prüfer, de Filippo, Sudmant, Alkan, Fu, Do, Rohland, Tandon, Siebauer, Green, Bryc, Briggs, Stenzel, Dabney, Shendure, Kitzman, Hammer, Shunkov, Derevianko, Patterson, Andrés, Eichler, Slatkin, Reich, Kelso and Pääbo2012). Denisova 4, the molar unearthed in 2000, is dated to less than 47,000±8,000 years ago on the basis of stratigraphy (Jacobs et al. Reference Jacobs, Li, Shunkov, Kozlikin, Bolikhovskaya, Agadjanian, Uliyanov, Vasiliev, O’Gorman, Derevianko and Roberts2019); but 82,000–74,000 years ago on the basis of DNA (Sawyer et al. Reference Sawyer, Renaud, Viola, Hublin, Gansuage, Shunkov, Derevianko, Prüfer, Kelso and Pääbo2015). Denisova 8, the partial molar discovered in 2010, is stratigraphically estimated to be 132,000–93,000 years old (Jacobs et al. Reference Jacobs, Li, Shunkov, Kozlikin, Bolikhovskaya, Agadjanian, Uliyanov, Vasiliev, O’Gorman, Derevianko and Roberts2019); this stratigraphic estimate is consistent with a DNA-based one (and this is the only instance of such agreement). The extremely partial molar known as Denisova 2 was unearthed in 1984 and is tentatively dated on the basis of the stratigraphic layer in which it was purportedly found to 328,000–246,000 years ago (Jacobs et al. Reference Jacobs, Li, Shunkov, Kozlikin, Bolikhovskaya, Agadjanian, Uliyanov, Vasiliev, O’Gorman, Derevianko and Roberts2019).Footnote ²⁴ On the basis of molecular (DNA-based) dating, it is 181,000–128,000 years old (Slon et al. Reference Slon, Viola, Renaud, Gansauge, Benazzi, Sawyer, Hublin, Shunkov, Derevianko, Kelso, Prüfer, Meyer and Pääbo2017). Denisova 11, the hybrid bone fragment, is estimated on the basis of stratigraphy to be 150,000–118,000 years old (Jacobs et al. Reference Jacobs, Li, Shunkov, Kozlikin, Bolikhovskaya, Agadjanian, Uliyanov, Vasiliev, O’Gorman, Derevianko and Roberts2019); on the basis of DNA, it is estimated to be approximately 90,000 years old (Slon et al. Reference Slon, Majessoni, Vernot, de Filippo, Grote, Viola, Hajdinjak, Peyrégne, Nagel, Brown, Douka, Higham, Kozlikin, Shunkov, Derevianko, Kelso, Meyer, Prüfer and Pääbo2018). The Xiahe mandible is estimated on the basis of dating the matrix which was attached to it to be at least 160,000 years old. There is not sufficient molecular information available, at least given current tech, to obtain a DNA-based estimate of its age.Footnote ²⁵ Note the contradicting dates just relayed, which reflect a lack of agreement among findings derived via different methods and sources. The uncertainty reflected in the facts just shared often extends to the explanations and ideas which scientists have attempted to infer from these facts.

