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.

suck abstract from ncbi


10.1073/pnas.1615440114

http://scihub22266oqcxt.onion/10.1073/pnas.1615440114
suck pdf from google scholar
C5393229!5393229 !28348211
unlimited free pdf from europmc28348211
    free
PDF from PMC    free
html from PMC    free

Warning: file_get_contents(https://eutils.ncbi.nlm.nih.gov/entrez/eutils/elink.fcgi?dbfrom=pubmed&id=28348211 &cmd=llinks): Failed to open stream: HTTP request failed! HTTP/1.1 429 Too Many Requests in C:\Inetpub\vhosts\kidney.de\httpdocs\pget.php on line 215

suck abstract from ncbi

pmid28348211
      Proc+Natl+Acad+Sci+U+S+A 2017 ; 114 (15 ): 3867-3872
Nephropedia Template TP

gab.com Text

Twit Text FOAVip

Twit Text #

English Wikipedia


  • Evolution of the early Antarctic ice ages #MMPMID28348211
  • Liebrand D ; de Bakker AT ; Beddow HM ; Wilson PA ; Bohaty SM ; Ruessink G ; Pälike H ; Batenburg SJ ; Hilgen FJ ; Hodell DA ; Huck CE ; Kroon D ; Raffi I ; Saes MJ ; van Dijk AE ; Lourens LJ
  • Proc Natl Acad Sci U S A 2017[Apr]; 114 (15 ): 3867-3872 PMID28348211 show ga
  • Understanding the stability of the early Antarctic ice cap in the geological past is of societal interest because present-day atmospheric CO(2) concentrations have reached values comparable to those estimated for the Oligocene and the Early Miocene epochs. Here we analyze a new high-resolution deep-sea oxygen isotope (?(18)O) record from the South Atlantic Ocean spanning an interval between 30.1 My and 17.1 My ago. The record displays major oscillations in deep-sea temperature and Antarctic ice volume in response to the ?110-ky eccentricity modulation of precession. Conservative minimum ice volume estimates show that waxing and waning of at least ?85 to 110% of the volume of the present East Antarctic Ice Sheet is required to explain many of the ?110-ky cycles. Antarctic ice sheets were typically largest during repeated glacial cycles of the mid-Oligocene (?28.0 My to ?26.3 My ago) and across the Oligocene-Miocene Transition (?23.0 My ago). However, the high-amplitude glacial-interglacial cycles of the mid-Oligocene are highly symmetrical, indicating a more direct response to eccentricity modulation of precession than their Early Miocene counterparts, which are distinctly asymmetrical-indicative of prolonged ice buildup and delayed, but rapid, glacial terminations. We hypothesize that the long-term transition to a warmer climate state with sawtooth-shaped glacial cycles in the Early Miocene was brought about by subsidence and glacial erosion in West Antarctica during the Late Oligocene and/or a change in the variability of atmospheric CO(2) levels on astronomical time scales that is not yet captured in existing proxy reconstructions.
  • ?


  • DeepDyve
  • Pubget Overpricing
  • suck abstract from ncbi

    Linkout box