Skeletal calcite in living scleractinian corals: microboring fillings, not primary skeletal deposits.

نویسندگان

  • I G Macintyre
  • K M Towe
چکیده

1. For reviews, see S. Appelle, Psychol. Bull. 78, 266 (1971); M. M. Taylor, J. Opt. Soc. Am. 53,763 (1963). 2. Although the fact of orientation anisotropy is well established, its incidence has not been documented, as far as we are aware. Two earlier studies of anisotropy [H. Leibowitz, N. A. Myers, D. A. Grant, J. Opt. Soc. Am. 45, 76 (1955); J. C. Ogilvie and M. M. Taylor, ibid. 49, 898 (1955)] used a total of 11 subjects. Of these subjects, one showed no difference in performance for different orientations and two performed better for obliques. 3. M. H. Segall, D. T. Campbell, M. J. Herskovits, The Influence of Culture on Visual Perception (Bobbs-Merrill, Indianapolis, Indiana, 1966). 4. R. C. Annis and B. Frost, Science 182, 729 (1973). 5. Titmus Optical Company, Petersburg, Virginia. 6. Subjects with prescribed corrective lenses were required to wear them during testing. If any subjects scored below normal values on the T-O vision tester or exhibited large differences in acuity for orthogonal gratings in the experimental situation, we attempted to improve their performance to normal with lenses. Those with obvious amblyopias were dropped from the sample. Since we did not refract our subjects to ensure a perfect optical correction, we were concerned that some cases of uncorrected astigmatism might have influenced our results. However, when we computed an astigmatism ratio by dividing the acuity for one axis by that for the orthogonal axis, the distribution for both Chinese and Caucasian samples approximated that reported for normal subjects by D. E. Mitchell et al. (11). Thus, we conclude that the differences between Chinese and Caucasian scores reported here were not produced by systematic differences in astigmatism. 7. Contrast is defined as Lmax -Lmn

برای دانلود رایگان متن کامل این مقاله و بیش از 32 میلیون مقاله دیگر ابتدا ثبت نام کنید

ثبت نام

اگر عضو سایت هستید لطفا وارد حساب کاربری خود شوید

منابع مشابه

Biotic Control of Skeletal Growth by Scleractinian Corals in Aragonite–Calcite Seas

Modern scleractinian coral skeletons are commonly composed of aragonite, the orthorhombic form of CaCO3. Under certain conditions, modern corals produce calcite as a secondary precipitate to fill pore space. However, coral construction of primary skeletons from calcite has yet to be demonstrated. We report a calcitic primary skeleton produced by the modern scleractinian coral Acropora tenuis. W...

متن کامل

A unique skeletal microstructure of the deep-sea micrabaciid scleractinian corals.

Micrabaciids are solitary, exclusively azooxanthellate deep-sea corals belonging to one of the deepest-living (up to 5,000 m) scleractinian representatives. All modern micrabaciid taxa (genera: Letepsammia, Rhombopsammia, Stephanophyllia, Leptopenus) have a porous and often very fragile skeleton consisting of two main microstructural components known also from other scleractinians: rapid accret...

متن کامل

Skeletal mineralogy of coral recruits under high temperature and pCO2

Aragonite, which is the polymorph of CaCO3 precipitated by modern corals during skeletal formation, has a higher solubility than the more stable polymorph calcite. This higher solubility may leave animals that produce aragonitic skeletons more vulnerable to anthropogenic ocean acidification. It is therefore important to determine whether scleractinian corals have the plasticity to adapt and pro...

متن کامل

Aragonitic scleractinian corals in the Cretaceous calcitic sea

Changes in seawater chemistry have affected the evolution of calcifying marine organisms, including their skeletal polymorph (calcite versus aragonite), which is believed to have been strongly influenced by the Mg/Ca ratio at the time these animals first emerged. However, we show that micrabaciids, a scleractinian coral clade that first appeared in the fossil record of the Cretaceous, when the ...

متن کامل

Morphology, microstructure, crystallography, and chemistry of distinct CaCO3 deposits formed by early recruits of the scleractinian coral Pocillopora damicornis.

Scleractinian corals begin their biomineralization process shortly after larval settlement with the formation of calcium carbonate (CaCO(3)) structures at the interface between the larval tissues and the substrate. The newly settled larvae exert variable degrees of control over this skeleton formation, providing an opportunity to study a range of biocarbonate structures, some of which are trans...

متن کامل

ذخیره در منابع من


  با ذخیره ی این منبع در منابع من، دسترسی به آن را برای استفاده های بعدی آسان تر کنید

عنوان ژورنال:
  • Science

دوره 193 4254  شماره 

صفحات  -

تاریخ انتشار 1976