Please use this identifier to cite or link to this item: http://hdl.handle.net/2381/33511
Title: Chemical, experimental, and morphological evidence for diagenetically altered melanin in exceptionally preserved fossils
Authors: Colleary, C.
Dolocan, A.
Gardner, J.
Singh, S.
Wuttke, M.
Rabenstein, R.
Habersetzer, J.
Schaal, S.
Feseha, M.
Clemens, M.
Jacobs, B. F.
Currano, E. D.
Jacobs, L. L.
Sylvestersen, R. L.
Gabbott, Sarah E.
Vinther, J.
First Published: 13-Oct-2015
Publisher: National Academy of Sciences
Citation: Proceedings of the National Academy of Sciences USA, 2015, 112 (41), pp. 12592-12597
Abstract: In living organisms, color patterns, behavior, and ecology are closely linked. Thus, detection of fossil pigments may permit inferences about important aspects of ancient animal ecology and evolution. Melanin-bearing melanosomes were suggested to preserve as organic residues in exceptionally preserved fossils, retaining distinct morphology that is associated with aspects of original color patterns. Nevertheless, these oblong and spherical structures have also been identified as fossilized bacteria. To date, chemical studies have not directly considered the effects of diagenesis on melanin preservation, and how this may influence its identification. Here we use time-of-flight secondary ion mass spectrometry to identify and chemically characterize melanin in a diverse sample of previously unstudied extant and fossil taxa, including fossils with notably different diagenetic histories and geologic ages. We document signatures consistent with melanin preservation in fossils ranging from feathers, to mammals, to amphibians. Using principal component analyses, we characterize putative mixtures of eumelanin and phaeomelanin in both fossil and extant samples. Surprisingly, both extant and fossil amphibians generally exhibit melanosomes with a mixed eumelanin/phaeomelanin composition rather than pure eumelanin, as assumed previously. We argue that experimental maturation of modern melanin samples replicates diagenetic chemical alteration of melanin observed in fossils. This refutes the hypothesis that such fossil microbodies could be bacteria, and demonstrates that melanin is widely responsible for the organic soft tissue outlines in vertebrates found at exceptional fossil localities, thus allowing for the reconstruction of certain aspects of original pigment patterns.
DOI Link: 10.1073/pnas.1509831112
eISSN: 1091-6490
Links: http://www.pnas.org/content/112/41/12592?tab=author-info
http://hdl.handle.net/2381/33511
Version: Publisher Version
Status: Peer-reviewed
Type: Journal Article
Rights: Copyright © 2015, the authors. Exclusive licensee: PNAS. Deposited with reference to the publisher’s Author rights and permissions policy, available at http://www.pnas.org/site/aboutpnas/authorfaq.xhtml
Appears in Collections:Published Articles, Dept. of Geology

Files in This Item:
File Description SizeFormat 
Collearyetal-2015.pdfPublished (publisher PDF)1.68 MBAdobe PDFView/Open


Items in LRA are protected by copyright, with all rights reserved, unless otherwise indicated.