Here are some of the scientific claims that have been made about the Denisova. The Denisova might be a novel, independent population of archaic hominins who lived in parts of Eurasia at the same time as did some Neanderthals and/or anatomically modern humans (Krause et al. Reference Krause, Fu, Good, Viola, Shunkov, Derevianko and Pääbo2010). Or, they might not be; these specimens might just be partial, especially degraded fragments from members of previously known groups such as Neanderthals and/or anatomically modern humans (Caldararo Reference Caldararo2010; Caldararo and Guthrie Reference Caldararo and Guthrie2011a, Reference Caldararo and Guthrie2011b, Reference Caldararo and Guthrie2012). The Denisovan genome seems to contain a contribution (.5%–8%) from an otherwise unknown hominin group, but nothing else about this mysterious, potential ancestor is known (Prüfer et al. Reference Prüfer, Racimo, Patterson, Jay, Sankararaman, Sawyer, Heinze, Renaud, Sudmant, Filippo, Li, Mallick, Dannemann, Fu, Kircher, Kuhlwilm, Lachman, Meyer, Ongyerth, Siebauer, Theunert, Tandon, Moorjani, Pickrell, Mullikin, Vohr, Green, Hellmann, Phillip, Blanche, Cann, Kitzman, Shendure, Eichler, Lein, Bakken, Golovanova, Doronichev, Shunkov, Derevianko, Viola, Slatkin, Reich, Kelso and Pääbo2014). According to mitochondrial DNA, the Denisovan population diverged from present-day humans around a million years ago, about twice as long ago as Neanderthals did (Krause et al. Reference Krause, Fu, Good, Viola, Shunkov, Derevianko and Pääbo2010); but according to nuclear DNA, the Denisovan and Neanderthal populations diverged from present-day humans around half a million years ago, at about the same time (Reich et al. Reference Reich, Green, Kircher, Krause, Patterson, Durand, Viola, Briggs, Stenzel, Johnson, Maricic, Good, Marques-Bonet, Alkan, Fu, Mallick, Li, Meyer, Eichler, Stoneking, Richards, Talamo, Shunkov, Derevianko, Hublin, Kelso, Slatkin and Pääbo2010; Sawyer et al. Reference Sawyer, Renaud, Viola, Hublin, Gansuage, Shunkov, Derevianko, Prüfer, Kelso and Pääbo2015). Initial estimates of the date of divergence between Denisovans and modern humans put the split between 1,313,500 and 779,300 years ago (Krause et al. Reference Krause, Fu, Good, Viola, Shunkov, Derevianko and Pääbo2010); that estimate was then narrowed to date the divergence between Denisovans and modern humans to 804,000 years ago (Reich et al. Reference Reich, Green, Kircher, Krause, Patterson, Durand, Viola, Briggs, Stenzel, Johnson, Maricic, Good, Marques-Bonet, Alkan, Fu, Mallick, Li, Meyer, Eichler, Stoneking, Richards, Talamo, Shunkov, Derevianko, Hublin, Kelso, Slatkin and Pääbo2010). However, then it was widened again and altered to date the split to sometime between 700,000 and 170,000 years ago (Meyer et al. Reference Meyer, Kircher, Gansauge, Li, Racimo, Mallick, Schraiber, Jay, Prüfer, de Filippo, Sudmant, Alkan, Fu, Do, Rohland, Tandon, Siebauer, Green, Bryc, Briggs, Stenzel, Dabney, Shendure, Kitzman, Hammer, Shunkov, Derevianko, Patterson, Andrés, Eichler, Slatkin, Reich, Kelso and Pääbo2012). A combined estimate dates the split between Neanderthals and Denisovan on the one hand and modern humans on the other to either 589,000–553,000 years ago or 765,000–550,000 years ago (Prüfer et al. Reference Prüfer, Racimo, Patterson, Jay, Sankararaman, Sawyer, Heinze, Renaud, Sudmant, Filippo, Li, Mallick, Dannemann, Fu, Kircher, Kuhlwilm, Lachman, Meyer, Ongyerth, Siebauer, Theunert, Tandon, Moorjani, Pickrell, Mullikin, Vohr, Green, Hellmann, Phillip, Blanche, Cann, Kitzman, Shendure, Eichler, Lein, Bakken, Golovanova, Doronichev, Shunkov, Derevianko, Viola, Slatkin, Reich, Kelso and Pääbo2014). Finally, based on study of Denisova 3, 4–6% of the genome of “present-day Melanesians” might come from the Denisova (Reich et al. Reference Reich, Green, Kircher, Krause, Patterson, Durand, Viola, Briggs, Stenzel, Johnson, Maricic, Good, Marques-Bonet, Alkan, Fu, Mallick, Li, Meyer, Eichler, Stoneking, Richards, Talamo, Shunkov, Derevianko, Hublin, Kelso, Slatkin and Pääbo2010); or perhaps 3.0%±0.8% (Meyer et al. Reference Meyer, Kircher, Gansauge, Li, Racimo, Mallick, Schraiber, Jay, Prüfer, de Filippo, Sudmant, Alkan, Fu, Do, Rohland, Tandon, Siebauer, Green, Bryc, Briggs, Stenzel, Dabney, Shendure, Kitzman, Hammer, Shunkov, Derevianko, Patterson, Andrés, Eichler, Slatkin, Reich, Kelso and Pääbo2012). Study of Denisova 8 also indicates some increased gene flow to Papuans and Australians relative to other non-African populations (Sawyer et al. Reference Sawyer, Renaud, Viola, Hublin, Gansuage, Shunkov, Derevianko, Prüfer, Kelso and Pääbo2015); but in the case of both Denisova 2 (Slon et al. Reference Slon, Viola, Renaud, Gansauge, Benazzi, Sawyer, Hublin, Shunkov, Derevianko, Kelso, Prüfer, Meyer and Pääbo2017) and Denisova 4, “there are not enough data to similarly detect gene flow” (Sawyer et al. Reference Sawyer, Renaud, Viola, Hublin, Gansuage, Shunkov, Derevianko, Prüfer, Kelso and Pääbo2015, 15699).

4. Race to publication

In Svante Pääbo’s popular book Neanderthal Man (Reference Pääbo2014), there is a nice account of the initial decision to publish this finding—the one about the relatively greater contribution of the Denisova to the genomes of a few modern-day people from Papua and Bougainville, in contrast with some other modern-day persons from different regions. There was concern that the finding was a technical error, and corresponding debate about whether or not to publish the set of findings with or without that particular result. Pääbo quotes some correspondence among members of the research group:

Clearly, these scientists are capable of considering some risks associated with their making or failing to make candidate scientific claims. Regrettably, in this exchange, the only conceptual option associated with knowing about the result, and yet not publishing it, is that of the easily dismissed “political correctness.” And the scientists’ overwhelming focus with respect to the risks they are taking is on themselves and their reputations, rather than elsewhere—such as with the other, living Papuans whom they are discussing.

In the introduction to this paper, I presented and discussed two philosophical aims: (1) to characterize the phenomenon of sensational science awareness and (2) to document the interaction of that phenomenon with the philosophically much more familiar one of inductive risk—an interaction which I characterize as generating amplified inductive risk. But I have two further, more practical aims, which I mentioned only very briefly: (3) to increase awareness of the phenomenon of inductive risk amongst scientists of this particular domain, that of paleogenetics, and (4) to encourage the members of this domain to seek some collective action which might save individual members from needing to privilege, quite so heavily, their consideration of the risks they might be taking on for themselves and their reputations over the risks they might be imposing on others. In other words, I aim to demonstrate to these scientists that there is more to considering the ethical, moral, political, and social consequences of their claims than mere “political correctness.” And to gently remind them that caring only about how something will impact you is really not a good look.

