ESR dating of pleistocene mammal teeth and its implications for the biostratigraphy and geological evolution of the coastal plain, Rio Grande do Sul, southern Brazil

The fossiliferous deposits in the coastal plain of the Rio Grande do Sul State, Southern Brazil, have been known since the late XIX century; however, the biostratigraphic and chronostratigraphic context is still poorly understood. The present work describes the results of electron spin resonance (ESR) dating in eleven fossil teeth of three extinct taxa (Toxodon platensis, Stegomastodon waringi and Hippidion principale) collected along Chui Creek and nearshore continental shelf, in an attempt to assess more accurately the ages of the fossils and its deposits. This method is based upon the analysis of paramagnetic defects found in biominerals, produced by ionizing radiation emitted by radioactive elements present in the surrounding sediment and by cosmic rays. Three fossils from Chui Creek, collected from the same stratigraphic horizon, exhibit ages between (42 +/- 3) Ka and (34 +/- 7) Ka, using the Combination Uptake model for radioisotopes uptake, while a incisor of Toxodon platensis collected from a stratigraphic level below is much older. Fossils from the shelf have ages ranging from (7 +/- 1) 10(5) Ka to (18 +/- 3) Ka, indicating the mixing of fossils of different epochs. The origin of the submarine fossiliferous deposits seems to be the result of multiple reworking and redeposition cycles by sea-level changes caused by the glacial-interglacial cycles during the Quaternary. The ages indicate that the fossiliferous outcrops at Chui Creek are much younger than previously thought, and that the fossiliferous deposits from the continental shelf encompass Ensenadan to late Lujanian ages (middle to late Pleistocene). (C) 2009 Elsevier Ltd and INQUA. All rights reserved.

Development of Dichelops melacanthus and its egg parasitoid Telenomus podisi reared on Bt-soybean MON 87701 x MON 89788 and its near conventional isoline under different temperatures.

Dichelops melacanthus was studied under controlled conditions (60 ± 10% RH and 14/10 h L/D photoperiod), and three constant temperatures (19, 25, and 31 ± 2 °C). Fresh pods of MON 87701 × MON 89788 soybeans and its near non-Bt isoline (A5547) were supplied to nymphs and adults. The biology of T. podisi was studied in the same controlled RH conditions, but only at the standard temperature of 25 ± 2°C. Overall, the development of D. melacanthus was better at higher temperatures, which accelerated the development of the stink bug without affecting adult biological parameters. No influence of Bt-soybeans on the biology of the pest was observed in any temperature studied, which shows that D. melacanthus is not affected by this transgenic soybean. The egg parasitoid T. podisi also was not harmed when it parasitized eggs of the pest fed with MON 87701 × MON 89788 soybeans, with similar results to those obtained in non-Bt isogenic soybeans. Thus, this study demonstrates that D. melacanthus is favored at high temperatures (31 ± 2 °C), and that neither did MON 87701 × MON 89788 soybean pods affect the development of the pest nor its parasitoid T. podisi.

CT scanning in archaeology

In this chapter we will review the use of x-ray computed tomography (CT) scanning in the field of archaeology. The story will be told in roughly chronological order, starting with the first reported use of a CT scanner in the field of archaeology and then look at some some possibilities for the future. Since the introduction of the x-ray CT scanner in the 1970’s the quality of the images has steadily improved enabling the role of the CT scanner to expand into the field of archaeology. In the context of this chapter, archaeology will be deemed to include the study of ancient human remains and artefacts but exclude remains from pre-history, which normally comes under the heading of palaeontology. (It would perhaps be appropriate to note that CT scanners have been successfully applied in the study of fossils). CT scans have mostly been used to study mummies but have also been used to examine other archaeological artefacts such as clay tablets, scrolls, pottery, bronze statues and swords.

How do heterogametic females survive without gene dosage compensation?

