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SOUVENIR COMMITTEE - Birbal Sahni Institute of Palaeobotany

SOUVENIR COMMITTEE - Birbal Sahni Institute of Palaeobotany

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Training Programme on “PALYNOLOGY IN FOSSIL FUEL EXPLORATION”<br />

[ September 10-17, 2012 ]<br />

HISTORY OF PALEONTOLOGY, ADVANCES IN MICROFOSSIL<br />

STUDIES,BIOCHRONOSTRATIGRAPHY, RESOLUTION ACHIEVED APPLICATION IN<br />

HYDROCARBON EXPLORATION<br />

DSN RAJU<br />

MSR Residency, 2 nd Floor, Pragati Marg, J.N.Road, Rajahmundry-533103, A.P., India<br />

E-mail: rajudsn1@gmail.com<br />

Paleontology is one <strong>of</strong> the historical sciences along with archaeology, geology, biology, astronomy,<br />

cosmology and history itself. Before 17 th, Paleontology focuses on the macroscopic animal fossils preserved<br />

on the rocks based on the available information. The information <strong>of</strong> small fishes and marine shells on inland<br />

mountains were given by Xenophanes, Pythagora and Xanthus and large benthic foraminifera Nummulites<br />

(Herodotus). The Paleontology was used to understand the nature <strong>of</strong> mountains, climate, sea-level change,<br />

paleogeography: The 17 th century: the first diagram illustrating the disposition <strong>of</strong> strata, and its unconformity<br />

<strong>of</strong> later beds on earlier inclined strata (Steno,1638-1687), The outstanding geological figure <strong>of</strong> the 17 th century<br />

was undoubtedly carried out for advent <strong>of</strong> cryptic fauna (Micrograptia, 1665), foraminifera (Rotalia); sutures<br />

<strong>of</strong> ammonites (Hook 1965) under compound microscopes which named as micropaleontology and possible<br />

used in as a chronological index (extinction <strong>of</strong> species). After a centaury, a new branch named Palynology<br />

for the pollen and spores was introduced by Hyde and Williams in 1944.<br />

They are monumental in integration <strong>of</strong> micr<strong>of</strong>ossil data with other branches <strong>of</strong> geology in<br />

interpretation <strong>of</strong> plate tectonics and paleogeography.<br />

The birth <strong>of</strong> economic or commercial micropaleontology can be attributed to the advent <strong>of</strong> oil industry.<br />

This signalled the present “Application phase <strong>of</strong> micropaleontology in Hydrocarbon exploration and<br />

production.’<br />

The advent <strong>of</strong> sequence stratigraphy in 1977 demanded a major role by micropaleontologists.<br />

Advances in the study <strong>of</strong> micr<strong>of</strong>ossils: The morphological nature <strong>of</strong> forms to molecular (ribosomal DNA<br />

sequences) micro-paleontology suggested by various workers (Srinivasan, 2007, Hayward et al 2003).<br />

Hydrocarbon reservoirs were first predicted based on the recovery <strong>of</strong> micr<strong>of</strong>ossils from well to well (<br />

Gryzbowski, 1980). A detailed account on advances in the application <strong>of</strong> biostratigraphy to Petroleum<br />

Exploration and Production (Giwa et.al. 2006). The sub branches include: 1. Biostratigraphy, 2.<br />

Biostratigraphic events concept, 3. High resolution biostratigraphy, 4. Wellsite biostratigraphic support,<br />

5. Biosteering, 6. Ecostratigraphic techniques, 7. Quantitative stratigraphy and 8. Biostratigraphic workstation.<br />

Studies on stable isotopes and trace elements in foraminifera as proxy <strong>of</strong> paleoclimate, paleobiology and<br />

paleooceanography are under progress in India.<br />

Resolution achieved in biochronostratigraphy through various tools/methods:<br />

Micr<strong>of</strong>ossils palyed/ playing a major role in Dating <strong>of</strong> sediments, seismic origins and well log breaks,<br />

Well to well, inter basinal and intercontinental correlations,Determination <strong>of</strong> paleoenvironments/<br />

paleobathymetries, recognition and estimation <strong>of</strong> duration <strong>of</strong> hiatuses including submarine, eEstablishing<br />

biochronostratigraphic frame work,3 rd , 4 th , 5 th /6 th order stratigraphic cycles and relative sea level fluctuations<br />

and an independent scheme <strong>of</strong> foraminiferal sequence stratigraphy and to some extent din<strong>of</strong>lagellates cysts<br />

sequence stratigraphy.<br />

Geosteering is related to process <strong>of</strong> drilling a borehole; adjusting the borehole position( inclination<br />

and azimuth angles) on the fly to reach one or more geological targets.<br />

Biosteering is combined data <strong>of</strong> paleontological related to the entombed micr<strong>of</strong>ossils in rocks in<br />

horizontal wells and LWD (log whilst drilling) for steering decisions. Because <strong>of</strong> fossils allow determination <strong>of</strong><br />

<strong>Birbal</strong> <strong>Sahni</strong> <strong>Institute</strong> <strong>of</strong> <strong>Palaeobotany</strong>, Lucknow<br />

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