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Natural Science Forum / Biology / Paleontology / September 2004



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Pikaia...  Earlier Cordates?

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Brett Aubrey - 13 Sep 2004 04:40 GMT
Question follows Wikipedia excerpt...

*****
Pikaia
From Wikipedia, the free encyclopedia.
Pikaia is a Middle Cambrian fossil found near Mount Pika in the Burgess
Shale by Walcott. Described by him in 1911 and classified as a Polychaete
worm, based on the obvious and regular segmentation of the body.

Conway Morris placed Pikaia gracilens in the chordates in 1979, which
probably makes it one of the oldest ancestors of the modern vertebrates.

Retrieved from "http://en.wikipedia.org/wiki/Pikaia"
*****

Can anyone point me to chordates (or chordate candidates) predating Pikaia
(~550MYA)?  TIA.

Regards,  Brett Aubrey.
Gautam Majumdar - 13 Sep 2004 20:29 GMT
> Can anyone point me to chordates (or chordate candidates) predating
> Pikaia (~550MYA)?  TIA.

Chen J Y, Dzik J, Edgecombe G D, Ramskold L, Zhou G Q, A possible early
Cambrain chordate, Nature 1995; 377: 720-22

Shu D G, Conway Morris S, Zhang X L, A Pikaia-like chordate from the Lower
Cambrian of China, Nature 1996; 384: 157-58 (Claimed Yunnanozoon was a
Chordate)

The above two claims were disputed. See : Shu D, Zhang X, Chen L,
Reinterpretation of Yunnanozoon as the earliest known hemichordate, Nature
1996; 380: 428-30

Shu D, Luo H, Conway Morris S, Zhang X, Hu S, Chen L, Han J, Zhu M, Li Y,
Chen L, Lower Cambrian vertebrates from south China, Nature 1999; 402:
42-46 (Description of two species from Early Cambrian - Myllokunmingia &
Haikouichthys)

Janvier P, Catching the first fish, Nature 1999; 402: 21-22 (Review of the
Cambrian chordates)

Xian-guang H, Aldridge R J, Siveter D J, Siveter D J, Xiang-hong F, New
evidence on the anatomy and phylogeny of the earliest vertebrates,
Proceedings of The Royal Society Biological Sciences 2002; 269: 1865-69
(Two previously described species from lower Cambrian - Myllokunmingia &
Haikouichthys - were shown to be the same species)

Sheep farmer finds oldest fossil,
http://news.bbc.co.uk/1/hi/sci/tech/3208583.stm (This claim of a Chordate
from Precambrian is disputed - other palaeontologists think it is a
kimberella - a basal mollusc. This one has not been published in a
peer-reviewed journal yet)

HTH

Signature

Gautam Majumdar

Please send e-mails to gmajumdar@freeuk.com

John Harshman - 13 Sep 2004 20:45 GMT
> Question follows Wikipedia excerpt...
>
[quoted text clipped - 13 lines]
> Can anyone point me to chordates (or chordate candidates) predating Pikaia
> (~550MYA)?  TIA.

Gautam Majumdar has given you the list of references I would have if I'd
been quicker. I'll content myself with some quibbles. Pikaia (and the
Burgess Shale) are considerably younger than you say, somewhere around
520ma or a bit younger. Dates in the Cambrian have recently been moved
up a bit. The period now starts at 543ma and ends at 490ma. The other
chordate candidates are mostly from the Chengjiang fauna, perhaps as
much as 10ma earlier than the Burgess.
Brett Aubrey - 15 Sep 2004 00:15 GMT
> > Question follows Wikipedia excerpt...
> > *****
< snip >
"http://en.wikipedia.org/wiki/Pikaia"
> > *****
> > Can anyone point me to chordates (or chordate candidates) predating Pikaia
[quoted text clipped - 7 lines]
> chordate candidates are mostly from the Chengjiang fauna, perhaps as
> much as 10ma earlier than the Burgess.

Thanks, Gautham and John.
Don Kenney - 16 Sep 2004 00:02 GMT
>> Question follows Wikipedia excerpt...
>>
[quoted text clipped - 21 lines]
>chordate candidates are mostly from the Chengjiang fauna, perhaps as
>much as 10ma earlier than the Burgess.