When the male is the heterogametic sex (XX♀-XY♂ or XX♀-XO♂), as inDrosophila, orthopteran insects, mammals andCaenorhabditis elegans, X-linked genes are subject to dosage compensation: the single X in the male is functionally equivalent to the two Xs in the female. However, when the female is heterogametic (ZZ♂-ZW♀), as in birds, butterflies and moths, Z-linked genes are apparently not dosage-compensated. This difference between X-linked and Z-linked genes raises fundamental questions about the role of dosage compensation. It is argued that (i) genes which require dosage compensation are primarily those that control morphogenesis and the prospective body plan; (ii) the products of these genes are required in disomic doses especially during oogenesis and early embryonic development; (iii) heterogametic females synthesize and store during oogenesis itself morphogenetically essential gene products - including those encoded by Z-linked genes — in large quantities; (iv) the abundance of these gene products in the egg and their persistence relatively late into embryogenesis enables heterogametic females to overcome the monosomic state of the Z chromosome in ZW embryos. Female heterogamety is predominant in birds, reptiles and amphibians, all of which have megalecithal eggs containing several thousand times more maternal RNA and other maternal messages than eggs of mammals,Caenorhabditis elegans, orDrosophila. This increase in egg size, yolk content and, concomitantly, the size of the maternal legacy to the embryo, may have facilitated female heterogamety and the absence of dosage compensation.

Power analysis for detecting trends in juvenile spotted seatrout abundance in Florida Bay

The spotted seatrout (Cynoscion nebulosus) is considered a key species relative to the implementation of the Comprehensive Everglades Restoration Plan (CERP). One of the goals of the CERP is to increase freshwater flows to Florida Bay. Increased freshwater flows can have potential positive and negative impacts on spotted seatrout populations. At low salinities, the planktonic eggs of spotted seatrout sink to the bottom and are not viable (Alshuth and Gilmore, 1994; Holt and Holt, 2002). On the other hand, increased freshwater flows can alleviate hypersaline conditions that could result in an expansion of the distribution of the early life stages of spotted seatrout (Thayer et al., 1999; Florida Department of Environmental Protection1). Thus it would be useful to develop a monitoring program that can detect changes in seatrout abundance on time scales short enough to be useful to resource managers. The NOAA Center for Coastal Fisheries and Habitat Research (NOAA) has made sporadic collections of juvenile seatrout using otter trawls since 1984 (see Powell et al, 2004). The results suggest that it might be useful to sample for seatrout in as many as eight different areas or basins (Figure 1): Bradley Key, Sandy Key, Johnson Key, Palm Key, Snake Bight, Central, Whipray and Crocodile Dragover. Unfortunately, logistical constraints are likely to limit the number of tows to about 40 per month over a period of six months each year. Inasmuch as few seatrout are caught in any given tow and the proportion of tows with zero seatrout is often high, it is important to determine how best to allocate this limited sampling effort among the various basins so that any trends in abundance may be detected with sufficient statistical confidence. (PDF contains 16 pages)

Reavaliação deposicional da Bacia de São José de Itaboraí com base em dados geológicos e geofísicos

A Bacia de São José de Itaboraí está localizada no Município de Itaboraí, no Estado do Rio de Janeiro. Ela foi descoberta em 1928, pelo Engenheiro Carlos Euler, que após analisar um suposto caulim encontrado na Fazenda São José pelo seu então proprietário, Sr. Ernesto Coube, verificou que se tratava de calcário. Os Professores Rui Lima e Silva e Othon H. Leonardos, enviados ao local para estudos, encontraram uma grande quantidade de fósseis de gastrópodes continentais, despertando o interesse científico pela região. Os estudos preliminares de campo e análises químicas evidenciaram boas perspectivas de exploração do calcário para a fabricação de cimento do tipo Portland. Por mais de 50 anos, a Companhia Nacional de Cimento Portland Mauá (CNCPM) explorou a pedreira. Desde sua descoberta, a Bacia de São José, paralelamente às atividades de mineração, foi objeto de pesquisas científicas realizadas por geólogos, paleontólogos e arqueólogos. No início da década de 80, a Cia. de Cimento Mauá decidiu abandonar a área em função do esgotamento econômico da reserva de minério. Com a retirada das bombas que impediam a inundação da pedreira, formou-se uma lagoa que passou a impedir o livre acesso aos afloramentos. Desde então as pesquisas sobre a Bacia ficaram concentradas aos materiais coletados no período de exploração de calcário. Material esse distribuído no Museu Nacional (MN), Departamento Nacional da Produção Mineral (DNPM), Instituto de Geociências da UFRJ, entre outros. Em 1990, a área que pertencia a CNCPM foi desapropriada por pressão da comunidade científica. A mesma passou a pertencer ao Município de Itaboraí, que criou o Parque Paleontológico de São José de Itaboraí, por meio da Lei 1.346, de 12 de dezembro de 1995. O objetivo desse trabalho foi gerar novos dados através do método geofísico conhecido como magnetometria. Para isso foram realizados levantamentos de campo utilizando um magnetômetro portátil e GPS, foram analisados e corrigidos dados utilizando softwares específicos, elaborados modelos e criados perfis a partir de descrições de testemunhos de sondagem. Os resultados obtidos visam possibilitar uma nova interpretação da geologia e da estratigrafia da bacia, dando condições para que se possa ter uma atualização dos conhecimentos relacionados à região, após quase meio século de atividade mineradora.

