Feeding Ecology Analysis Supports a Marine Diet in the Extinct Chatham Island Duck (Anas Chathamica)

Feeding Ecology Analysis Supports a Marine Diet in the Extinct Chatham Island Duck (Anas Chathamica)

Emu - Austral Ornithology ISSN: (Print) (Online) Journal homepage: https://www.tandfonline.com/loi/temu20 Feeding ecology analysis supports a marine diet in the extinct Chatham Island Duck (Anas chathamica) Rodrigo B. Salvador, Karyne M. Rogers, Alan J. D. Tennyson & Barbara M. Tomotani To cite this article: Rodrigo B. Salvador, Karyne M. Rogers, Alan J. D. Tennyson & Barbara M. Tomotani (2021): Feeding ecology analysis supports a marine diet in the extinct Chatham Island Duck (Anaschathamica), Emu - Austral Ornithology, DOI: 10.1080/01584197.2021.1939719 To link to this article: https://doi.org/10.1080/01584197.2021.1939719 Published online: 22 Jun 2021. Submit your article to this journal Article views: 9 View related articles View Crossmark data Full Terms & Conditions of access and use can be found at https://www.tandfonline.com/action/journalInformation?journalCode=temu20 EMU - AUSTRAL ORNITHOLOGY https://doi.org/10.1080/01584197.2021.1939719 Feeding ecology analysis supports a marine diet in the extinct Chatham Island Duck (Anas chathamica) Rodrigo B. Salvador a, Karyne M. Rogers b, Alan J. D. Tennyson a and Barbara M. Tomotani c aNatural History Department, Museum of New Zealand Te Papa Tongarewa, Wellington, New Zealand; bGNS Science, National Isotope Centre, Lower Hutt, Wellington, New Zealand; cNIOO-KNAW, Netherlands Institute of Ecology, Wageningen, The Netherlands ABSTRACT ARTICLE HISTORY The Chatham Island Duck, Anas chathamica, is one of many New Zealand bird species that became Received 8 September 2020 extinct after Polynesian arrival. The Chatham Island Duck was a large flightlessbird, with salt glands Accepted 1 June 2021 on its skull, which led to the hypothesis that it lived in a marine habitat. We tested this hypothesis KEYWORDS using a combination of stable isotope analysis (carbon and nitrogen) and analysis of morphoana­ Anas chathamica; Anatidae; tomical features. We also conducted a comparative analysis with other anatids from the Chatham New Zealand; stable Islands and New Zealand. Furthermore, we trialled the non-destructive technique of portable X-ray isotopes; X-ray fluorescence fluorescence (elemental composition of bones) to assess whether it can be helpful for reconstruct­ ing the ecology and habitat of extinct species. We obtained data from museum specimens: 12 samples of A. chathamica and 55 of other anatids for isotope analysis; and 23 samples of A. chathamica and 63 of other anatids for X-ray fluorescence. Results from isotope analysis, supported by anatomical features, show that A. chathamica had a more fully marine diet than previously hypothesised, mainly composed of invertebrates. The large body size of A. chathamica is possibly related to territoriality and combat, which is also supported by the presence of carpal weaponry. Our data demonstrate the importance that the marine environment likely played in the life of this extinct species, while highlighting the key role natural history collections can have in ecological studies. Introduction habits of extinct species by defining their feeding ecology (Peterson and Fry 1987; Kelly 2000; Inger and Bearhop Recent technological and methodological advances 2008). The δ13C and δ15N values of organisms reflect those allow us to explore a vast and still largely untapped of their environment and, thus, can be used to infer diet wellspring of ecological information in natural history and trophic relationships (Mizutani et al. 1992; Post 2002; collections (Webster 2017; Meineke et al. 2018; Salvador Fox and Bearhop 2008; Bond and Jones 2009). Nitrogen and Cunha 2020). Besides the more usual studies focus­ isotopes are indicative of trophic level (e.g. DeNiro and ing on current anthropogenic effects of environment Epstein 1981; Minagawa and Wada 1984; Peterson and Fry and global change (Meineke et al. 2018; Schmitt et al. 1987; Post 2002), while carbon isotopes are related to 2018), another important aspect of using museum speci­ sources of carbon from the animals’ feeding environment mens is the reconstruction of the ecology of species that (e.g. marine versus freshwater; Kelly 2000; Fry 2006; Fox became extinct in historical times due to anthropogenic and Bearhop 2008; Inger and Bearhop 2008). activity. Given that typically very few specimens remain Portable X-ray fluorescence (pXRF) provides the ele­ of such species, it is important that they are analysed in mental composition of a sample, determining the abun­ as much detail as possible, balancing destructive and dance of major and trace elements assimilated from the non-destructive techniques (Webster 2017). Among bird’s habitat and diet (Plummer et al. 1994; Rogers the new methodologies now available to us are isotope 2019). This method is widely used in archaeology to analysis (destructive) and portable X-ray fluorescence determine the provenance of human bones and artefacts (non-destructive). (e.g. LaBrecque et al. 1998; Adan-Bayewitz et al. 2007; Stable isotope analysis is an established methodology for Byrnes