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10.1038/s41467-018-04311-8 http://scihub22266oqcxt.onion/10.1038/s41467-018-04311-8 C5953921!5953921!29765030     free     free     free       Nat+Commun 2018 ; 9 (ä): ä Nephropedia Template TP {{tp|p=29765030|t=2018. Early Cambrian origin of the shelf sediment mixed layer |pdf=|usr=}}{{29765030}} gab.com Text Early Cambrian origin of the shelf sediment mixed layer JO: Nat Commun http://www.kidney.de/pget.php?&tw=1&pmid=29765030 #FOAvip The mixed layer of modern oceans is a zone of fully homogenized sediment resulting from bioturbation. The mixed layer is host to complex biogeochemical cycles that directly impact ecosystem functioning, affecting ocean productivity and marine biodiversity. The timing of origin of the mixed layer has been controversial, with estimates ranging from Cambrian to Silurian, hindering our understanding of biogeochemical cycling and ecosystem dynamics in deep time. Here we report evidence from the Global Stratotype Section and Point (GSSP) of the basal Cambrian in the Burin Peninsula of Newfoundland, Canada, showing that a well-developed mixed layer of similar structure to that of modern marine sediments was established in shallow marine settings by the early Cambrian (approximately 529 million years ago). These findings imply that the benthos significantly contributed to establishing new biogeochemical cycles during the Cambrian explosion. Twit Text FOAVip Early Cambrian origin of the shelf sediment mixed layer ????Nat Commun http://www.kidney.de/pget.php?&tw=1&pmid=29765030 #FOAvip Twit Text # Free Paper on # # # # # LINK http://www.kidney.de/pget.php?&tw=1&pmid=29765030 #FOAvip English Wikipedia <ref>{{Cite pmid|29765030}}</ref> Early Cambrian origin of the shelf sediment mixed layer #MMPMID29765030 Gougeon RC; Mángano MG; Buatois LA; Narbonne GM; Laing BA Nat Commun 2018[]; 9 (ä): ä PMID29765030show ga The mixed layer of modern oceans is a zone of fully homogenized sediment resulting from bioturbation. The mixed layer is host to complex biogeochemical cycles that directly impact ecosystem functioning, affecting ocean productivity and marine biodiversity. The timing of origin of the mixed layer has been controversial, with estimates ranging from Cambrian to Silurian, hindering our understanding of biogeochemical cycling and ecosystem dynamics in deep time. Here we report evidence from the Global Stratotype Section and Point (GSSP) of the basal Cambrian in the Burin Peninsula of Newfoundland, Canada, showing that a well-developed mixed layer of similar structure to that of modern marine sediments was established in shallow marine settings by the early Cambrian (approximately 529 million years ago). These findings imply that the benthos significantly contributed to establishing new biogeochemical cycles during the Cambrian explosion. äEarly Cambrian origin of the shelf sediment mixed layer (epmc).pdf DeepDyve Pubget Overpricing