Huevos y larvas de tres especies de peces marinos, Anchoa marinii, Brevoortia aurea y Prionotus nudigula

The description of the embryonic and early larval stages of three species of marine fishes: the anhovy, Anchoa marinii, the menhaden Brevoortia aurea and the gurnard, Prionotus nudigula is given. The time required from the fertilization to the hatching for each species was calculated. The eggs of these three species are found in the plankton collected in the zone situated in the vicinity of Mar del Plata. The eggs are only found in the plancton which was close to the shore. The anchoa marinii eggs are found in the sea from the middle of December at a water temperature of approximately 16,0°C to the end of April. Their greatest concentration takes place in January at 20,0-21,0°C. The eggs of Brevoortia aurea are found in the plakton from the beginning of October at a water temperature of approximately 10,0°C to the middle of December. Their greatest concentration takes place in November at 13,0-15,0°C. Only once were the menhaden's eggs can be found in the sea from the middle of November at the water temperature of aproximately 13,0° to the end of April. Their greatest concentration takes place in January and February at 20,0-21,0°C.

Estudo fenotípico da região Aorta-Gônada-Mesonefros, de embriões de galinhas Gallus gallus domesticus, com ênfase na aorta dorsal

Acredita-se que os primeiros progenitores da hematopoese definitiva surjam da diferenciação do endotélio da aorta dorsal, na altura da região da Aorta-Gônada-Mesonefros (AGM). Com o intuito de estudar esta região e o fenótipo das células do endotélio da aorta dorsal nesta posição topográfica, ovos galados de Gallus gallus domesticus L. foram incubados em chocadeira, classificados em estádios de E16 a E25 e processados histotecnologicamente para obtenção de secções seriadas na altura da região AGM. Estas passaram por coloração por Hematoxilina-Eosina, histoquímica para PAS, PAS-diastase e Alcian Blue pH 1.0 e pH 2.5, histoquímica por lectinas fluoresceinadas e imunofluorescência para moléculas de superfície, citoesqueleto e matriz extracelular. Foi observada hipertrofia endotelial no assoalho da aorta nos estádios observados, o qual se apresentava positivo ao PAS, com ocorrência frequente de vacuolizações basais PAS negativas, e o surgimento ocasional de grupamentos celulares intravasculares. Nestes, as células que se destacavam da membrana basal do endotélio expressavam progressivamente mais material PAS positivo, o qual, no entanto, em nenhum momento pareceu se tratar de glicogênio. Em relação às glicosaminoglicanas, notamos a presença predominante de ácido hialurônico por todo o mesênquima da região e em outras estruturas como periferia da notocorda, tubo neural e mesoderma lateral. Ocorreu co-expressão de fibronectina e α-actina de músculo liso em células circunjacentes à aorta, na face ventral do vaso. GFAP e BMP-4 são expressas entre as células do tubo neural e em sua periferia, assim como na notocorda do embrião. As lectinas Abrus precatorius, Lens culinarise Ricinus communis mostraram-se positivas principalmente na região subedotelial do assoalho da aorta nos estádios observados neste trabalho. Bandeiraea simplicifolia exibiu pouca marcação na aorta dorsal e a Arachis hypogeae foi negativa. Outras estruturas da região AGM também expressaram resíduos de açúcares revelados por estas lectinas, tais como: notocorda, tubo neural, mesênquima, intestino primitivo e saco vitelínico. Estes resultados acrescentam elementos morfológicos e bioquímicos ao conhecimento sobre a região AGM de embriões de galinha e sobre o endotélio, possivelmente hemogênico, da aorta dorsal.

