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Re(3): All kinds of odd observat...



Thanks for the insights on burrowing and its relation to the K/T boundary
problem, Norm.  I had read Chuck Savrda's 1993 paper in _Geology_ on how he
showed a noncatastrophic origin for the K/T boundary in the U.S. Gulf Coast,
based on trace fossil evidence; I'll have to go back and read it again.  Is
this the paper you referred to or did I miss a more recent one in _Geology_? 
Incidentally, he's a neighbor of mine (relatively speaking) here in the
southeastern U.S., so I also remember talking with him about some of his
conclusions before the 1993 paper was published.  Apparently his evidence
disappointed some people who wanted a tsunamite to be there.

A similar form of disappointment happened on a field trip to the K/T boundary
in the Pote Quarry of Recife, Brazil, last year (associated with the ISC
meeting there).  Some of us ichnologists on the field trip found burrows in
the "tsunamite" that had been interpreted there (no burrows had been reported
before), so a lot of controversy erupted right there at the outcrop about
whether it was a catastrophic deposit or not.  (The ichnolgists and some other
sedimentologists said "not.")  It was pretty fun to witness and participate.

I had talked briefly with Tony Ekdale about some of his work on the "burrowing
problem" but hadn't read the paper in the Copenhagen K/T symposium volume. 
Fortunately, I'll get to talk with both him and Richard Bromley about it in
Denmark next month - the Third International Ichnofabric Workshop will be
meeting there.  I'm sure it'll be a fun topic for discussion and I'll be glad
to share my impressions.  Unfortunately (for me!), I'll miss the part of the
workshop field trip that visits the K/T boundary at Stevns Klint.

Just out of curiousity - how far apart (lithostratigraphically) are the
multiple anomalies at Brazos and Braggs?  Some burrow systems, such as
_Thalassinoides_ or _Ophiomorpha_, have vertical extents of 2-3 meters.  Not
to be a constant devil's advocate, but I'd like to see more accounting for the
effects of bioturbation in the light of such possibilities.

Anthony Martin
Geosciences Program, Emory University
Atlanta, Georgia  USA



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