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Post by surroundx on Nov 14, 2016 9:47:43 GMT
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Post by surroundx on Nov 14, 2016 12:07:20 GMT
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Post by surroundx on Aug 1, 2017 10:42:39 GMT
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Post by Melanie on Feb 14, 2018 18:56:39 GMT
Cloutier, Sackton, Grayson, Edwards, Baker. [2018.] First nuclear genome assembly of an extinct moa species, the little bush moa (Anomalopteryx didiformis). bioRxiv 262816. [ bioRxiv preprint]
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Post by surroundx on Jul 15, 2018 2:45:07 GMT
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Post by surroundx on Dec 18, 2018 12:56:54 GMT
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Post by Melanie on Jul 17, 2019 13:49:42 GMT
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Post by Melanie on May 30, 2021 7:52:40 GMT
Jamie R. Wood, Melanie J. Vermeulen, Nicola Bolstridge, Shar Briden, Theresa L. Cole, Jessica Rivera-Perez, Lara D. Shepherd, Nicolas J. Rawlence & Janet M. Wilmshurstaf, 2021 Mid-Holocene coprolites from southern New Zealand provide new insights into the diet and ecology of the extinct little bush moa (Anomalopteryx didiformis)Quaternary Science Reviews. 263: Article 106992. doi: 10.1016/j.quascirev.2021.106992Abstract: Mid-Holocene coprolites from southern New Zealand provide new insights into the diet and ecology of the extinct little bush moa (Anomalopteryx didiformis)Knowledge about the diets of New Zealand's extinct moa (Aves: Dinornithiformes) is heavily biased towards just three species ( Dinornis robustus, Megalapteryx didinus and Pachyornis elephantopus), which represent about 90% of all identified coprolites and gizzard content samples. By comparison, the diets of the other six moa species are poorly known. Here, we report the discovery of a new coprolite deposit attributed to little bush moa ( Anomalopteryx didiformis) based on DNA barcoding and former moa species distributions. The deposit is the southernmost site from which moa coprolites have been recovered and just the second to contain mid-Holocene specimens. Moreover, the deposit provides the longest known temporal span (∼2200 years) of moa coprolites within a stratigraphic context. Pollen and plant DNA from the coprolites, as well as associated plant macrofossils, indicate that the deposit spans a period when the forest canopy was transitioning from Podocarpaceae to silver beech ( Lophozonia menziesii) dominance about 6800–4600 years ago. Our analysis of coprolite content supports the current hypothesis that little bush moa browsed trees and shrubs within the forest understorey, but provides new evidence that ferns were also an important part of their diet. Based on this finding, we suggest that moa might once have played a previously unrecognised role in the dispersal of ground fern spores throughout New Zealand forests.
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Post by Melanie on May 24, 2024 21:41:20 GMT
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Post by Melanie on Jun 12, 2024 17:33:57 GMT
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Post by Sebbe on Oct 27, 2024 8:21:08 GMT
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Post by Sebbe on Oct 27, 2024 8:48:21 GMT
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