As you say, Cambrian dates have been in a state of flux for a couple
of decades.  The difference between Chengjiang and the Mt Stephens
beds may be even more than 10ma.  A couple of years ago, the
Lower-Cambrian Middle Cambrian boundary in New Brunswick was
radiometrically dated at 511ma.  Which would make the Burgess Shale
even younger if it doesn't turn out that the Lower-Middle Cambrian
boundary in Western North America isn't the same as in New Brunswick.

And I believe that the Chengjiang beds are very close to the classical
start of the Lower Cambrian -- first trilobites.  I've sort of lost
track of when that would be, and even if I knew, it's probably
changed.  ... But maybe around 525ma?  So the Burgess might be 20
million years or more younger than the Maotianshan Shales.

And one other possible early chordate.  Emmonaspis from the Lower
Cambrian of Vermont.

There are articles on both the Maotianshan chordates and Emmonaspis in
the Wikipedia.  

http://en.wikipedia.org/wiki/Maotianshan_shales
http://en.wikipedia.org/wiki/Emmonaspis
Brett Aubrey - 16 Sep 2004 01:22 GMT
<snip>
> >Gautam Majumdar has given you the list of references I would have if I'd
> >been quicker. I'll content myself with some quibbles. Pikaia (and the
[quoted text clipped - 7 lines]
> of decades.  The difference between Chengjiang and the Mt Stephens
> beds

Your Mt. Stephen comment struck me...  Mt  Stephen is on the south side of
Highway 1 while Mt. Burgess (Walcott's initial find) is on the north.  Is
the Burgess Shale on both mountains?  Others as well (Mt. Field and Wapta
Mountain, e.g., both closer than Mt. Stephen)?  TIA.  Regards, Brett Aubrey.

<snip>
Don Kenney - 17 Sep 2004 10:01 GMT
><snip>
>> >Gautam Majumdar has given you the list of references I would have if I'd
[quoted text clipped - 15 lines]
>
><snip>

I believe that the Stephen Formation is exposed in a number of places
along a front of -- as I recall -- 35 km or so in Yoho National Park.
As I rememberl the story, Desmond Collins had trouble getting permits
to dig at Walcott's original quarry a few decades ago, so he asked for
permits to look for additional sites, then when out and found a number
of them.  You could try a Google search on Desmond Collins.  He used
to have a very interesting paper posted somewhere on the Internet that
described -- as I recall -- six different faunas with at least some
soft bodied members from the Stephen Formation -- of which the Burgess
is only one member.
John Harshman - 16 Sep 2004 01:51 GMT
>>>Question follows Wikipedia excerpt...
>>>
[quoted text clipped - 27 lines]
> Lower-Cambrian Middle Cambrian boundary in New Brunswick was
> radiometrically dated at 511ma.

You may be right. But do you have a reference for the 511ma date? I was
going by memory. However, Bowring & Martin in Briggs & Crowther's
Palaeobiology II (a great general reference, by the way) are actually a
bit more precise than I had remembered. They put the Upper-Middle
boundary at 500ma, Lower-Middle boundary at 514ma, and the lower
boundary of the Atdabanian (first trilobites) at 525ma. Also according
to Palaeobiology II, the Chengjiang is near the top of the Tommotian
(just before those trilobites appear), at about 525ma.  Assuming all
that, it's possible that there's as much as 25 million years between the
Chengjiang and Burgess, or as little as 11. Given the strong similarity
of the biotas, I would guess that they were closer in time than the maximum.

> Which would make the Burgess Shale
> even younger if it doesn't turn out that the Lower-Middle Cambrian
[quoted text clipped - 14 lines]
> http://en.wikipedia.org/wiki/Maotianshan_shales 
> http://en.wikipedia.org/wiki/Emmonaspis
Don Kenney - 17 Sep 2004 09:52 GMT
>>>>Question follows Wikipedia excerpt...
>>>>
[quoted text clipped - 29 lines]
>
>You may be right. But do you have a reference for the 511ma date?

I've seen it in several places.  This one looks credible (to me
anyway):

http://www.uni-wuerzburg.de/palaeontologie/Stuff/casu6.htm

> I was
>going by memory. However, Bowring & Martin in Briggs & Crowther's
[quoted text clipped - 26 lines]
>> http://en.wikipedia.org/wiki/Maotianshan_shales 
>> http://en.wikipedia.org/wiki/Emmonaspis
 
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