Cryptic coral-crinoid "hanging gardens" from the Middle Devonian of southern Morocco
Authors:
Jakubowicz et al
Abstract:
An unusual and exceptionally well preserved cryptic community of cnidarians, crinoids, sponges, and microbes developed in a submarine cavity of Middle Devonian age in the Hamar Laghdad area (Morocco). The biota encrusted the cavity roof and grew predominantly in an upside-down position, forming spectacular "hanging gardens." The investigated assemblage differs strikingly from both its Paleozoic and modern analogues; it constitutes one of a very few known examples of fossil cryptic assemblages developed in relatively deep water settings, and is the first report of a cryptic paleoecosystem dominated by rugose corals. The results support the view that during the middle Paleozoic there was no distinct polarization between open-surface and cryptic faunas in deep-water environments, but keen competition for space already existed in Devonian cryptic assemblages. The regional species pool seems to have been the main determinant of the ecological succession and structure of this cryptic community.
Showing posts with label crinoids. Show all posts
Showing posts with label crinoids. Show all posts
Saturday, December 28, 2013
A Cryptic Coral-crinoid "Hanging Garden" From Eifelian/Givetian Devonian Morocco
Labels:
cnidaria,
corals,
crinoids,
devonian,
eifelian,
fossils,
Givetian,
invertebrates,
morocco,
paleontology,
paleozoic,
sponges
Tuesday, February 19, 2013
Oldest Biomarkers Recovered to Date from Carboniferous Crinoids
Though scientists have long believed that complex organic molecules couldn't survive fossilization, some 350-million-year-old remains of aquatic sea creatures uncovered in Ohio, Indiana, and Iowa have challenged that assumption.
The spindly animals with feathery arms—called crinoids, but better known today by the plant-like name "sea lily"—appear to have been buried alive in storms during the Carboniferous Period, when North America was covered with vast inland seas. Buried quickly and isolated from the water above by layers of fine-grained sediment, their porous skeletons gradually filled with minerals, but some of the pores containing organic molecules were sealed intact.
That's the conclusion of Ohio State University geologists, who extracted the molecules directly from individual crinoid fossils in the laboratory, and determined that different species of crinoid contained different molecules. The results will appear in the March issue of the journal Geology.
William Ausich, professor in the School of Earth Sciences at Ohio State and co-author of the paper, explained why the organic molecules are special.
"There are lots of fragmented biological molecules—we call them biomarkers—scattered in the rock everywhere. They're the remains of ancient plant and animal life, all broken up and mixed together," he said. "But this is the oldest example where anyone has found biomarkers inside a particular complete fossil. We can say with confidence that these organic molecules came from the individual animals whose remains we tested."
The molecules appear to be aromatic compounds called quinones, which are found in modern crinoids and other animals. Quinones sometimes function as pigments or as toxins to discourage predators.
Sorry, no Carboniferous Sea World.
Labels:
biomarkers,
carboniferous,
crinoids,
fossils,
invertebrates,
oceans,
paleontology,
Tournaisian
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