As comunidades de anfíbios e lagartos dos remanescentes de restingas do estado do Espírito Santo: uma análise da ocorrência e distribuição das espécies

Ecologicamente, comunidades são conjuntos de populações convivendo no mesmo espaço e tempo. A forma como as espécies que compõem estas comunidades, como elas se distribuem e como estão estruturadas, depende de inúmeros fatores, entre eles históricos, biogeográficos e evolutivos. Neste estudo, buscamos compreender como as comunidades de anfíbios anuros e de lagartos estão estruturadas e quais fatores ambientais e de degradação são determinantes nesta estruturação. Amostramos cinco remanescentes de restinga no estado do Espírito Santo, utilizando método de procura ativa em transecções lineares nas diferentes fisionomias vegetais destes ecossistemas. Realizamos amostragens nas estações seca e de chuvas em todas as restingas, e somamos um total de 60 horas de esforço amostral para os anfíbios e 75 horas para os lagartos. Registramos um total de 32 espécies de anfíbios anuros conjuntamente nos cinco remanescentes de restinga, sendo duas destas espécies endêmicas deste ecossistema: Scinax agilis e Melanophryniscus setiba. A restinga do Parque Paulo Cesar Vinha foi o remanescente com a maior riqueza de espécies de anuros, enquanto a restinga da Reserva Biológica de Comboios foi, comparativamente, o remanescente com menor riqueza de espécies. Em termos de composição de espécies, as restingas de Praia das Neves e Paulo Cesar Vinha foram as mais similares, enquanto a restinga de Comboios foi a mais distante na análise de agrupamento. Registramos no conjunto de restingas seis modos reprodutivos para as espécies de anuros, sendo 75% deles relacionados aos ambientes aquáticos. A disponibilidade de locais de desova esteve positivamente relacionada à riqueza de espécies. Todos os mesohábitats das restingas, com exceção das fitofisionomias de halófila-psamófila, foram utilizados pelos indivíduos registrados, entretanto, uma porcentagem considerável dos indivíduos foi encontrada nos alagados. Em relação às comunidades de lagartos, adotamos além dos nossos dados, aqueles disponíveis em Dias e Rocha (2014) e aqueles disponíveis em Winck (2012). Registramos um total de 23 espécies de lagartos nos remanescentes de restinga amostrados nos estados do Rio de Janeiro, Espírito Santo e Bahia. Observamos que as comunidades presentes nos remanescentes estudados possuem considerável diferenciação entre elas. A diversidade beta (β) foi elevada enquanto o grau de aninhamento foi intermediário. Registramos ainda a presença do lagarto exótico invasor Hemidactylus mabouia em ambiente natural nos remanescentes de restinga estudados neste Tese. Encontramos 45 indivíduos, distribuídos em três dos cinco remanescentes amostrados. Registramos ainda ovos de H. mabouia (2 deles eclodidos) em dois dos cinco locais estudados, indicando que o recrutamento de indivíduos está ocorrendo com sucesso nas populações invasoras. A presença de H. mabouia esteve relacionada à restingas com maior frequência de degradação ambiental. Consideramos que os dados obtidos nesta tese, fornecem informações de considerável importância para o entendimento da estrutura das comunidades de anfíbios e lagartos nos ecossistemas de restinga ao longo da costa brasileira

The co-evolutionary relationship between bitterling fishes and freshwater mussels: insights from interspecific comparisons

