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10.1007/s12542-017-0345-9 http://scihub22266oqcxt.onion/10.1007/s12542-017-0345-9 C5487870!5487870!28680185     free     free     free Deprecated: Implicit conversion from float 213.6 to int loses precision in C:\Inetpub\vhosts\kidney.de\httpdocs\pget.php on line 534 Deprecated: Implicit conversion from float 213.6 to int loses precision in C:\Inetpub\vhosts\kidney.de\httpdocs\pget.php on line 534       Palaontol+Z 2017 ; 91 (2): 223-35 Nephropedia Template TP {{tp|p=28680185|t=2017. Graptolites from glacial erratics of the Laerheide area, northern Germany |pdf=|usr=}}{{28680185}} gab.com Text Graptolites from glacial erratics of the Laerheide area, northern Germany JO: Palaontol Z http://www.kidney.de/pget.php?&tw=1&pmid=28680185 #FOAvip Ordovician and Silurian glacial erratics of the Laerheide area (Lower Saxony, north-western Germany) bear well-preserved graptolites. The faunas provide important information on the origin and transport direction of the sediments preserved in a kame, representing the Drenthe stadial of the Saalian glaciation. The faunas even include species not commonly encountered in the successions of mainland Sweden, from where the erratics presumably originated. The most common graptolites are from Upper Ordovician (Sandbian to Katian) limestones and from Katian black shales. More common, however, are greenish limestones, sand- and siltstones, often combined in the term ?Grünlich-Graues Graptolithengestein?, in which upper Wenlock to Ludlow (upper Silurian) graptolites are common. Twit Text FOAVip Graptolites from glacial erratics of the Laerheide area, northern Germany ????Palaontol Z http://www.kidney.de/pget.php?&tw=1&pmid=28680185 #FOAvip Twit Text # Free Paper on # # # # # LINK http://www.kidney.de/pget.php?&tw=1&pmid=28680185 #FOAvip English Wikipedia <ref>{{Cite pmid|28680185}}</ref> Graptolites from glacial erratics of the Laerheide area, northern Germany #MMPMID28680185 Maletz J; Schöning H Palaontol Z 2017[]; 91 (2): 223-35 PMID28680185show ga Ordovician and Silurian glacial erratics of the Laerheide area (Lower Saxony, north-western Germany) bear well-preserved graptolites. The faunas provide important information on the origin and transport direction of the sediments preserved in a kame, representing the Drenthe stadial of the Saalian glaciation. The faunas even include species not commonly encountered in the successions of mainland Sweden, from where the erratics presumably originated. The most common graptolites are from Upper Ordovician (Sandbian to Katian) limestones and from Katian black shales. More common, however, are greenish limestones, sand- and siltstones, often combined in the term ?Grünlich-Graues Graptolithengestein?, in which upper Wenlock to Ludlow (upper Silurian) graptolites are common. äGraptolites from glacial erratics of the Laerheide area, northern Germ(epmc).pdf DeepDyve Pubget Overpricing