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Pregunta Yacimientos, Ejercicios de Paleontología

Asignatura: Paleontologia, Profesor: Leopoldo Marquez Sanz, Carrera: Biologia, Universidad: UV

Tipo: Ejercicios

2017/2018

Subido el 28/06/2018

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3. 4 Lagerstätten
341 Exceptional l y Prese r v ed Fossils
DEGBRI G CS
colìfintu >L) c e rt, l]ïl vt t i n\ a n d wl1aA pnJcesses lead tk
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Introduction
Extr a ordina r y fossil occ u r r enc e s a r e c om m only refe r r e d
to as FossilLagerstät t en (s e e Seila c her et i1/1985)Two
ty p es o f Fo s s ilLagerstät t e n are n o r m a l l y re c o gniz e d : (1)
con c entration depo s its, wher e the o cc u rr e n c e is r e ma
able for the sheer abu n dan c e of spe c ime n s (egBo n e
beds, c o quina s ) and (2) co n s e r v a tion deposits w here
the pr e s e r v ation is o f u n u su a l quality (egArticulated
skeletons, fossilized soft tissue s )Co n c e ntration depo s its
(Konze n tratLagerstätten) ty p ic a l l y a c c umulate o v er a
significa n t period of time a nd the fossils have the r efore
been s u bje c ted to time a v eraging (s e e Sectio n 3 2 7)
Cons e r v a tion deposits (Kons e r v atLagersti
t t e n ), on the
othe r hand, are u s ually the re su lt of a c atastr o phic e v e n t,
s u ch as rapid bu r ial, and r e present a n instant in ge
o
gic a l timeCons e rvation deposits have attractetl more
attentio n be c au s e o f their higher info r mation content
particula r ly tho s e that pre s e r v e the n onbiomine r alized
(soc a lledsoft') tissu e s o f orga n isms, which are the
fo c us he r eTheir majo r impo r tanc e to the study of the
history of life lies in the much more complete picture of
a n cie n t commu n itie s that they afford, compared to the
normal fo s sil reco r d of ha r d skeletons
The histo r y of l i fe a n d the
distribution of the co n tinents
Kons e rvatLage r s täuen are abu n da t parhm0
ar s
tings du r ing differe n t inte n ,ì. of ge0l 0 ca: timtThe
distribution of the s et aphL)nomi whd owi i5 C
l
trolled largely by m a jor e
\ e n ts in the e vL\0
utio n of life
and by the clistributiL)
n LìF the c o n tinents 4 A0listìn and
Brigg s 199 1, 199 3)
Prior to the appe a rance LìF biA
ìmineralizeL
l skeleton s /n
the late Prec a mbrin,
md E,
triv Cambrian ( e e fie(tio n
122), special conlitiL) ns w e r e required tor pr e s e r ation
T h e wi d e s pre l Ll ooc11r r enc e L\f E dia c a r a n fos ils in
shallow marine settings r etle c ts the a bse nc e tìf grazing
invertt brates[ ì nLï the re s i 1ltdnt prevalence of micr oha+
mats (md tgmunLìs : Seilacher 1999)The diver iDcation
of inw?rtebr a tus in the Cambria n e nsur e d that mi cmbi 1l
The c o ntext and style o f pr e s e r v ation of softbodied
fo s sils is deter1
T tined by a hie r archy of con trois
Although these c o n trols are not yet fully unclerstood,
they help to e x plain why e x ceptional prese r vation is
mats we r e n o longe r ubiquitou s , and the pr e ser ation of
soft tissues required othe r s pe c ial circumstancesThe
Burgess Shaletype Lagerstät t en of the CamtTfian ar
most abundant in de e per slope/hiìsin settings, 1
4 heri?
finegrained sedime n t accumulated in episodic dep°
tional eventsAt this time de e p bioturbators had vet tLl
invade deepe r wate r s e ttings in large number ; E
helf
subsequent radiatio n fro m o nshor e to offshore coJ1
tributed to the abs e n c e of Burges s shaletype Lagers.À
ten in younger rocks (Alliso n a nd Briggs 19931
pf3
pf4
pf5

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