Hypothesis: In parasites that use hosts for offspring development, adults may base oviposition decisions on a range of host traits related either to host quality or the co-evolutionary relationship between parasite and host. We examined whether host quality or co-evolutionary dynamics drive the use of hosts in the bitterling-mussel relationship. Organisms: Six species of bitterling fish (Acheilognathinae) and eight species of freshwater mussels (Unionidae, Corbiculidae) that are used by bitterling for oviposition. Site of experiments: Experimental tanks in Wuhan, China, at the site of the natural distribution of the studied species. Methods: Three experiments that controlled for host accessibility and interspecific interactions were conducted to identify host preferences among bitterling fishes and their mussel hosts. We started with a broad interspecific comparison. We then tested bitterling behavioural choices, their temporal stability, and mussel host ejection behaviour of the eggs of generalist and specialist bitterling species. Finally, we measured host mussel quality based on respiration rate and used published studies on mussel gill structure to infer mussel suitability as hosts for bitterling eggs. Results: We found significant interspecific differences among bitterling species in their use of mussel hosts. Bitterling species varied in their level of host specificity and identity of preferred hosts. Host preferences were flexible even among apparently specialized species and fishes switched their preferences adaptively when the quality of individuals of preferred host species declined. Mussels varied considerably in their response to oviposition through egg ejections. Host preference by a generalist bitterling species correlated positively with host quality measured as the efficiency of the mussel gills to extract oxygen from inhaled water. Host ability to eject bitterling eggs correlated positively with their relative respiration rate, probably due to a higher velocity of water circulating in the mussel gill chamber.

Foreign gene transfer into Chinese shrimps (Penaeus chinensis) with gene gun

Plasmids pG DNA-RZ1 with a GFP (green fluorescent protein) reporter gene and a ribozyme gene incising penaeid white spot baculovirus (WSBV) were first introduced into the fertilized eggs of Chinese shrimps by gene gun. The treated and control samples of different development stages were observed with a fluorescent microscope. The transient expression of GFP gene was high in nauplius and zoea larvae. Results from RT-PCR and PCR for adults showed that the foreign genes had been transferred into the shrimps and had expressed the corresponding proteins. This work has established a transgenic method for penaeid shrimps, which will set base for the application of genetic engineering breeding into industry.

重庆老龙洞二叠系-三叠系界线地层微生物岩研究

The largest mass extinction in the Phanerozoic happened at the end of the Permian. The microbialites formed in the extreme environments after the mass extinction has become a hotspot for geologists and paleontologists throughout the world. The dendroid microbialites that were described for the first time in 1999 from the Permian-Triassic boundary section at Laolongdong, Chongqing, have been studied by many geologists from China and overseas. Two important viewpoints about their origin have been proposed. Some researchers believed that they resemble Quaternary travertine shrubs in form, and may belong to microbialites. Some other researchers proposed that the dendroid structure is composed of clots formed by coccoidal cynaobacteria, and is microbialite. Our detailed survey on the section reveals that: (1) there is an interval of speckled “microbialite” in the section, and it underlies the dendroid “microbialite”, (2) the dendroid “microbialite” does not always have dendroid appearance; they are dendroid only in very local places; they are not dendroid in most places; for this reason, they are not comparable to recent tufa; (3) the volume of the dendroid structure greatly increases toward the top of the dendroid microbialite interval: accounting to 70% of the whole rock in the top part. This distribution pattern implies that the formation of this structure may be related to downward migration of the diagenetic fluid. Examination of thin sections reveals that the dendroid structure or point-like structure in the “microbialite” look as lighter areas in the thin sections and are composed of large blocky clear calcites containing scattered yellow dirty small calcite rhombi and irregular “points” of relict lime mudstone or wackestone or packstone. Their formation is by any one of the following two processes: (1) dissolution → filling of large blocky calcite; (2) dolomitization → dedolomitization → dissolution by meteoric fresh water → filling by large blocky calcites. It has been found that there are at least two sea-level falls during the P-T transition. As the sea level fall, the carbonate deposits came into supratidal environment, and suffered dolomitization caused by evaporative fluid or mixing water of sea water and meteoric water. Since the fluid migrated downward from the top of the deposits and in random pathway, the dolomitization formed dendroid or speckled dolomitic areas. As the deposits came into subaerial environments, the meteoric fresh water migrated along the dendroid or speckled dolomitic area with higher porosity, and dissolution happened, which caused the rock became spongy or alveolate. In later time, after the strata came into phreatic zone, large clear blocky calcites grew in and filled the pores in the spongy areas. The dendroid and speckled structure were formed in this way, rather than composed of clots formed by coccoid cyanobecteria. The microbial fossils in Laolongdong section include two types. The first is the tube-like cyanobecteria in middle Bed 3, which are generally less than 1 mm in length, taper toward one end, and are internally filled by microspars. They are straight or sinuous, with micritic wall 0.005~0.01 mm thick. Since this kind of microbial fossils are abundant in middle Bed 3, this rock belongs to microbialite. The second type occurs in Bed 5 and lower and middle Bed 6. They are irregular globular in shape, generally 0.2 ~ 0.5 mm in size, with several outward progresses, and internally filled by one layer of needle-like calcite cements on the wall and the large blocky calcite in the inner space. According to their shape and preservation way, it is inferred that this kind of fossils were formed from some kind of bacterial colony. The bacterial colony may be cuticle in composition, since it has some hardness as it is indicated by its resistance to deposit loading. These organisms discomposed during diagenetic time, and formed good porosity. In later diagenetic time, these pores were firstly cemented by needle-like calcites and later filled by large blocky calcites. So, the bacterial colony promoted the formation of dendroid and speckled structures. However, they did not always form such structures. On the other hand, even though no bacterial colony or other microbes or any kind of fossils were present, dendroid or speckled structures can form. Bed 4 of Laolongdong section contains abundant gastropods but no microbial fossils, and is not microbialite, even though it is speckled. The top of Bed 6 is dendroid, but contain no microbial fossils, and is not micrbialite.

