Index fossils are sometimes used by Geologists to determine stratigraphic data about Earth's surface. This is true in the case of spores and pollen grains, the reproductive materials found in plants. By doing so provides the palyntologist means to determine relative age and position of rock, containing the spores. When studying drill cores, this kind of information can be useful to miners searching for fossil fuels.
Palynologists have used index fossils for practical applications, including understanding relationship between major groups of plants, specifically, gymnosperms and angiosperms.
A good index fossil is considered to be one that is easily identifiable, with wide horizontal distribution, and vertical range of approximately one million years. Traditionally, due to scarcity and difficulty in identification, plant megafossils were rarely used as index fossils. Though possessing wide geographical distribution in various sedimentary rocks, the vertical range spans millions of years. Assemblages of megafossils used as indices (or, indexes), accompanied by palynological information, scientists have been able to characterize restrictive stratigraphic units in rock units containing megafossils.
EON |
ERA |
PERIOD |
EPOCH |
Characteristic organisms and major geological events |
Duration in millions of years |
Began (m.y.a.) |

|
CENOZOIC ERA |
QUARTERNARY PERIOD

|
HOLOCENE EPOCH |
|
Last 5,000 years |
0-10,000 years ago |
PLEISTO- CENE EPOCH |
|
2.5 million years |
10,000 to 1.6 million years ago |
TERTIARY PERIOD
 Late Tertiary

Middle Tertiary

Early Tertiary

KT Times
|
PLIOCENE EPOCH |
|
4.5 million years |
2.5-7 million years ago |
MIOCENE EPOCH |
|
19 million years |
7-26 million years ago |
OLIGOCENE EPOCH |
|
12 million years |
26-38 million years ago |
EOCENE EPOCH |
|
16 million years duration |
38-54 million years ago |
PALEOCENE EPOCH |
|
11 million years duration |
54-65 million years ago |
MESOZOIC ERA |
CRETACEOUS PERIOD

Later Cretaceous
Early Cretaceous
|
UPPER
Maastrichtian
Campanian
Santonian
Coniacian
Turonian
Cenomanian |
|
76 million years duration |
65-141 million years ago |
LOWER
Albian
Aptian
Barremian
Hauterivian
Valanginian
Berriasian |
JURASSIC PERIOD

|
UPPER
Tithonian
Kimmeridgian
Oxfordian |
|
54 million years duration |
141-195 million years ago |
MIDDLE
Callovian
Bathonian
Bajocian
Aalenian |
LOWER
Toarcian
Pliensbachian
Sinemurian
Hettangian |
TRIASSIC PERIOD

|
UPPER
Rhaetian
Norian
Carnian |
|
30 million years duration |
208-245 million years ago |
MIDDLE
Ladinian
Anisian |
LOWER (Scythian)
Olenekian
Induan |
PALEOZOIC ERA |
PERMIAN PERIOD

|
UPPER
Lopingian
- Changhsingian
- Wuchiapingian
MIDDLE
Guadalupian
- Capitanian
- Wordian
- Roadian |
|
55 million years duration |
245-280 million years ago |
LOWER
Cisuralian
- Kungurian
- Artinskian
- Sakmarian
- Asselian |
C A R B O N I F E R O U S |
PENNSYLVANIAN |
UPPER
Kasimovian | Gzhelian |
|
45 million years duration |
280-325 million years ago |
MIDDLE
Moscovian |
LOWER
Bashkirian |
MISSISSIPPIAN
 Carboniferous
|
UPPER
Serpukhovian
MIDDLE
Viséan |
|
20 million years duration |
286-360 million years ago |
LOWER
Tournaisian |
DEVONIAN PERIOD

|
UPPER
Fammenian | Fransnian |
|
50 million years duration |
360-408 million years ago |
MIDDLE
Givetian | Eifelian |
LOWER
Praghian | Lockhovian |
SILURIAN PERIOD

|
UPPER
Pridolian | Ludlovian |
|
40 million years duration |
408-438 million years ago |
LOWER
Wenlockian | Llandoverian |
ORDOVICIAN PERIOD

|
UPPER
Ashgillian | Caradocian
MIDDLE
Llandeilian | Llanvirnian |
|
65 million years duration |
438-505 million years ago |
LOWER
Arenigian | Tremadocian |
CAMBRIAN PERIOD

Late Cambrian

Early Cambrian
|
UPPER
Furongian |
|
70 million years duration |
505-540 million years ago |
MIDDLE
* table below |
LOWER
* table below |

