Graptolites
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Transcript of Graptolites
-151 Middle East Geology -Geol 501-142
Types of Graptolites in Cambrian-Ordovician and their Environmental Significance
By:
Abdullah [email protected]
KFUPMEarth Science Department
Mar. 8, 2015
-152 Middle East Geology -Geol 501-142
Outline• Introduction.• Linnaean system for Graptolites.• Graptolite morphology.• Selective Graptolites• Environmental Significance• Conclusion.
-153 Middle East Geology -Geol 501-142
Introduction• Fossils provide information on geological time, evolutionary history,
and ancient environments.
• Graptolites are an extinct group of marine, colonial animals that
built their skeletons from a variety of proteins.
• They varied in colony size from 2 mm to over 1 m in length, and
in form from simple sticks to complicated bushy shapes.
• Graptolites are considered as excellent index fossils because of
their reputation for being distributed worldwide.
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Objectives• To discuss the origin and types of Graptolites, from Cambrian to
Ordovician.• To discuss some of their environmental significance.
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Modern Biological classification
Labspaces, March 26, 2011
Incr
easi
ng n
umbe
r of c
omm
on tr
aits Linnaean taxonomy
(Carolus Linnaeus),
All organisms grouped into five Kingdoms (Boggs,1995)
~90 phyla
Millions
-156 Middle East Geology -Geol 501-142
Hierarchical linnaean system for GraptolitesHemichordata
(Phylum)Enteropneusta(Class)
Graptolithina(Class)Dendroidea(Order)
Graptoloidea(Order)
Tuboidea(Order)
Camaroidea(Order)
Stolonoidea(Order)
Crustoidea(Order)
Planctosphaeroi-dea(Class)
Pterobranchia(Class)
Graptolites (Extinct)
(Mu,1987; Wikipedia, 2015)
Animalia(Kingdome)
Deuterostomia(Superphylum)
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Graptolite Classification
•Frech 1897•Mu 1950, 1973•Mu & Zhan 1966•Bulman 1955•Obut 1955, 1964•Jannmusson 1960, 1965•Bulman 1963b, 1970•Yu & Fang 1979•Lapwroth 1879, 1880
-158 Middle East Geology -Geol 501-142
Graptolite hard-part morphology
Orientation of a Graptolite Stipe.(Milsom, 2013)
Dendroid. Graptoloid
Different thecal types of Graptolites
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Benthic and Planktic diversity
Bent
hic
Plan
ktic
(Milsom, 2013)
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Selective GraptolitesCo
llect
ed fr
om (M
ilsom
& R
igby
, 201
3;
Geo
-logi
c.or
g, M
ar. 2
015;
-1511 Middle East Geology -Geol 501-142
Selective GraptolitesCo
llect
ed fr
om (M
ilsom
& R
igby
, 201
3;
Nat
ural
His
tory
Mus
eum
, Mar
. 201
5; N
ew B
runs
wic
k M
useu
m, M
ar. 2
015)
More >> Graptolites| Earth Lab Database
-1512 Middle East Geology -Geol 501-142
Environmental Significance
• Graptolites are useful in biostratigraphy to date and correlate
Paleozoic rocks. For instance Hanadir and Ra’an members
• The paleogeographic, distribution of graptolites is useful for
biogeographic interpretations and plate tectonic reconstructions.
• The occurrence of graptolite-rich rocks is an important record of
shelf margin development and of oceanographic conditions in seas
above shelf margins.
• Graptolites provide a promising tool for recognizing maximum
flooding surfaces.
-1513 Middle East Geology -Geol 501-142
Conclusion• Graptolithina, a class of Hemichordata, comprises chiefly six orders
known as Dendroidea, Graptoloidea,Tuboidea,Camaroidea, Stolonoidea and Crustoidea.
• Graptolites stared to form in the Middle Cambrian, increased in the early Ordovician and became extinct in the mid-Devonian.
• Graptolites are considered as excellent index fossils because of their reputation for being distributed worldwide.
• Graptolites are useful in biostratigraphy to date and correlate Paleozoic rocks. Besides, they are useful for biogeographic interpretations, plate tectonic reconstructions, oceanographic conditions and recognizing maximum flooding surfaces.
• Graptolites were found in Hanadir and Ra’an members of Qasim formation in Saudi Arabian, and Sahmah, Hasirah, and Saih Nihayda formations in Oman.
-1515 Middle East Geology -Geol 501-142
References• Berry, W. B. (1962). Graptolite occurrence and ecology. Journal of Paleontology, 285-
293.• Egenhoff, S., & Maletz, J. (2007). Graptolites as indicators of maximum flooding
surfaces in monotonous deep-water shelf successions. Palaios, 22(4), 373-383.
• Finney, S. C., & Berry, W. B. (1997). New perspectives on graptolite distributions and their use as indicators of platform margin dynamics. Geology, 25(10), 919-
922.• Le Hérissé, A., Al-Ruwaili, M., Miller, M., & Vecoli, M. (2007). Environmental changes
reflected by palynomorphs in the early Middle Ordovician Hanadir Member of the Qasim Formation, Saudi Arabia. Revuede micropaléontologie, 50(1), 3-16.
• Maletz, J. (n.d.). Graptolites. University at Baffalo. Retrieved March 5, 2015, from http://www.glyfac.buffalo.edu/Faculty/jorgm/WebJorg07/malgraps.htm
• McKerrow, W. S., & Scotese, C. R. (Eds.). (1990). Palaeozoic palaeogeography and biogeography.
• Milsom, C., & Rigby, S. (2013). Fossils at a Glance. John Wiley & Sons.• Mu, A. T. (1987). Graptolite taxonomy and classification. Bulletin of the Geological
Society of Denmark, 35(3-4), 203-207.