Figure 1 provides a demonstration of one way in which the publication of this kind of scientific result impacts other people. The caption reads “Melanesians like these Mekeo tribesmen in Papua New Guinea show genetic evidence of ancient Denisovan ancestry.”Footnote ²⁶ I genuinely do not want to presume, so instead I am just going to ask: Is this what the person whose genome was initially sequenced for the purposes of these analyses looked like (described in Pääbo Reference Pääbo2014, 183)? Is it what the second Papuan, and the third person from the island of Bougainville—those who served to provide supplementary data—looked like (Pääbo Reference Pääbo2014, 245)? Were those three people a trio of Mekeo “tribesmen,” standing out in a field of greenery, resplendent in their “tribal” gear?Footnote ²⁷ I am concerned that this is not a picture of the people whose genomes were sequenced for this study, nor is it of the setting in which they were sequenced. Again, I do not want to presume, but it rather looks like a heavily stereotyped, very selective, and correspondingly misrepresentative picture instead—one which trades on some of our most tired Western tropes and biases, while not-so-subtly sending a rather racist message about the apparently “ancient” genetics of the Mekeo and other Papuan people who, Science tells us, happen to have quite a bit more archaic hominin or non-anatomically modern human DNA than the rest of us.

Figure 1. On the left, a captioned photo which ran in volume 352, issue 6282 of Science in April of 2016; on the right, the photo in context with its accompanying news item (Zahn Reference Zahn2016). Note that the alt text generated by Microsoft Word for this photo was “A picture containing tree, outdoor, plant.” For informative discussion of algorithmic bias, please see Bozdag (Reference Bozdag2013), Danks and London (Reference Danks and London2017), or Biddle (Reference Biddle2020), among many others. (From Zahn, Laura M. Reference Zahn2016. “Denisovan DNA Retained in Melanesians.” Science 352 (6282): 183. Reprinted with permission of AAAS. Readers may view, browse, and/or download material for temporary copying purposes only, provided these uses are for noncommercial personal purposes. Except as provided by law, this material may not be further reproduced, distributed, transmitted, modified, adapted, performed, displayed, published, or sold in whole or in part, without prior written permission from the publisher.)

5. The argument from inductive risk

Time for some philosophical nuts and bolts—for deployment of the machinery needed to transform thinking about the potentially racist impacts of scientific work from political correctness to professional responsibility. In 2000, the philosopher of science Heather Douglas published a paper in Philosophy of Science called “Inductive Risk and Values in Science.” In it, she revived Hempel’s (Reference Hempel1954, Reference Hempel and Spiller1960) concept of inductive risk and then used that concept to make an argument. Since Douglas does not herself christen the argument, I will henceforth refer to it as “the argument from inductive risk” merely as convenient shorthand for “the argument from ‘Inductive Risk and Values in Science,’ written by Heather Douglas and published in Philosophy of Science in the year 2000.”Footnote ²⁸

There are three crucial components to the overall argument contained in Douglas (Reference Douglas2000). The first occurs in the following passage:

This argumentative component can be validly, deductively formulated: for example, as two instances of modus tollens, or as one instance of hypothetical syllogism followed by one instance of modus tollens. As written, the argument is enthymemic (it relies on an implicit premise), but the missing step in the argument is easily supplied:

1. 1. “To claim that scientists ought not consider the predictable consequences of error (or inductive risk) is to argue that scientists are somehow not responsible for their actions as scientists.”

2. 2. IMPLICIT: To claim that scientists are somehow not responsible for their actions as scientists is to argue that scientists do not have the same moral responsibilities as the rest of us.

3. 3. “[S]cientists have the same moral responsibilities as the rest of us.”

4. -----------------------------------------------------------------------------------------------------------------------------------------

5. 4. DERIVED: Therefore, it is not the case that “scientists ought not consider the predictable consequences of error (or inductive risk).”

Note that this conclusion can be more simply stated: scientists ought to consider the predictable consequences of error (or inductive risk). Note also that this restatement is logically equivalent; it simply removes the double negative. Since the argument is deductively valid, whether or not we accept this conclusion depends entirely on its premises. These premises get some defense in Douglas (Reference Douglas2000), but perhaps not as much defense as they require. The author is especially curt when it comes to defending premise 3; recall her entertaining statement that “Arguing that scientists have the same moral responsibilities as the rest of us is beyond the scope of this paper” (563).

