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Journal ArticleDOI

Larger foraminifera, giant cells with a historical background

Lukas Hottinger
- 01 Aug 1982 - 
- Vol. 69, Iss: 8, pp 361-371
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TLDR
The history of foraminifera as recorded by the shell of numerous taxa illustrates the repetitive rise of benthic, large-sized K-strategists throughout geologic time and points to the functional importance of shell shape during the long vegetative life.
Abstract
The history of foraminifera as recorded by the shell of numerous taxa illustrates the repetitive rise of benthic, large-sized K-strategists throughout geologic time. The phylogeny reconstructed by methods of comparative anatomy and supported by biostratigraphic distribution permits to identify analogous shell structures pointing to functions of the living cell. The shell registers autecological adaptation, ontogeny, protoplasmic streaming patterns, protoplasmic differentiation and patterns of differentiation at the cell surface. The high potential of shell regeneration points to the functional importance of shell shape during the long vegetative life and documents experiments performed by nature itself. The extended knowledge of their history, their size and their natural recording device in their shell predestines the foraminifera as experimental system to explore the performances of free-living single cells and many mechanisms regulating their life.

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Journal ArticleDOI

Ecology of extant nummulitids and other larger benthic foraminifera: applications in palaeoenvironmental analysis

TL;DR: A substantial body of literature has built up on the ecology of modern LBF, especially in terms of their environmentally sensitive depth distribution, reproductive strategy and morphology, and the symbiotic relationship between many larger foraminifera and photosynthetic algae as mentioned in this paper.
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Evolution and Geological Significance of Larger Benthic Foraminifera

TL;DR: In this paper, the Mesozoic larger benthic foraminifera assemblages in the understanding of the global distribution of carbonate sediments and their value in contributing raw data to palaeoenvironmental and palaeoclimatic models.
Journal ArticleDOI

Recognition of stratigraphic sequences in carbonate platform and slope deposits: empirical models based on microfacies analysis of Palaeogene deposits in southeastern Spain

TL;DR: In this paper, three different empirical models for platform accommodation cycles were designed: a ramp model, distinctive for the Lower Eocene, a combined ramp-rimmed model, characteristic for the Middle and Upper Eocene and a rimmed model representative for Oligocene cycles.
Journal ArticleDOI

Similarities between planktonic and larger foraminiferal evolutionary trends through Paleogene paleoceanographic changes

TL;DR: The evolution of planktonic foraminiferal faunas dominated by warm-water taxa, even though oxygen isotopes only recorded relatively minor cooling, can be reconciled by the explanation that the biotic communities responded to changes in trophic resources and euphotic habitats that accompanied the temperature reduction as discussed by the authors.
Journal ArticleDOI

Assessing the contribution of foraminiferan protists to global ocean carbonate production.

TL;DR: The importance of foraminifera within the CaCO3 budget of the world's oceans is highlighted, as they contribute almost 5% of the annual present‐day carbonate production in the world’s reef and shelf areas and approximately 2.5% in all oceans.
References
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Journal ArticleDOI

Ultrastructural and radiotracer studies of pore function in foraminifera

TL;DR: Clusters of mitochondria have been observed close to the inner end of the pores in Nonionella stella, Globobulimina pacifica, Buliminella tenuata, Bolvina argentea, Loxostomum pseudobeyrichi, Cassidulinoides cornuta and Bolivina cf.
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The role of foraminifera in the trophic structure of marine communities

TL;DR: Foraminifera are recorded as feeding chiefly upon bacteria, small diatoms, and nannoplankton in a wide variety of marine environments, and form part of a key link in marine food chains, assimilating energy available from minute autotrophs and also retrieving energy available during the final stages of degradation of organic debris.
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Differentiation of protoplasm in nummulitidae (Foraminifera) from Elat, Red Sea

TL;DR: The canal system in the shells of Operculina ammonoides and Heterostegina depressa d'Orbigny is interpreted as consisting of a system of invaginations of the cell wall determining the morphology of proximal parts of the pseudopods.
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