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New parasite in a coprolite of 240 million years, biogeography of fossil coelacanths, and the influence of air pollutants in a coastal area of northeastern Brazil

The present issue of the Annals of the Brazilian Academy of Sciences (AABC) publishes several papers on paleontology. Among them is the study of Priscilla da Silva (Fundação Oswaldo Cruz) and colleagues who have made quite an interesting discovery: a new parasite in a coprolite of 240 million years (Da Silva et al. 2014). Coprolites or fossilized feces are not particularly rare, being constantly recovered during paleontological excavations, for all in areas that represent ancient shallow seas, lagoons or lakes (e.g., Vila Nova et al. 2011), where often they can be the most common fossil found. Occasionally they are also found in terrestrial environments (Souto 2000Souto PRF. 2000. Tetrapod coprolites from the middle Triassic of southern Brazil. Gaia, Geosci J 16: 51-57.). Nevertheless they are not very commonly reported upon, possibly due to the fact that it is very hard to be sure which kind of animal produced them. Notwithstanding, it is quite an important material to be studied since they provide some important information regarding an animal's diet.

In the case of the specimen studied by Da-Silva and colleagues, they could attribute a coprolite to a primitive herbivorous cynodont, even though they were not able to precise which species. The material was recovered from layers of the Triassic Santa Maria Formation in Rio Grande do Sul at a site called Cortado. Being perhaps one of the few cases of a primitive cynodont coprolite, the most important aspect of this discovery was the identification of parasite eggs that the authors have attributed to a new ascarid species. It would be interesting to proceed with this kind of study in other coprolites of the Santa Maria Formation that might reveal more of such parasite, and try to establish if it was endemic to this region of southern Brazil during this geologic period.

Another interesting contribution published in the present issue of the AABC is on the distributional pattern of an extinct group of coelacanths. This group of lobe-finned fishes is presently represented by only two species found in the coastline of the Indian Ocean and Indonesia (Holder et al. 1999Holder MT, Erdmann MV, Wilcox TP, Caldwell RL and Hillis DM. 1999. Two Living Species of Coelacanths?”. Proceedings of the National Academy of Sciences of the United States of America 96(22): 12616-12620.), but in deep time they showed quite some diversity (Johanson et al. 2006Johanson Z, Long JA, Talent JA, Janvier P and Warren JW. 2006. Oldest coelacanth, from the Early Devonian of Australia. Biol Lett 2: 443-446., Miguel et al. 2014Miguel R, Gallo V and Morrone JJ. 2014. Distributional patterns of †Mawsoniidae (Sarcopterygii: Actinistia). An Acad Bras Cienc 86: 159-170.). Raphael Miguel (Universidade do Estado do Rio de Janeiro) and colleagues have reviewed the distribution of the extinct coelacanth group called Mawsoniidae. Although known since the Triassic, those fishes are particularly common in Cretaceous deposits (Miguel et al. 2014Miguel R, Gallo V and Morrone JJ. 2014. Distributional patterns of †Mawsoniidae (Sarcopterygii: Actinistia). An Acad Bras Cienc 86: 159-170.). Biogeographic studies are quite interesting since they can help explain why the organisms are where they are (e.g.,Gallo et al. 2013Gallo V, Avilla LS, Pereira RCL and Absolon BA. 2013. Distributional patterns of herbivore megamammals during the Late Pleistocene of South America. An Acad Bras Cienc 85: 533-546.). In this particular contribution, Miguel and colleagues have found evidences that the break up of the continents which started in the Triassic might have played a major rule in the distributions of those fishes.