But in a Reference Douglas2003 paper (“The Moral Responsibilities of Scientists”), Douglas clarifies the meaning of premise 3, and she defends the premise extensively in her Reference Douglas2009 book, Science, Policy, and the Value-Free Ideal. What Douglas means when she says that “scientists have the same moral responsibilities as the rest of us” is actually that scientists are not excused from their general moral responsibilities (as persons) by their special role responsibilities (as scientists)—contra, for instance, Bridgman (Reference Bridgman1947) or Price (Reference Price1965). In the case of inductive risk, what this means is that scientists are not excused by their status as scientists from their general moral responsibility to consider what might predictably follow from their saying something false. There are some circumstances, Douglas admits, in which special role responsibilities can trump this sort of general moral responsibility, but in the case of scientists and this particular sort of risk: “the social structures that would allow for such a reduction in general moral responsibilities are not in place” (Reference Douglas2003, 60). So, if one accepts that there is a general moral responsibility of persons to consider what might predictably follow from their saying something which is potentially false (in deciding whether or not they have sufficient reason to say it), and one accepts that scientists are not specially excused from this general moral responsibility because of their role as scientists, then “scientists have the same moral responsibilities as the rest of us.”Footnote ²⁹

Douglas’s account of the general moral responsibility of persons to consider what might predictably follow from their saying something which is potentially false (in deciding whether or not they have sufficient reason to say it) is grounded in the concepts of recklessness and negligence (following Feinberg Reference Feinberg1970). Douglas’s account of why scientists are not excused from this general moral responsibility by their scientific role responsibilities is grounded in two further points: first, that “someone must be responsible for thinking about the potential consequences at these decision points or the general responsibilities go completely neglected” (Douglas Reference Douglas2003, 64); and second, that scientists themselves are the only sufficiently informed and appropriately positioned persons capable of performing this task. Hence, scientists have the same general responsibilities as the rest of us—including that of considering what might predictably follow from saying something potentially false (in deciding whether or not there is sufficient reason to say it)—and they are not excused from this responsibility by their status as scientists.Footnote ³⁰

The next crucial component of the argument from inductive risk occurs on page 565 of Douglas (Reference Douglas2000). In the prior component, Douglas stressed the responsibility which scientists have to consider predictable consequences of their potential errors in judgment, including those errors of deciding to say something which turns out to be false. In this new component, Douglas stresses those consequences which are both clear and nonepistemic. And, Douglas argues, considering consequences which are nonepistemic requires considering values which are nonepistemic.Footnote ³¹ Here is the relevant text:

Again, this argumentative component can be deductively, validly formulated. If we think of Douglas’s emphasis on consequences which are both clear and nonepistemic as conditional specifications of when her initial conclusion about predictable consequences applies, and we consider her move from considering consequences to considering values as an entailment, then we can structure this argumentative component in a valid way with moves as simple as conjunction and modus ponens.

Interpreted in this manner, the argument says: if consequences are not just predictable but also clear, then inductive risk should be considered; if consequences are nonepistemic, then those considerations of inductive risk should be nonepistemic as well; and here (the argument points to them) are some cases with consequences that are both clear and nonepistemic. Thus, inductive risk should be considered, and these considerations should be nonepistemic. Since all of this is happening in what have often been presented as the “internal” stages of science, what this means is that we have nonepistemic values being considered (and responsibly so) even in those “internal” stages.Footnote ³² And that’s it for the (supposed!) last stand of the value-free ideal. Hewing close to the text now (Douglas Reference Douglas2000, 565):

1. 5. “In cases where the consequences of making a choice and being wrong are clear, the inductive risk of the choice should be considered by the scientists making the choice.”

2. 6. “[W]here the weighing of inductive risk requires the consideration of non-epistemic consequences, non-epistemic values have a legitimate role to play in the internal stages of science.”

3. 7. “In the cases I [Douglas] discuss below, the consequences of the choices include clear non-epistemic consequences[.]”

4. -----------------------------------------------------------------------------------------------------------------------------------------

5. 8. DERIVED: Therefore, in the discussed cases, “non-epistemic values have a legitimate role to play in the internal stages of science.”

Premise 5 is a qualified restatement of conclusion 4; it is licensed as long as the preceding argumentative component has been. Premise 7 is amply demonstrated by Douglas’s (Reference Douglas2000) case study involving rat tumors, liver slides, and the chemical dioxin. That leaves premise 6, the inference from nonepistemic consequences to nonepistemic value considerations, as a new claim requiring at least some defense. The idea here is that nonepistemic impacts of professionally erring in judgment necessarily incur consideration of nonepistemic values—at least, when such impacts are both clear and predictable. Douglas claims that in such cases and in order to determine how to handle the risk of professionally erring in judgment, scientists in their professional capacity must consider the nonepistemic impacts—a.k.a. the (dis)value—of such error.

One could attempt to avoid this entailment from the known, clear existence of nonepistemic impacts to the necessary consideration by scientists of those impacts and their (dis)value in uncertain cases. In recent work pursuant of this line of thought, Douglas (Reference Douglas2021) explores the space of possible responses and presents four alternatives which might be adopted instead: (i) using random processes, such as coin flipping, to settle uncertain cases; (ii) using only epistemic values, like accuracy or consilience, to respond to nonepistemic risks of error; (iii) asking scientists to remain agnostic in all cases of uncertainty, limiting themselves to the communication of degrees of certainty and lack thereof; or (iv) licensing scientists to settle only small uncertainties, while requiring they disclose all larger ones.

