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	<title>Planktonic Foraminifera - Revision history</title>
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	<updated>2026-04-22T21:05:34Z</updated>
	<subtitle>Revision history for this page on the wiki</subtitle>
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		<title>0:0:0:0:0:0:0:1: Content Updated.</title>
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		<summary type="html">&lt;p&gt;Content Updated.&lt;/p&gt;
&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;&amp;#039;&amp;#039;&amp;#039;Planktonic Foraminifera&amp;#039;&amp;#039;&amp;#039;  floating forms of the order Foraminifera, class Sercodina, phylum Protozoa; the single celled most primitive animal. They are most numerous in the surface and near surface parts of the open warm ocean water and mostly live about to a depth less than 2,000m. They lack locomotary organs and are distributed by ocean currents. In some cases they are carried thousands of kms in the [[Ocean|ocean]] and commonly die far away from their birth places. There are only a few species of planktonic foraminifera but they are represented in the ocean in numerous quantities. The tests of Globigerina makes up a large part of the [[Sediment|sediment]]s, covering about 35% of the ocean bottom and making up 80% of the fauna in the bottom sediments at many localities. Their presence has been even reported from great depths ranging from 3,000 m to 5,000 m. The common five genera of the Planktonic foraminifera belong to the families of Globorotaliidae. They are Globigerina, Globigerinoides, Globigerinella, Orbulina and Globorotalia.&lt;br /&gt;
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Planktonic foraminifera are considered good guide fossils for the correlation of regional and inter-regional sedimentary strata due to their vast distribution, short stratigraphic ranges with simple identifying characters. A number of authors have proposed various biozones based on the planktonic foraminifera from Cretaceous to Holocene.&lt;br /&gt;
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Planktonic foraminifera may lead to an erroneous interpretation as their tests are carried by ocean currents to a long distance to almost all depositional environments of the open ocean though their distribution is mainly restricted to the tropical and subtropical environments.&lt;br /&gt;
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In Bangladesh planktonic foraminifera (particularly nummulite) are noted in the Eocene Limestone Formation encountered in the subcrops of the north-western Bogra Shelf region and in the outcrops of the Sunamganj and Sylhet districts. Nummulitic Sylhet Limestone Formation is not traced in the south and south-eastern geosynclinal portion of the country. Planktonic foraminifera may be isolated from the [[Bhuban Formation|bhuban formation]] of Bangladesh if detail work is carried out. In Bangladesh two studies have recently been conducted on the planktonic foraminifera from two gravity cores of the northeast [[Bay of Bengal|bay of bengal]] and planktonic foraminifera from core samples of the continental slope of the Bay of Bengal. [Mujibur Rahman Khan]&lt;br /&gt;
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[[Category:Natural Sciences]]&lt;br /&gt;
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[[bn:প্লাঙ্কটনিক ফোরামিনিফেরা]]&lt;/div&gt;</summary>
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