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10.1038/s41598-017-13821-2 http://scihub22266oqcxt.onion/10.1038/s41598-017-13821-2 C5670171!5670171!29101399     free     free     free Deprecated: Implicit conversion from float 211.6 to int loses precision in C:\Inetpub\vhosts\kidney.de\httpdocs\pget.php on line 534 Deprecated: Implicit conversion from float 211.6 to int loses precision in C:\Inetpub\vhosts\kidney.de\httpdocs\pget.php on line 534 Deprecated: Implicit conversion from float 211.6 to int loses precision in C:\Inetpub\vhosts\kidney.de\httpdocs\pget.php on line 534 Deprecated: Implicit conversion from float 211.6 to int loses precision in C:\Inetpub\vhosts\kidney.de\httpdocs\pget.php on line 534 Deprecated: Implicit conversion from float 211.6 to int loses precision in C:\Inetpub\vhosts\kidney.de\httpdocs\pget.php on line 534       Sci+Rep 2017 ; 7 (ä): ä Nephropedia Template TP {{tp|p=29101399|t=2017. Enhanced Arctic Amplification Began at the Mid-Brunhes Event ~400,000 years ago |pdf=|usr=}}{{29101399}} gab.com Text Enhanced Arctic Amplification Began at the Mid-Brunhes Event ~400,000 years ago JO: Sci Rep http://www.kidney.de/pget.php?&tw=1&pmid=29101399 #FOAvip Arctic Ocean temperatures influence ecosystems, sea ice, species diversity, biogeochemical cycling, seafloor methane stability, deep-sea circulation, and CO2 cycling. Today?s Arctic Ocean and surrounding regions are undergoing climatic changes often attributed to ?Arctic amplification? ? that is, amplified warming in Arctic regions due to sea-ice loss and other processes, relative to global mean temperature. However, the long-term evolution of Arctic amplification is poorly constrained due to lack of continuous sediment proxy records of Arctic Ocean temperature, sea ice cover and circulation. Here we present reconstructions of Arctic Ocean intermediate depth water (AIW) temperatures and sea-ice cover spanning the last ~ 1.5 million years (Ma) of orbitally-paced glacial/interglacial cycles (GIC). Using Mg/Ca paleothermometry of the ostracode Krithe and sea-ice planktic and benthic indicator species, we suggest that the Mid-Brunhes Event (MBE), a major climate transition ~ 400?350 ka, involved fundamental changes in AIW temperature and sea-ice variability. Enhanced Arctic amplification at the MBE suggests a major climate threshold was reached at ~ 400 ka involving Atlantic Meridional Overturning Circulation (AMOC), inflowing warm Atlantic Layer water, ice sheet, sea-ice and ice-shelf feedbacks, and sensitivity to higher post-MBE interglacial CO2 concentrations. Twit Text FOAVip Enhanced Arctic Amplification Began at the Mid-Brunhes Event ~400,000 years ago ????Sci Rep http://www.kidney.de/pget.php?&tw=1&pmid=29101399 #FOAvip Twit Text # Free Paper on # # # # # LINK http://www.kidney.de/pget.php?&tw=1&pmid=29101399 #FOAvip English Wikipedia <ref>{{Cite pmid|29101399}}</ref> Enhanced Arctic Amplification Began at the Mid-Brunhes Event ~400,000 years ago #MMPMID29101399 Cronin TM; Dwyer GS; Caverly EK; Farmer J; DeNinno LH; Rodriguez-Lazaro J; Gemery L Sci Rep 2017[]; 7 (ä): ä PMID29101399show ga Arctic Ocean temperatures influence ecosystems, sea ice, species diversity, biogeochemical cycling, seafloor methane stability, deep-sea circulation, and CO2 cycling. Today?s Arctic Ocean and surrounding regions are undergoing climatic changes often attributed to ?Arctic amplification? ? that is, amplified warming in Arctic regions due to sea-ice loss and other processes, relative to global mean temperature. However, the long-term evolution of Arctic amplification is poorly constrained due to lack of continuous sediment proxy records of Arctic Ocean temperature, sea ice cover and circulation. Here we present reconstructions of Arctic Ocean intermediate depth water (AIW) temperatures and sea-ice cover spanning the last ~ 1.5 million years (Ma) of orbitally-paced glacial/interglacial cycles (GIC). Using Mg/Ca paleothermometry of the ostracode Krithe and sea-ice planktic and benthic indicator species, we suggest that the Mid-Brunhes Event (MBE), a major climate transition ~ 400?350 ka, involved fundamental changes in AIW temperature and sea-ice variability. Enhanced Arctic amplification at the MBE suggests a major climate threshold was reached at ~ 400 ka involving Atlantic Meridional Overturning Circulation (AMOC), inflowing warm Atlantic Layer water, ice sheet, sea-ice and ice-shelf feedbacks, and sensitivity to higher post-MBE interglacial CO2 concentrations. äEnhanced Arctic Amplification Began at the Mid-Brunhes Event ~400,000 (epmc).pdf DeepDyve Pubget Overpricing