The irony is that none of these responses actually avoid the consideration of nonepistemic values in the process of their adoption (when their adoption is possible). This is because none of these are normal, or default, procedures in science, and the choice to adopt them is motivated, in this context at least, by consideration of nonepistemic values. When faced with an ambiguous piece of observational data,Footnote ³³ scientists do not typically (i) flip a coin in order to decide how to record their observation.Footnote ³⁴ Deciding to deviate from normal procedure in such a manner, and because of nonepistemic risk, just is to consider nonepistemic (dis)value, not in how to score the observation itself, but in what procedure to adopt for scoring.Footnote ³⁵ The same can be said for pursuit of option (ii), using epistemic values to respond to nonepistemic risks and (dis)value. Say a scientist would normally feel free to speculate about historical migration patterns among geese solely on the basis of molecular data. But when it comes to historical migration patterns among archaic hominins, scientists might alternatively decide that due to the foreseeable interpretive impact such speculations might have and given the risk of error, there must be consilience between available sources of molecular and morphological data before such speculations can be published. This line of reasoning emphasizes the epistemic value (of consilience) over alternatives (such as pace of inquiry), but it still considers nonepistemic values (like special respect for persons) in the process of choosing which epistemic values to highlight (in this case, consilience over pace). Note that the pervasiveness of induction means it is not even close to possible for scientists to (iii) remain agnostic in all cases of uncertainty; and in many cases, (iv) disclosing all and only the larger uncertainties while remaining agnostic about them will not be possible either (e.g., as in the case of climate science projection and advising [Havstad and Brown Reference Havstad, Brown, Elliott and Richards2017]).Footnote ³⁶ In cases where response (iv) is possible, when attempted, it will again be a deviation from the norm, adoption of which is being motivated by consideration of nonepistemic values.

In sum, none of these attempts to reject premise 6—the claim that, when inductive risk requires consideration of nonepistemic impacts, nonepistemic values have a legitimate role to play in the internal stages of science—actually succeed either in being possible or, when possible, in eliminating a legitimate role for nonepistemic values even in the internal stages of science. Recall that this component of Douglas’s argument from inductive risk is deductively valid. If its premises have all been successfully defended, then it must be admitted as sound. Or, to state the contrapositive: because this argument is deductively valid, if you want to reject the conclusion of this argument, then you need to find a premise to reject.

The third and final crucial component of the overall argument contained in Douglas (Reference Douglas2000) is the explicit establishment of which conditions do and do not trigger the argument from inductive risk—at least, as demonstrated in this piece of writing. Recall the narrowed scope of premise 5: “In cases when the consequences of making a choice and being wrong are clear” (Reference Douglas2000, 565). And that of premise 6: “[W]here the weighing of inductive risk requires the consideration of non-epistemic consequences” (565). Based on the targeting of this discussion towards predictable impacts that are both clear and nonepistemic, the author partitions science into four regions or zones. This occurs on pages 577–578, as Douglas concludes her piece:

1. A. “When there is very low uncertainty, such that a scientist believes there is virtually no chance of being wrong.”

2. B. “[W]here making a wrong choice has no impact on anything outside of that area of research.”

3. C. “[W]here the science will likely be useful but the potential consequences of error may be difficult to foresee.”

4. D. “[W]hen non-epistemic consequences of error can be foreseen.”

It is in zone D that Douglas’s overall argument conclusively applies, demonstrating that “non-epistemic (i.e., social, ethical, political) values … are a required part of the internal aspects of scientific reasoning” (559). Zone C is a “gray area” (578)—one that will have to be decided on a case-by-case basis. Zones B and A are exempt from the force of the argument.Footnote ³⁷

6. Amplified inductive risk

Scientific research which extracts molecular information from Denisovan specimens and compares that archaic genomic data to current genomic data, attributing more nonanatomically modern human ancestry to some populations than others, is zone D science—science in which negative, nonepistemic impacts of error can be readily foreseen. It is also science for which the chance of error is quite high since (among other concerns) there is only one high-coverage nuclear genome (from Denisova 3).Footnote ³⁸ The initial studies, those that attribute significant Denisovan ancestry to Papua New Guineans compared to other non-African populations such as the French (Reich et al. Reference Reich, Green, Kircher, Krause, Patterson, Durand, Viola, Briggs, Stenzel, Johnson, Maricic, Good, Marques-Bonet, Alkan, Fu, Mallick, Li, Meyer, Eichler, Stoneking, Richards, Talamo, Shunkov, Derevianko, Hublin, Kelso, Slatkin and Pääbo2010; Meyer et al. Reference Meyer, Kircher, Gansauge, Li, Racimo, Mallick, Schraiber, Jay, Prüfer, de Filippo, Sudmant, Alkan, Fu, Do, Rohland, Tandon, Siebauer, Green, Bryc, Briggs, Stenzel, Dabney, Shendure, Kitzman, Hammer, Shunkov, Derevianko, Patterson, Andrés, Eichler, Slatkin, Reich, Kelso and Pääbo2012), as well as more recent follow-up studies (Skoglund and Jakobsson Reference Skoglund and Jakobsson2011; Qin and Stoneking Reference Qin and Stoneking2015; Vernot et al. Reference Vernot, Tucci, Kelso, Schraiber, Wolf, Gittelman, Dannemann, Grote, McCoy, Norton, Scheinfeldt, Merriwether, Koki, Friedlaender, Wakefield, Pääbo and Akey2016), are all based on genetic material obtained from one tiny bone fragment (part of the tip of a child’s pinky finger). Yet it is an utter mystery how so much genetic information, and of such high quality, was obtained from that particular sample. The scientists themselves have remarked on this fact—e.g., “No one thought we would have an archaic human genome of such quality” and “Everyone was shocked by the counts. That includes me” (Matthias Meyer, quoted in Gibbons Reference Gibbons2012, 1028). There are other significant sources of uncertainty, as well, such as the fact that the paucity of morphological data means consilience between molecular and morphological data can barely be sought, much less obtained. There are also pressing geographical questions to answer, such as how the Denisova—purportedly a group of hominins specially adapted to the high-altitude Tibetan Plateau (Huerta-Sánchez et al. Reference Huerta-Sánchez, Jin, Asan, Peter, Vinckenbosch, Liang, Yi, He, Somel, Ni, Wang, Ou, Huasang, Cuo, Li, Gao, Yin, Wang, Zhang, Xu, Yang, Li, Wang, Wang and Nielsen2014)—managed to make more of a genetic contribution to an extreme low-lying island population than to other, closer populations, and to a population living 5,000–7,500 kilometers away from where any of the Denisovan remains have been found, much of that distance across open water.

