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Globigerinoides

Globigerinoides is an extant genus of shallow-water planktonic foraminifera of family Globigerinidae. First appearing in the Oligocene, these foraminifera are found in all modern oceans. Species of this genus occupy the euphotic zone, generally at depths between 10 and 50 m, in waters which cover a range of salinities and temperatures. They are a shorter lived species, especially when compared to Globorotalia genus. As a genus, Globigerinoides is widely used in various fields of research including biostratigraphy, isotope geochemistry, biogeochemistry, climatology, and oceanography.

Morphology
The foraminifera of genus Globigerinoides are all shallow-water species with spinose forms made of hyaline calcite. As with other amoeboids these foraminifera utilize pseudopodia. Pseudopodia are widely used throughout their entire lifecycle for various purposes including feeding, movement, protection, and chamber formation. ==Symbionts==
Symbionts
Many Globigerinoides species bear photosynthetic symbiotic algae. The relationship between the symbiotic algae and its host foraminifera provides the host with at least three main advantages, including energy from photosynthesis, an enhancement of calcification, and uptake of host metabolites. All in all it is a prime example of ectosymbiosis. ==Notable species==
Notable species
Certain species of Globigerinoides are more commonly used in various types of research than others. Commonly used species include G. ruber,G. sacculifer, G. subquadratus, and G. altiaperturus. Globigerinoides sacculifer Globigerinoides sacculifer exhibits two different morphologies, known as G. sacculifer with sac and G. sacculifer without sac. The sac feature is a sac shaped terminal chamber that is formed prior to the production of the gametogenic calcite. When using G. sacculifer tests for bulk isotope analysis tests without the sac morphology are often preferentially selected. Globigerinoides ruber Globigerinoides ruber are carnivorous and prey upon copepods and nauplii. Once a copepod or nauplii is caught in its spines G. ruber uses its pseudopodia to draw the caught prey close to its test to allow it to feed.G. ruber has been found to tolerate hyposaline waters, in laboratory cultures it was able to remain alive in salinity ranges of 22-49%. Globigerinoides subquadratus Among other microfossil evidence, the last common occurrence of G. subquadratus is defined as the beginning of the Tortonian stage of the geologic time scale. The boundary is defined at the Monte dei Corvi Beach section in Italy. Globigerinoides altiaperturus The first appearance datum of G. altiaperturus is the proposed base of the Burdigalian stage of the geologic time scale. The boundary has not yet been defined with a GSSP by the International Commission on Stratigraphy. == References ==
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