Сотворение Земли. Как живые организмы создали наш мир

Haug J. T., Caron J.-B., Haug C. 2013. Demecology in the Cambrian: synchronized molting in arthropods from the Burgess Shale // BMC Biology, 11, 64. DOI: 10.1186/1741-7007-11-64

Hints O. et al. 2010. Biodiversity patterns of Ordovician marine microphytoplankton from Baltica: Comparison with other fossil groups and sea-level changes // Palaeogeography, Palaeoclimatology, Palaeoecology, 294, 161–73.

Holland P. W. H. 2015. Did homeobox gene duplications contribute to the Cambrian explosion? // Zoological Letters, 1, 1. DOI: 10.1186/s40851-014-0004-x

Janvier P. 1996. Early Vertebrates. Oxford: Oxford Univ. Press, 393 p. (Oxford Monographs on Geology and Geophysics, 33).

Klemetsen A. 2010. The charr problem revisited: exceptional phenotypic plasticity promotes ecological speciation in postglacial lakes // Freshwater Reviews, 3, 49–74.

Kowalewski M., Kelley P. H., eds. 2002. The Fossil Record of Predation // Paleontological Society Papers, 8, 1–398.

Kröger B., Vinther J., Fuchs D. 2011. Cephalopod origin and evolution: A congruent picture emerging from fossils, development and molecules // Bioessays, 33, 602–13.

Krumbein W. E., Paterson D. M., Stal L. J., eds. 1994. Biostabilization of Sediments. Oldenburg: Bibliotheks und Informationssystem der Carl von Ossietzky Universität, 526 p.

Lamsdell J. C., Hoşgör I., Selden P. A. 2013. A new Ordovician eurypterid (Arthropoda: Chelicerata) from southeastern Turkey: Evidence for a cryptic Ordovician record of Eurypterida // Gondwana Research, 23, 354–66.

Lee M. S. Y., Soubrier J., Edgecombe G. D. 2013. Rates of phenotypic and genomic evolution during the Cambrian Explosion // Current Biology, 23, 1889–95.

Lenton T. M. et al. 2014. Co-evolution of eukaryotes and ocean oxygenation in the Neoproterozoic era // Nature Geoscience, 7, 257–65.

Logan G. A. et al. 1995. Terminal Proterozoic reorganization of biogeochemical cycles // Nature, 376, 53–6.

Ma X., Edgecombe G. D., Hou X., Goral T., Strausfeld N. J. 2015. Preservational pathways of corresponding brains of a Cambrian euarthropod // Current Biology, 25, 1–7. DOI: 10.1016/j.cub.2015.09.063

Marshall D. J., Lamsdell J. C., Shpinev E., Braddy S. J. 2013. A diverse chasmataspidid (Arthropoda: Chelicerata) fauna from the Early Devonian (Lochkovian) of Siberia // Palaeontology, 57, 631–55.

Martin R. E., Quigg A., Podkovyrov V. 2008. Marine biodiversification in response to evolving phytoplankton stoichiometry // Palaeogeography, Palaeoclimatology, Palaeoecology, 258, 277–91.

Meysman F. J. R., Middelburg J. J., Heip C. H. R. 2006. Bioturbation: a fresh look at Darwin’s last idea // TRENDS in Ecology and Evolution, 21, 688–95.

Mills D. B., Canfield D. E. 2016. A trophic framework for animal origins // Geobiology, 15, 197–210.

Moysiuk J., Smith M. R., Caron J.-B. 2017. Hyoliths are Palaeozoic lophophorates // Nature, 541, 394–7.

Müller K. J., Walossek D. 1987. Morphology, ontogeny and life-habit of Agnostus pisiformis from the Upper Cambrian of Sweden // Fossils and Strata, 19, 1–124.

Ortega-Hernández J., Van Roy P., Lerosey-Aubril R. 2016. A new aglaspidid euarthropod with a six-segmented trunk from the Lower Ordovician Fezouata Konservat-Lagerstätte, Morocco // Geological Magazine, 253, 524–36.

Parker A. R. 2011. On the origin of optics // Optics & Laser Technology, 43, 323–9.

Penny A. M., Wood R. A., Zhuravlev A. Yu., Curtis A., Bowyer F., Tostevin R. 2017. Intraspecific variation in an Ediacaran skeletal metazoan: Namacalathus from the Nama Group, Namibia // Geobiology, 15, 81–93.

Pruss S. B., Finnegan S., Fischer W. W., Knoll A. H. 2011. Carbonates in skeleton-poor seas: New insights from Cambrian and Ordovician strata of Laurentia // Palaios, 25, 73–84.