|
PROTERO- ZOIC ERA |
VENDIAN PERIOD

|
|
-- |
540-650 million years ago |
PRE-VENDIAN PERIOD |
|
650-2,500 million years ago |
ARCHAEAN
3.8 to 2.5 billion years ago
The atmosphere of Earth was very different from what we breathe today; at that time, it was likely a reducing atmosphere of methane, ammonia, and other toxic gases. During this time, the Earth's crust cooled enough that rocks and continental plates began to form. Early in the Archaean that life first appeared on Earth. Our oldest fossils date to roughly 3.5 billion years ago, and consist of bacteria microfossils. All life during the more than one billion years of the Archaean was bacterial, stromatolites, colonies of photosynthetic bacteria which have been found as fossils in Early Archaean rocks of South Africa and Western Australia. Stromatolites increased in abundance throughout the Archaean, but began to decline during the Proterozoic. |
2,500-3800 million years ago |
HADEAN
4.5 to 3.8 billion years ago
Hadean time is not a geological period as such. During Hadean time, the Solar System was forming. Sometime during the first 800 million or so years of its history, the surface of the Earth changed from liquid to solid. Once solid rock formed on the Earth, its geological history began. This most likely happened prior to 3.8 billion years, but hard evidence for this is lacking. Erosion and plate tectonics has probably destroyed all of the solid rocks that were older than 3.8 billion years. |
3,800-4,600 million years ago |
CAMBRIAN SUBDIVISIONS
Cambrian is divided into three epochs — the Early Cambrian (Lower Cambrian, Caerfai or Waucoban), Middle Cambrian (St Davids or Albertian) and Furongian (a.k.a. Late/Upper Cambrian, Merioneth or Croixan). Each of the epochs are divided into two faunal stages. Only one, Paibian has been recognized by the International Commission on Stratigraphy. Others are still unnamed. However, the Cambrian is divided into several regional faunal stages.
Source: Answers.com - Cambrian Subdivisions
| |
Chinese |
North American |
Russian-Kazakhian |
Australian |
Regional |
| Furongian |
|
Ibexian |
Ayusokkanian |
Idamean |
Dolgellian |
| |
Sunwaptan |
Sakian |
Mindyallan |
Festiniogian |
| |
Steptoan |
Aksayan |
Payntonian |
Maentwrogian |
| |
Marjuman |
Batyrbayan |
|
|
| Middle Cambrian |
Maozhangian |
Mayan |
Boomerangian |
|
| Zuzhuangian |
Delamaran |
Amgan |
Undillian |
|
| Zhungxian |
|
|
Florian |
|
| |
|
|
Templetonian |
|
| |
Dyeran |
|
Ordian |
|
| Early Cambrian |
Longwangmioan |
Toyonian |
Lenian |
| Changlangpuan |
Montezuman |
Botomian |
|
|
| Qungzusian |
|
Atdabanian |
|
|
| Meishuchuan |
|
Tommotian |
|
|
| |
|
Nemakit-Daldynian |
|
|
Extant organisms in their structure and distribution, reflect the composition of their environments. We assume extinct organisms also adapted to their environment in the same way. If this assumption is true, then it is possible to determine seasonal variations using growth rings from petrified wood, including paleo-environmental availability of water and temperature changes. Fossilized wood which reflects lack of growth rings, indicate a continuous supply of water and uniform temperature, just as thickened cuticles and sunken stomata of fossilized leaves indicate a lack of water, while roots and spongy stem tissue suggest a swampy or aquatic paleo-environment. With such information extracted from morphology and anatomy of fossil plants, provides in part, the basis for paleoecology and paleoclimatology. Further studies are taken into consideration, such as those on sedimentary materials which naturally occur with the fossils and, how the fossil became preserved, all play into better understanding the paleoenvironment. Specialists caution however, conclusions should never be based entirely upon extant organisms and how they interact with present environments. What we observe occuring today, is not necessarily the key to the past. (Paleobotany and the Evolution of Plants, Stewart and Rothwell, 1993; DiMichele & Wing, 1987.)
Paleofloristics, which specializes in assemblages of fossil plants, provides insight into Earth's restricted and widescale climate. On the worldwide scale, such studies have provided scientists with insight into plate tectonics and continental drift. These studies can also provide further insight into plant distribution, population, migration and significant changes in early environments. Studies on succession of plants in the geological column have became popular among paleoecologists, and also useful in studies on extant organisms and plant successions in natural history.
Successional changes in organisms throughout natural history are the basis of studies related to the evolution of life. Most paleontologists focus more on relative stratigraphic positioning of fossils, than absolute ages. It remains more important to most in the field, to determine how a fossil relates to other specimen with objective to un-ravel evolutionary patterns and origins.
REFERENCES
Bringing Fossils to Life, An Introduction to Paleobiology, McGraw Hill Publishers, Donald R. Prothero
Paleobotany and the Evolution of Plants, by Cambridge University Press; 2 edition, Wilson N. Stewart, Gar W. Rothwell
Atlas of the Prehistoric World, by Discovery Channel Books, Douglas Palmer
Kingfisher Illustrated Dinosaur Encyclopedia, Kingfisher Publishers, David Burnie
FURTHER SUGGESTED READING
Adrienne Mayor's books
1) The First Fossil Hunters (Princeton 2000) explains how ancient Greek and Roman discoveries of mysterious petrifed bones of extinct dinosaurs and mastodons led to myths about griffins, giants, and monsters. Watch for "Ancient Monster Hunters" on the History Channel.
2) Fossil Legends of the First Americans (Princeton 2005) gathers exciting Native American discoveries and myths about fossils, from tiny shells to enormous dinosaur bones, with stories from more than 45 different tribes, beginning with the Aztecs & Incas.
Stephen Meyer's article, "Are Dinosaurs Mentioned in the Bible?"
Comments Fossils, Extinction, Geology and Genesis
Article last updated August 17, 2006
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