Use my Search Websuite to scan PubMed, PMCentral, Journal Hosts and Journal Archives, FullText. Kick-your-searchterm to multiple Engines kick-your-query now !>

A dictionary by aggregated review articles of nephrology, medicine and the life sciences Your one-stop-run pathway from word to the immediate pdf of peer-reviewed on-topic knowledge.

10.1073/pnas.1612147114 http://scihub22266oqcxt.onion/10.1073/pnas.1612147114 C5410786!5410786!28396389     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       Proc+Natl+Acad+Sci+U+S+A 2017 ; 114 (17): 4324-9 Nephropedia Template TP {{tp|p=28396389|t=2017. Subduction zone forearc serpentinites as incubators for deep microbial life |pdf=|usr=}}{{28396389}} gab.com Text Subduction zone forearc serpentinites as incubators for deep microbial life JO: Proc Natl Acad Sci U S A http://www.kidney.de/pget.php?&tw=1&pmid=28396389 #FOAvip We document organic matter encapsulated in rock clasts from a oceanic serpentinite mud volcano above the Izu?Bonin?Mariana subduction zone (Pacific Ocean). Although we cannot pinpoint the exact origin of the organic matter, chemical analysis of the constituents resembles molecular signatures that could be produced by microbial life deep within or below the mud volcano. Considering the known temperature limit for life, 122 °C, and the subduction zone forearc geotherm where such mud volcanoes are located, we estimate that life could exist as deep as ?10,000 m below the seafloor. This is considerably deeper than other active serpentinizing regions such as midocean ridges and could have provided sheltered ecosystems for life to survive the more violent phases of Earth?s history. Twit Text FOAVip Subduction zone forearc serpentinites as incubators for deep microbial life ????Proc Natl Acad Sci U S A http://www.kidney.de/pget.php?&tw=1&pmid=28396389 #FOAvip Twit Text # Free Paper on # # # # # LINK http://www.kidney.de/pget.php?&tw=1&pmid=28396389 #FOAvip English Wikipedia <ref>{{Cite pmid|28396389}}</ref> Subduction zone forearc serpentinites as incubators for deep microbial life #MMPMID28396389 Plümper O; King HE; Geisler T; Liu Y; Pabst S; Savov IP; Rost D; Zack T Proc Natl Acad Sci U S A 2017[Apr]; 114 (17): 4324-9 PMID28396389show ga We document organic matter encapsulated in rock clasts from a oceanic serpentinite mud volcano above the Izu?Bonin?Mariana subduction zone (Pacific Ocean). Although we cannot pinpoint the exact origin of the organic matter, chemical analysis of the constituents resembles molecular signatures that could be produced by microbial life deep within or below the mud volcano. Considering the known temperature limit for life, 122 °C, and the subduction zone forearc geotherm where such mud volcanoes are located, we estimate that life could exist as deep as ?10,000 m below the seafloor. This is considerably deeper than other active serpentinizing regions such as midocean ridges and could have provided sheltered ecosystems for life to survive the more violent phases of Earth?s history. äSubduction zone forearc serpentinites as incubators for deep microbial(epmc).pdf DeepDyve Pubget Overpricing