Given the uncertainty in this domain, the corresponding chance of making false scientific claims and the pernicious interpretive implications likely to be erroneously drawn—i.e., the utterly foreseeable attempts at scientized racism—one might expect that the scientists working in this domain would consider raising their standards of evidence in response to the predictably pernicious consequences which their risky racial pronouncements might erroneously entail. In other words: if what you are thinking about scientifically claiming is going to predictably add further fuel to the briskly burning racial fire, then you might want to make extra sure that what you are saying is scientifically necessary, justified, and correct.Footnote ³⁹ Of course, as we have already seen, if practitioners are not aware of the argument from inductive risk, then such considerations of impacts and consequences can sometimes and unfortunately be quickly dismissed as mere political correctness. But the argument itself is not so easy to rebut. There is also the matter of pressing matter of incentives, such as what sort of considerations might incentivize practitioners to waive away thought of consequences, caution, or concern for others.Footnote ⁴⁰

The science being discussed here is not just zone D science, or science for which the argument from inductive risk decisively applies; it is also predictably sensational science. Predictably sensational science is science which practitioners can foreseeably expect to capture and sustain public interest in a way that is likely to foster its development and to amplify the publication and prestige of its results. We need an additional, complementary zoning scheme:

1. I. When there is very low public interest in a scientific issue, such that the science has virtually no chance being sensationalized.

2. II. Where the evidence pertaining to a scientific issue is so decisive in terms of either its absence or presence that sustained, public speculation about that issue is nigh impossible.

3. III. Where there is enough evidential ambiguity pertaining to a scientific issue such that sustained speculation is possible, but the degree of public interest in that issue is also so ambiguous that sensationalization is difficult to predict.

4. IV. When there is overwhelming public interest in a scientific issue, and speculation about that issue can be predictably fueled by at least some, but still scant, availability of evidence.

Just as Douglas’s work on inductive risk identifies four zones in which its conclusion is of more or less pressing concern, so too does this analysis of sensational science pick out different regions in which its force is more or less likely to be felt. Just as Douglas’s first two zones are ones in which inductive risk is not of much concern, so too are my first two zones those in which the matter of sensationalization will likely be moot. Just as Douglas’s zone C is a gray area, one in which the influence of inductive risk will likely need assessment on a case-by-case basis, so too will sensationalization perhaps or perhaps not be in play for my zone III. And, for both of us, it is in our fourth and final zones that the phenomena we are characterizing (inductive risk in Douglas’s case, sensationalization in mine) are obviously in play.

In Douglas’s first zone (or zone A, as I am calling it), there is a lack of the scientific uncertainty required for the argument from inductive risk to get off the ground. In zone B, there are no nonepistemic impacts to worry about, even in the case of whatever error might be generated by scientific uncertainty. In zone C, there is the requisite scientific uncertainty, along with probable nonepistemic impacts, but the unpredictability of those impacts makes it difficult to hold scientists responsible for those impacts, even in the case of error. And in zone D, there is all of what is required for the argument from inductive risk to decisively apply: scientific uncertainty, nonepistemic impacts, and predictability. Similarly, in my first zone (zone I), there is a lack of the sort of public interest required for sensational science. In my zone II, the evidential situation is unlikely to sustain the sort of speculation that tends to fuel sensational science. In my zone III, there is the potential for public interest, along with enough evidential ambiguity to make speculation possible, but the unpredictability of the interaction between these two factors makes it difficult to anticipate the sensationalization (or not) of the relevant science. Finally, in my zone IV, there is predictably sensational science: science characterized by overwhelming public interest and just the sort of scant evidential situation to fuel enduring speculation.Footnote ⁴¹

Douglas’s argument from inductive risk is fueled by the risk of error conferred by the following three factors: scientific uncertainty, the existence of nonepistemic impacts, and the predictable foreseeability of those impacts. Sensational science is alternatively fueled: by overwhelming public interest, at least some evidential ambiguity, and a steady enough stream of scientific discoveries (just enough to keep the press releases coming, while still leaving plenty of uncertain room for breathless and ongoing speculation). And, if we put these two phenomena together—inductively risky considerations with sensational science potential—what we get are cases of amplified inductive risk: scientific cases in which inductively high-risk pronouncements are nonetheless driven by the promise of heightened public interest, just enough of a scant evidential situation to fuel speculation, and the predictably foreseeable sensationalization of the relevant science.Footnote ⁴²