Lastly, I would like to call attention to the paper by Stelyus Mkoma (Instituto Nacional de Ciência e Tecnologia de Energia e Ambiente/INCT-E&A, Salvador) and colleagues, on the effect of air pollutants on the atmosphere of coastal areas close to large urban centers. Recently the AABC published some quite interesting papers on different kinds of pollution that occur in distinct areas (e.g., Lacerda et al. 2012Lacerda LD, Bastos WR and Almeida MD. 2012. The impacts of land use changes in the mercury flux in the Madeira River, Western Amazon. An Acad Bras Cienc 84: 69-78., Silva et al. 2012Silva DML, Camargo PB, Mcdowell WH, Vieira I, Salomão MSMB and Martinelli LA. 2012. Influence of land use changes on water chemistry in streams in the State of São Paulo, southeast Brasil. An Acad Bras Cienc 84: 919-930., Fonseca et al. 2013, Hermes et al. 2013Hermes N, Schneider RCS, Molin DD, Riegel GZ, Costa AB, Corbellini VA, Torres JPM and Malm O. 2013. Environmental pathways and human exposure to manganese in southern Brazil. An Acad Bras Cienc 85: 1275-1288.). Mkoma et al. (2014)Mkoma SL, Da Rocha GO, Domingos JSS, Santos JVS, Cardoso MP, Da Silva RL and De Andrade JB. 2014. Atmospheric particle dry deposition of major ions to the South Atlantic coastal area observed at Baía de Todos os Santos, Brazil. An Acad Bras Cienc 86: 37-55 have studied major ion species in order to establish the degree in which the emission of pollutants have affected the atmosphere on the coast of the Baía de Todos os Santos, in Salvador, northeastern Brazil (Mkoma et al. 2014Mkoma SL, Da Rocha GO, Domingos JSS, Santos JVS, Cardoso MP, Da Silva RL and De Andrade JB. 2014. Atmospheric particle dry deposition of major ions to the South Atlantic coastal area observed at Baía de Todos os Santos, Brazil. An Acad Bras Cienc 86: 37-55). As has been pointed out before, the concentration of ionic species could affect the quality of the nearby ecosystem and consequently, human health (He and Balasubramanian 2008He J and Balasubramanian R. 2008. Rain-aerosol coupling in the tropical atmosphere of Southeast Asia: distribution and scavenging ratios of major ionic species. J Atmos Chem 60: 205-220.). In a very comprehensive study, Mkoma and colleagues have shown the main sources for particle dry deposition and established that it formed a very important mechanism representing air-to-sea fluxes of major ions species. The cover of the present issue is dedicated to their study.

REFERENCES

  • Da Fonseca EM, Baptista Neto JA, Mcalister J, Smith B, Fernandez MA and Balieiro FC. 2013. The Role of the Humic Substances in the Fractioning of Heavy Metals in Rodrigo de Freitas Lagoon, Rio de Janeiro - Brazil. An Acad Bras Cienc 85: 1289-1301.
  • Da Silva PA, Borba VH, Dutra JMF, Leles D, Da-Rosa AAS, Ferreira LF and Araujo A. 2014. A new ascarid species in cynodont coprolite dated of 240 million years. An Acad Bras Cienc 86: 265-269.
  • Gallo V, Avilla LS, Pereira RCL and Absolon BA. 2013. Distributional patterns of herbivore megamammals during the Late Pleistocene of South America. An Acad Bras Cienc 85: 533-546.
  • He J and Balasubramanian R. 2008. Rain-aerosol coupling in the tropical atmosphere of Southeast Asia: distribution and scavenging ratios of major ionic species. J Atmos Chem 60: 205-220.
  • Hermes N, Schneider RCS, Molin DD, Riegel GZ, Costa AB, Corbellini VA, Torres JPM and Malm O. 2013. Environmental pathways and human exposure to manganese in southern Brazil. An Acad Bras Cienc 85: 1275-1288.
  • Holder MT, Erdmann MV, Wilcox TP, Caldwell RL and Hillis DM. 1999. Two Living Species of Coelacanths?”. Proceedings of the National Academy of Sciences of the United States of America 96(22): 12616-12620.
  • Johanson Z, Long JA, Talent JA, Janvier P and Warren JW. 2006. Oldest coelacanth, from the Early Devonian of Australia. Biol Lett 2: 443-446.
  • Lacerda LD, Bastos WR and Almeida MD. 2012. The impacts of land use changes in the mercury flux in the Madeira River, Western Amazon. An Acad Bras Cienc 84: 69-78.
  • Miguel R, Gallo V and Morrone JJ. 2014. Distributional patterns of †Mawsoniidae (Sarcopterygii: Actinistia). An Acad Bras Cienc 86: 159-170.
  • Mkoma SL, Da Rocha GO, Domingos JSS, Santos JVS, Cardoso MP, Da Silva RL and De Andrade JB. 2014. Atmospheric particle dry deposition of major ions to the South Atlantic coastal area observed at Baía de Todos os Santos, Brazil. An Acad Bras Cienc 86: 37-55
  • Silva DML, Camargo PB, Mcdowell WH, Vieira I, Salomão MSMB and Martinelli LA. 2012. Influence of land use changes on water chemistry in streams in the State of São Paulo, southeast Brasil. An Acad Bras Cienc 84: 919-930.
  • Souto PRF. 2000. Tetrapod coprolites from the middle Triassic of southern Brazil. Gaia, Geosci J 16: 51-57.
  • Vila Nova BC, Saraiva AAF, Moreira JKR and Sayão JM. 2011. Controlled excavations in the Romualdo Formation lagerstätte (Araripe Basin, Brazil) and pterosaur diversity: remarks based on new findings. Palaios 26: 173-179.

Publication Dates

  • Publication in this collection
    Mar 2014
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