and Bush 2016), but can also be used to investigate acquiring environmental and ecological information. The bones of other species, including fossils (e.g. Plummer ratio between the stable isotopes of carbon (13C/12C) and et al. 1994; Rogers 2019). However, besides its use for nitrogen (15N/14N) are particularly useful to reconstruct detection of pollutants (e.g. Radu and Diamond 2009; CONTACT Rodrigo B. Salvador [email protected] This article has been corrected with minor changes. These changes do not impact the academic content of the article. © 2021 BirdLife Australia 2 R. B. SALVADOR ET AL. Peinado et al. 2010), the use of pXRF in zoo-ecological Herein we use a combination of independent lines of analyses has not been thoroughly explored yet. evidence to assess whether A. chathamica lived primar­ New Zealand’s avifauna, although not particularly ily in a marine environment. Namely, we analyse mor­ rich, is among the most recognisable in the world due pho-anatomical features that are potentially related to to its numerous flightless ‘oddities’. Unfortunately, the marine habits and use stable isotope data to gain infor­ country also ranks high in the number of extinct species mation about diet, and thus habitat. To provide better during the Holocene as more than a third of its breeding support to our analyses of A. chathamica, we also supply bird diversity has been extirpated, including several comparative data on other anatid species that inhabit waterfowl species (Holdaway 1989; Young et al. 1996; the Chatham Islands, as well as other oceanic islands Tennyson and Martinson 2007). The Chatham Islands around New Zealand. Finally, we test whether pXRF can (located ca. 800 km east of mainland New Zealand), offer useful information for ecological studies of extinct despite its limited size, had a reasonably diverse water­ species through the retention and accumulation of diet­ fowl fauna comprising nine species, four of which ary or environmentally specificelements in bones. Being became entirely extinct via anthropic action, with a portable and non-destructive procedure, it is worth­ another four species locally extinct in the Chathams while exploring its potential uses for cases where only but surviving elsewhere in New Zealand (Holdaway few precious museum specimens are available. 1989; Millener 1999; Tennyson and Martinson 2007; Miskelly 2008). One such casualty was the endemic Material and methods Chatham Island Duck, Anas chathamica (Oliver 1955), extinguished through hunting by early Polynesian set­ Our comparative analyses included specimens of tlers (Williams 1964; Tennyson and Martinson 2007). A. chathamica, as well as other Anas spp. present in Anas chathamica had some unique and unusual fea­ New Zealand: Brown Teal, A. chlorotis G.R. Gray, 1845; tures, including its size (largest in genus), flightlessness, Grey Duck, A. superciliosa Gmelin, 1789; Auckland carpal weaponry (proportionally the largest in Island Teal, A. aucklandica (G.R. Gray, 1849); Campbell Anseriformes) and the presence of large salt glands on Island Teal, A. nesiotis (J.H. Fleming, 1935). The former the skull (Figure 1; Williams 2015a, 2015b; Watanabe two were present both on the Chatham Islands and on 2017). Very few bones of this duck have been collected New Zealand’s mainland (we analysed specimens from so far, either from natural settings or middens (Marshall both settings), and the latter two inhabit other archipela­ et al. 1987; Williams 2015b), and this lack of physical gos south of the New Zealand mainland and are flightless material makes it difficult to study the species in more like A. chathamica. We also included the extinct endemic detail. Previous authors proposed that A. chathamica Chatham Island Merganser, Mergus milleneri Williams & had a marine-based diet due to the physiological pre­ Tennyson, 2014, for comparison, which likely had sence of salt glands (Williams 2015a), but that hypoth­ a marine-based diet. esis has not been tested so far. The isotope dataset stems from a joint project of Murray J. Williams and Richard N. Holdaway that took place in 2000–2005, to which we have been granted access. Part of the dataset has already been published by Holdaway et al. (2013: A. chlorotis) and Williams et al. (2012: M. milleneri), but the remaining values are reported here for the first time. Samples for stable isotope analysis were largely obtained from bone specimens housed at the Museum of New Zealand Te Papa Tongarewa (NMNZ, Wellington) and Canterbury Museum (CM, Christchurch) (Supplementary Material: Table S1). Furthermore, stable isotope values reported here include samples taken from bones during fieldwork by Murray J. Williams (MJW), of which no voucher speci­ mens remain (Table S1). The bones were prepared and analysed at the Stable Isotope Laboratory of GNS Figure 1. Skull of A. chathamica (NMNZ S.029475), from Maunganui Beach, Chatham Island, showing the impression of Science (Lower Hutt, New Zealand). Bone collagen the salt glands above each orbital cavity (arrow). Photograph by extraction followed the protocol of Holdaway and Jean-Claude Stahl, Te Papa. Credit: NMNZ, CC BY-NC-ND 4.0.

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