Science that is zoned D + IV is extremely sticky science. The argument from inductive risk encourages scientists to be extra careful about the judgments they make in this domain due to the high chance of error, and the predictable nonepistemic impacts. But here, the potential for sensationalization also encourages scientists to be more reckless than usual since they are quite likely to obtain support for their research, as well as gain publicity and prestige for their results given the public interest likely to capture initial attention along with the scant evidential situation likely to sustain enduring speculation. In these cases of amplified inductive risk, just when we want scientists to be more cautious than usual (given the argument from inductive risk), they are instead heavily incentivized to be less cautious than usual (due to the predictable sensationalization of the science). I suspect that scientific study of the Denisova is appropriately tagged as both D- and IV-zone science, and that this is why we are currently being treated to the degree and sort of speculation we are presently getting despite the risk of error, the predictably pernicious interpretations, the small sample sizes, the lack of consilience between morphological and molecular data, and the rather glaring absence of coherent or consistent narratives.

7. Potential adjustments to practice

At this point, there are various recommendations which we might make to the paleogeneticists working on purported relationships between Denisovan genetic remains and apparent subsubpopulations of current humans. (Presuming that this is a case to which the argument from inductive risk applies, and that it is also a case of predictably sensational science—i.e., presuming that this is indeed a case of amplified inductive risk.) These responses could be arranged on a spectrum from least to most accommodating. At the least permissive end of the spectrum, we might simply call for scientists to cease work on the project of detecting and pronouncing who among the apparent subsubpopulations of current humans has more or less “ancient” genetics than others.Footnote ⁴³ Calling for a moratorium on such work, however, will only produce a halt in research if scientists elect to heed that call, and I suspect that what makes amplified inductive risk cases so tricky to handle is just how heavily incentivized scientists are to work on these issues, along with how handsomely those who do so are rewarded with publicity and prestige. Alternatively, at the most permissive end of the spectrum, we could simply endorse what might be termed “business as usual,” understood as no critique of the science as it is currently being practiced, no attempt to interfere with scientists proceeding in whatever manner they elect to proceed—with or without consideration of inductive risk, pernicious interpretive implications, and responsibility for foreseeable impacts of erring in professional judgment. Between these two options—which might rather glibly be glossed as “do not do it” on the one hand and “do whatever you want” on the other—are a host of more mixed responses. In what remains of this piece, I will consider three (though there are more in the possibility space).

First, we might decide that scientists can continue working in this area with impunity for even the predictably pernicious impacts of any erroneous scientific claims they might make as long as they disclose the uncertainty of their pronouncements when making them. The really interesting thing about this option is that the scientists involved already do this; but qualifying their scientific claims with statements of uncertainty seems to do nothing to blunt the publicity the work receives, or the predictably pernicious interpretive implications drawn from it.Footnote ⁴⁴ Here is a particularly sobering example of an especially direct admission of uncertainty: “We caution that these analyses make several simplifying assumptions” (Prüfer et al. Reference Prüfer, Racimo, Patterson, Jay, Sankararaman, Sawyer, Heinze, Renaud, Sudmant, Filippo, Li, Mallick, Dannemann, Fu, Kircher, Kuhlwilm, Lachman, Meyer, Ongyerth, Siebauer, Theunert, Tandon, Moorjani, Pickrell, Mullikin, Vohr, Green, Hellmann, Phillip, Blanche, Cann, Kitzman, Shendure, Eichler, Lein, Bakken, Golovanova, Doronichev, Shunkov, Derevianko, Viola, Slatkin, Reich, Kelso and Pääbo2014, 46).Footnote ⁴⁵ The literature is replete with additional instances.

Consideration of this first option, along with the realization that going this route seemingly does nothing to mitigate the problem of amplified inductive risk, suggests a second option. Perhaps we need to tag these papers with some sort of “warning label” that might nudge authors, readers, and commentators from all communities (scientific, journalistic, public) to take the speculative nature of much of Denisovan paleogenetics quite a bit more seriously. It is possible that an illustrative graphic—perhaps placed on the first page of any scientific publication regarding the Denisova—which makes clear precisely how little material exists, relatively speaking, as well as how much more information scientists would like to have than they currently do, would more effectively draw attention to the speculative nature of this research than qualifications and hedges buried in the text have. Please see Table 2 for a text-based example, one drawn from a relatively recent publication about the Denisova (Slon et al. Reference Slon, Viola, Renaud, Gansauge, Benazzi, Sawyer, Hublin, Shunkov, Derevianko, Kelso, Prüfer, Meyer and Pääbo2017). Note, however, that a more visual rather than textual presentation of the information would likely be more elegant and effective. Perhaps an infographic with differential amounts of information available conveyed by icons of relative size would suit. Note also that it is vital that the two halves of the table are thought of together.

Table 2. An example of what an evidential “warning label” might look like based on the data reported in Slon et al. (Reference Slon, Viola, Renaud, Gansauge, Benazzi, Sawyer, Hublin, Shunkov, Derevianko, Kelso, Prüfer, Meyer and Pääbo2017). On the left, the relative evidential situation informs readers precisely how little there is in the way of Denisovan specimens relative to other archaic hominins; on the right, the ideal evidential situation informs readers that this relative paucity of material matters for the conclusions being drawn.

