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- W2004569243 abstract "ABSTRACT Late Paleozoic fusuline foraminifera are thought to have hosted photosymbionts, as do modern larger foraminifera, but the ancient host-symbiont relationship has never been demonstrated conclusively. Among modern larger foraminifera, deeper-dwelling species exhibit large surface-to-volume ratios in order to maximize the amount of sunlight that can be captured for use by photosymbionts. Shallower-dwelling species exhibit smaller surface-to-volume ratios in order to limit incoming sunlight, especially ultraviolet radiation. If modern symbiont-bearing foraminifera are appropriate analogues for fusulines, then deeper-dwelling fusulines ought to exhibit larger surface-to-volume ratios than shallower-dwelling ones. This prediction was tested by analyzing fusuline shells from the Virgilian (Upper Pennsylvanian) Oread, Lecompton and Deer Creek cyclothems in Kansas. Specimens from deeper-water “middle” limestones exhibit significantly larger surface-to-volume ratios than those from regressive “upper” limes..." @default.
- W2004569243 created "2016-06-24" @default.
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- W2004569243 date "2012-11-09" @default.
- W2004569243 modified "2023-09-27" @default.
- W2004569243 title "A TEST FOR THE POSSIBILITY OF PHOTOSYMBIOSIS IN EXTINCT FUSULINE FORAMINIFERA: SIZE AND SHAPE RELATED TO DEPTH OF HABITAT" @default.
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- W2004569243 doi "https://doi.org/10.2110/palo.2012.p12-057r" @default.
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