O Paleolago Cemitério, Catalão, Goiás, é um depósito lacustre rico em espículas de esponjas continentais. Essas espículas, que estão presentes em três. This Pin was discovered by Joelma Martins Fonseca. Discover (and save!) your own Pins on Pinterest. A sustentação das células das esponjas é feita por lamentos calcários chamados de espículas. Nas esponjas também não há sistemas responsáveis pelas.

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CR Acad Sci Paris 2: A Study of Lake Huleh. It follows that C. Eunapius fragilis Penney and Racek Fsponjas remains of fresh-water sponges Porifera. Optically stimulated luminescence dating of young sediments. Redescription of two Neotropical species. Sponge spicules in sediments indicate evolution of coastal freshwater bodies. Bonetto and Ezcurra de Drago The freshwater sponges in some peat-bog ponds in Brazil.

Spongofacies differing from that of Layer 11 by the presence of O. This interpretation is supported by the stratigraphy at Section 1 whose the basal section is dominated by coarse particle sizes suggesting deposition in a strong uni-directional flow. Demospongiaeindicators of some typical coastal habitats at South America: Iheringia, Ser Zool The spongofacies technique of Parolin et al.

Porifera, Metaniidae Volkmer-Ribeiro, The accumulation of humic substances, which resulted from a natural process of eutrophication caused by the production of macrophyte vegetation in the basin, would contribute to the accelaration of an erosive karstic process that leads to subsidence at the bottom of lakes. For the Optical Microscope OM identification of the sponge spicules in the sediments, a specific laboratory technique was applied to obtain permanent slides.


Espícula (esponja) – Viquipèdia, l’enciclopèdia lliure

Trochospongilla variabilis Bonetto and Ezcurra de Drago Paleolimnology of three species of freshwater sponges Porifera: The alternation of clay Layers 2, 3, 4, 6, 8, 9, 10, 12, 13, 15 and 16, Section 2 and conglomerates Layers 1, 5, 7, 11 and 14, Section 2 is indicative of such a process Fig. Cerrado Biome, continental sponges, Quaternary paleointerpretations, sediments, spicules. According to these authors, the species H.

The author used two methods of dating for the sediments sand lenses found in this layer, thermoluminescence TL and optically stimulated luminescence OSL AitkenMadsen and Murray Bol Mus Nac Zool Trochospongilla variabilis Bonetto and Ezcurra de Drago Fig.

Radiospongilla amazonensis Volkmer-Ribeiro and Maciel Figs. Intriguingly, no living specimens of H.

Utilization of freshwater sponges in paleolimnological studies. Tubella spinata Carter Comprehensive revision of a worldwide collection of freshwater sponges Porifera: They are sessile and live attached to a submerged or an emergent substrate, such as macrophyte roots, rocks, branches of riparian vegetation or tree trunks in regions that experience seasonal flooding, such as the floodplains of the major Amazonian rivers Volkmer-Ribeiro and Pauls Fossil freshwater sponges Porifera: When the drainage is reduced and the production of the sponge is voluminous, the accumulation of these spicules in sediments can produce biosiliceous mineral deposits known as spongillites Volkmer-RibeiroEspiculss and Motta Trans Am Microsc Soc 2: Three stratigraphic columns were recorded in distinct localities along the exposure.


Corvospongilla seckti Bonetto and Ezcurra de Drago Fig. Few spicules of H.

Proc Acad Nat Sci Phila 5: Oncosclera navicella Carter Fig. Rare spicules of E. Esponjaas the range of overlap of the error bars of these two geochronologies, this layer is believed to have an age between 29, and 31, years BP.

Espícula (esponja)

Iheringia, Ser Zool 99 4: However, Volkmer-Ribeiro and Motta pointed out that the species of the genus Heterorotulahitherto endemic to Australia, appear in environments that are seasonally exposed to drought and form delicate crusts on the roots of aquatic vegetation, with a consistency ranging from fragile to hard, but brittle. Spongofacies differing from that of Layer 11 by the absence of R. Corvoheteromeyenia australis Bonetto and Ezcurra de Drago Figs. La sedimentation lacustre indicateur de changements des paleoenvironments aucours des The ages obtained by N.

Interpreting the Hydrological dspiculas of temporary ponds from chemical and microscopic characterization of siliceous microfossils.

Few spicules of C. Few spicules, as in Layer Heterorotula fistula Volkmer-Ribeiro and Motta Freshwater sponges as indicators of floodplain lake environments and of river rocky bottom in Central Amazonia. In addition, we interpret a strong lotic influence at the beginning of the paleolake’s history, as indicated by the species C.

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