Entry Hoffman:2000:SE from sciam2000.bib

Last update: Sat Oct 14 03:06:25 MDT 2017                Valid HTML 3.2!

Index sections

Top | Symbols | Math | A | B | C | D | E | F | G | H | I | J | K | L | M | N | O | P | Q | R | S | T | U | V | W | X | Y | Z

BibTeX entry

@Article{Hoffman:2000:SE,
  author =       "Paul F. Hoffman and Daniel P. Schrag",
  title =        "Snowball {Earth}",
  journal =      j-SCI-AMER,
  volume =       "282",
  number =       "1",
  pages =        "68--75",
  month =        jan,
  year =         "2000",
  CODEN =        "SCAMAC",
  DOI =          "https://doi.org/10.1038/scientificamerican0100-68",
  ISSN =         "0036-8733 (print), 1946-7087 (electronic)",
  ISSN-L =       "0036-8733",
  bibdate =      "Fri May 17 10:26:08 MDT 2013",
  bibsource =    "http://www.math.utah.edu/pub/tex/bib/sciam2000.bib;
                 http://www.sciam.com/2000/0100issue/0100quicksummary.html",
  URL =          "http://www.nature.com/scientificamerican/journal/v282/n1/pdf/scientificamerican0100-68.pdf;
                 http://www.sciam.com/2000/0100issue/0100hoffman.html",
  abstract =     "A revolutionary hypothesis suggests that hundreds of
                 millions of years ago, ice up to a kilometer thick
                 engulfed even the tropics, snuffing out most life. A
                 runaway greenhouse effect ended the deep freeze but
                 baked the planet. These brutal climate reversals might
                 have encouraged the rise of multicellular organisms.",
  acknowledgement = ack-nhfb,
  fjournal =     "Scientific American",
  journal-URL =  "http://www.nature.com/scientificamerican",
}

Related entries