Current and Cretaceous-Cenozoic diversification of Angiosperms

نویسندگان

  • Serge Sheremet'ev
  • Xenia Chebotareva
چکیده

Cretaceous-Cenozoic history of angiosperms led to the a certain character of the distribution of taxa of different levels (the number of species and genera in families, species/genera ratio in families, the number of species in the genera). In most cases, these distributions are satisfactorily described by a power law (Pareto distribution). In logarithmic coordinates power function is a straight line. Empirical curves repeat this line is good enough, but on the right side of the graph (at low volumes taxa), there is a marked deviation of theoretical from the empirical curves. This suggests that the small volumes of taxa should be greater for full compliance with the theoretical curves. Modeling ratios among genera and species in families showed that only in the case of dynamic extinction factor observed satisfactory agreement between observed and calculated the number of species in a wide range of iterations. This suggested that there was a differential extinction of species during the evolution of angiosperms. This implies that the rate of extinction had to be minimal in genera with a large number of species. On the contrary, extinction rates may be increased by orders of magnitude with a decrease in the number of species. As a result, large genera became getting bigger and small genera become less. The species frequencies of distribution in the genera varied according to a power law. The initial divergence of taxa volume, which led to their further division into large and small, could be caused by the emergence and expansion of herbs with their functional and adaptive capabilities.

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

Evidence for a Cenozoic radiation of ferns in an angiosperm-dominated canopy.

In today's angiosperm-dominated terrestrial ecosystems, leptosporangiate ferns are truly exceptional--accounting for 80% of the approximately 11,000 nonflowering vascular plant species. Recent studies have shown that this remarkable diversity is mostly the result of a major leptosporangiate radiation beginning in the Cretaceous, following the rise of angiosperms. This pattern is suggestive of a...

متن کامل

Sex and the shifting biodiversity dynamics of marine animals in deep time.

The fossil record of marine animals suggests that diversity-dependent processes exerted strong control on biodiversification: after the Ordovician Radiation, genus richness did not trend for hundreds of millions of years. However, diversity subsequently rose dramatically in the Cretaceous and Cenozoic (145 million years ago-present), indicating that limits on diversification can be overcome by ...

متن کامل

Mass extinction, gradual cooling, or rapid radiation? Reconstructing the spatiotemporal evolution of the ancient angiosperm genus Hedyosmum (Chloranthaceae) using empirical and simulated approaches.

Chloranthaceae is a small family of flowering plants (65 species) with an extensive fossil record extending back to the Early Cretaceous. Within Chloranthaceae, Hedyosmum is remarkable because of its disjunct distribution--1 species in the Paleotropics and 44 confined to the Neotropics--and a long "temporal gap" between its stem age (Early Cretaceous) and the beginning of the extant radiation (...

متن کامل

Ecological Aspects of the Cretaceous Flowering Plant Radiation1

The first flowering plant fossils occur as rare, undiverse pollen grains in the Early Cretaceous (Valanginian-Hauterivian). Angiosperms diversified slowly during the Barremian-Aptian but rapidly during the Albian-Cenomanian. By the end of the Cretaceous, at least half of the living angiosperm orders were present, and angiosperms were greater than 70% of terrestrial plant species globally. The r...

متن کامل

Cenozoic insect-plant diversification in the tropics.

E volution has done wonders with mass extinctions. Organic diversity has rebuilt itself at least five times during the history of life on Earth, fashioning novelty from the organic remnants of each catastrophe (1). Modern biodiversity arose from a global extinction event at the end of the Cretaceous period (the ‘‘K-T’’ extinction) that probably was caused by an asteroid or comet impact. This pe...

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:

دوره   شماره 

صفحات  -

تاریخ انتشار 2016