NASA/Spacelink

  5/9/91: NASA DISCOVERS IMPACT LIKELY TIED TO DINOSAURS' DEMISE

  RELEASE: 91-71

        The  first  surface evidence of a buried impact crater formed
  by a comet or asteroid which may have caused the extinction of  the
  dinosaurs has been discovered by NASA researchers.

        The   scientists   believe  a  ring  of  sink  holes  in  the
  northwestern corner of the Mexican state of  Yucatan  outlines  the
  largest  known  impact  crater  on Earth. The crater, which is more
  than 125 miles in diameter, is a prime candidate in the search  for
  an  impact  that  may  have  caused  the planet-wide extinctions of
  dinosaurs and other species about 65 million years ago.

        Charles Duller  of  NASA's  Ames  Research  Center,  Mountain
  View, Calif., discovered the ring formation in 1987 while searching
  satellite imagery for water sources used by ancient Mayan cities.

        Two  other  members  of  the research team -- Dr. Kevin Pope,
  formerly of Ames and now with Geo Eco Arc Research  in  La  Canada,
  Calif.  and  Adriana  Ocampo  of  NASA's Jet Propulsion Laboratory,
  Pasadena, Calif. -- considered many other  geological  explanations
  before  concluding  the  formation  was  caused  by a buried impact
  crater.

        "The apparent age, location and size of the proposed  Yucatan
  impact   make  it  one  of  the  best  candidates  for  the  global
  catastrophic event, although multiple impacts remain a possibility.
  Regardless, the Yucatan impact alone would have had  a  devastating
  impact  on  the climate, animals and plant life of the Earth," Pope
  said.

        Some scientists believe such an impact pushed  so  much  dust
  and   debris   into   the   atmosphere  that  it  blocked  sunlight,
  interrupting the growth of plants,  starving  dinosaurs  and  other
  animals and freezing much of the Earth.

        The  results  of  the  study  by Duller, Pope and Ocampo were
  announced in the current issue of Nature magazine.

        The team's findings agree with the work of  other  scientists
  who  have  found unusual circular gravity and magnetic patterns and
  quartz fractured by an impact, all suggesting a  buried  crater  in
  the Yucatan.

        The  circular  hydro-geological feature, which they named the
  Cenote Ring (cenote is the local  Spanish  name  for  sink  holes),
  provides  surface  evidence of the buried crater's precise location
  and size.  It is centered near the town of Chicxulub, for which the
  buried crater is named.

        Duller mapped hundreds of water-filled sink holes which  form
  an  almost  perfect  semicircle that marks the crater's buried rim.
  Fresh water springs well up beneath the surface  where  the  Cenote
  Ring meets the shore line.

        The  sink  holes  are  found in clusters at some places along
  the rim and spaced up to a mile apart at others.  They average  300
  - 500 feet in diameter.

        Duller  and  Pope determined the half-circle of sink hole and
  severely fractured limestone outside and along the rim area.   This
  conclusion   was   verified   through  independent  hydrogeological
  research conducted by Dr. Luis Marin,  now  of  the  University  of
  Mexico, during his work on a doctoral thesis under Dr. Eugene Perry
  at Northern Illinois University.

        "As  the  buried  crater  rim settles over millions of years,
  the rock  on  top  slumps  and  cracks.   Underground  water  flows
  through the cracks on its way to the ocean.  As the water is forced
  around  the  unfractured rock in the center, the flow dissolves the
  limestone, causing cave-ins that create the sink holes," Pope said.

        Pope and Ocampo examined core sample data taken  from  nearby
  exploratory  oil  wells and found they geologically date the buried
  crater's floor at Late Cretaceous about 65 million years ago.   The
  crater floor has younger Tertiary sediments on top.

        According  to  the  fossil  record, more than half of Earth's
  plant and animal  species,  including  the  dinosaurs,  disappeared
  about  65  million  years  ago.  This abrupt change in evolutionary
  history occurred between the Cretaceous  and  Tertiary  periods  in
  Earth's  geologic  history  and  is  called the Cretaceous-Tertiary
  (K-T) boundary.

        Unusual amounts of the rare element iridium -- more  abundant
  in comets and asteroids than on Earth -- have been found in the K-T
  boundary in many locations worldwide, leading scientists to believe
  that   a  large  extraterrestrial  impact  caused  the  planet-wide
  extinctions.

        Rock and melted glassy fragments, "blown out" by  an  impact,
  have been found in the Caribbean and Gulf of Mexico region, causing
  scientists to concentrate the search for the suspect crater in this
  area.   Deposits  and erosion patterns produced by a gigantic tidal
  wave have been found at the K-T boundary in Texas,  Mexico  and  in
  cores from the Gulf of Mexico.

        "Our   research,"  Duller  said,  "adds  one  more  piece  of
  evidence  to  a  complex  and  intriguing  jigsaw   puzzle.    Many
  researchers  in different scientific fields have contributed to our
  understanding of the Yucatan impact.  Each additional piece  brings
  us  closer  to  understanding  one  of  the  great mysteries in the
  evolution of life on Earth."