In this and other fields, a mismatch between relative evidence bases might not matter for the conclusions being drawn, but that would presumably be reflected in a match between actual and ideal evidence bases. Alternatively, a mismatch between actual and ideal evidence bases might be standard practice for a field, but that would presumably be reflected in a match with other relative evidential situations. It is when there is both a relatively small evidence base and a significant mismatch between actual and ideal evidence bases that there is (epistemic) cause for concern.

A third available option is to point to the above lack of resolution in the literature (among others) and urge that, for both epistemic and inductive risk-style reasons, scientists should resist the pull of sensationalism while maintaining their normal (high) epistemic standards when it comes to things like sample size, reconciliation of data from multiple sources, and narrative consistency.Footnote ⁴⁶ For instance: a commitment to telling scientific stories about relative degrees of Denisovan ancestry amongst current peoples only when there is consilience between molecular, morphological, and geographic evidence (at least) would reduce intermittent speculation while still permitting such research to proceed, bringing such results to the public only when they are more reliable.Footnote ⁴⁷ I would be delighted were the relevant scientific community to attempt anything other than “business as usual,” and I welcome further attempts by the relevant scientists to come together—with one another and their critics—in order to articulate some form of response.Footnote ⁴⁸

8. Concluding remarks

In sum, I think that we should be very careful when claiming (as do Reich et al. Reference Reich, Green, Kircher, Krause, Patterson, Durand, Viola, Briggs, Stenzel, Johnson, Maricic, Good, Marques-Bonet, Alkan, Fu, Mallick, Li, Meyer, Eichler, Stoneking, Richards, Talamo, Shunkov, Derevianko, Hublin, Kelso, Slatkin and Pääbo2010; Meyer et al. Reference Meyer, Kircher, Gansauge, Li, Racimo, Mallick, Schraiber, Jay, Prüfer, de Filippo, Sudmant, Alkan, Fu, Do, Rohland, Tandon, Siebauer, Green, Bryc, Briggs, Stenzel, Dabney, Shendure, Kitzman, Hammer, Shunkov, Derevianko, Patterson, Andrés, Eichler, Slatkin, Reich, Kelso and Pääbo2012) that members of one population might be genetically more archaic than others—especially when scientific claims of relative genetic archaism might be taken to reinforce latent, racial judgments of primitivism. I think such caution is warranted even in a context where other molecular evidence (e.g., Skoglund and Jakobsson Reference Skoglund and Jakobsson2011; Prüfer et al. Reference Prüfer, Racimo, Patterson, Jay, Sankararaman, Sawyer, Heinze, Renaud, Sudmant, Filippo, Li, Mallick, Dannemann, Fu, Kircher, Kuhlwilm, Lachman, Meyer, Ongyerth, Siebauer, Theunert, Tandon, Moorjani, Pickrell, Mullikin, Vohr, Green, Hellmann, Phillip, Blanche, Cann, Kitzman, Shendure, Eichler, Lein, Bakken, Golovanova, Doronichev, Shunkov, Derevianko, Viola, Slatkin, Reich, Kelso and Pääbo2014) indicates more Neanderthal admixture with European populations than others. Probably, we ought to raise our standards of evidence in the making of such claims. But at the very least, surely, we ought not to be lowering our standards of evidence in response to the incentives and rewards of sensational science when it comes with such inductively risky and perniciously racial consequences for others.

And, in case this point is not yet clear: at present, there are some very serious questions about the special genetic relationship reported in the scientific literature between the Denisova and “present-day Melanesians.” Questions such as: How did the most significant genetic signature (by far) of the Denisova, supposedly a population of archaic hominins specially adapted to high-altitude living, end up in a low-altitude island population living at least 5,000 kilometers away from where any Denisovan remains have been found? If the Denisova were as widespread as that molecular contribution makes them seem, why is their genetic diversity as low as it is? Where—other than Denisova Cave, and perhaps Baishiya Karst—is the morphological and archeological evidence of their supposedly widespread population? Where, for instance, is the evidence of at least 160,000 years of hominin residence on the Tibetan Plateau? Scientists working on the Denisova are very aware of these questions:

The genetic results being produced here—by scientists doing some technically stunning ancient DNA work—are extremely intriguing, clearly. But the results do not yet cohere with one another even within the molecular realm, and certainly not when considering the archaeological, geographic, and morphological evidence bases as well.

My study of the relevant literature leads me to judge that there is an unusual lack of consilience in this work, and I suspect that it is the sensational character of the scientific work on archaic hominin genetic history which explains that (along with other related features, such as small sample sizes, excessive uncertainty, and lots of accompanying hedges). Proponents of the argument from inductive risk are, I think, likely to judge that this apparent lowering of epistemic standards is exactly the opposite of what should be happening—especially when it comes to linking work on archaic genetic history to current human genetics, and in ways with predictably racist outcomes.Footnote ⁴⁹ Any remaining opponents of the argument from inductive risk are, I think, likely to object to the proposed raising of epistemic standards in response to considerations of racism and social injustice, but they should also, I think, object to the apparent lowering of epistemic standards in response to considerations of publicity and prestige. I think it is difficult to dissuade persons from acting in ways which they are highly incentivized to pursue. But I also hope that by presenting the details of this case, articulating a sound version of the argument from inductive risk, and identifying the phenomenon of amplified inductive risk, we might begin to change some of the apparent incentives—in this instance, at least.Footnote ⁵⁰