甘肃临夏盆地龙担剖面晚新生代磁性地层与古环境

Linxia Basin, situated in the northeast belt of the Tibetan Plateau, is a late Cenozoic depression basin bounded by the Tibetan Plateau and the Chinese Loess Plateau. The Cenozoic deposition, spanning over 30Ma, in which very abundant mammal fossils were discovered, is very suitable for study of uplift processes and geo-morphological evolution of the Tibetan Plateau. The Longdan section (35°31′31.6″N，103°29′0.6″E) is famous for the middle Miocene Platybelodon fauna and the late Miocene Hipparion fauna for a long time and is also one of the earliest known places for wooly rhino, which lies on the east slope of Longdan, a small village of township Nalesi in the south of the Dongxiang Autonomous County, Linxia Hui Nationallity Autonomous Prefecture. The Longdan mammal fauna was discovered at the base of the Early Pleistocene loess deposits at Dongxiang, where the lithology is different from the typical Wucheng Loess on the Chinese Loess Plateau. The rich fossils contain many new species and the major two layers of fossils are in the loess beds. Geologically the fossiliferous area is located in the central part of the Linxia Cenozoic sedimentary basin. Tectonically the Linxia Basin is an intermountain fault basin, bordered by the Leijishan major fault in the south and the north Qinling and Qilianshan major faults in the north. The section is 51.6m thick above the gravel layer, including the 1.6m Late Pleistocene Malan Loess on the top and the other loess-paleosol sequences in the middle of the section. The base of the section is the Jishi Formation, consisting of gravel layer of 13 ~ 17m thick. In this study, 972 bulk samples were collected with an interval of 5cm and other 401 orientied samples were taken with a magnetic compass. In the laboratory, the paleomagnetism, medium grain size, susceptibility, color, micromorphology, anisotropy of magnetic susceptibility were analyzed. From the stratigraphic analysis, the Longdan section from the top 0.3m to the bottom 51.6m, containing 5 normal polarities (N1-N5) and 5 reversal polarities (R1-R5). The paleomagnetic results show N3 is the Olduvai subchron in the middle of the Matuyama chron, and then the chronology of the Longdan mammal fauna is constructed along the section. The Matuyama-Gauss boundary is 45m and N5 enters Gauss chron. The Olduvai subchron with the age of 1.77 ~ 1.95Ma is found just in the upper fossiliferous level of Longdan mammal fauna. Taking the deposit rate of the section into account, the geological age of the upper fossiliferous level of Longdan mammal fauna is estimated to be about 1.9Ma. The lower fossiliferous level is just below the Reunion subchron and its age is estimated to be 2.25Ma. In addition, anisotropy of magnetic susceptibility of the loess-paleosol and other climatic indexes were used for discussing the late Cenozoic paleoenvironmental changes at Longdan, from which the Longdan area should have been an area of predominantly steppe the same as the Longdan mammal fauna.

新元古代陡山沱期古海洋的氧化还原环境演变

High resolution geochemical analysis of Ediacaran Doushantuo Formation deposits in eastern Gorges area, including carbon and sulfur isotope compositions, trace elements, rare earth elements, and so on, show a whole panorama of the oceanic environment in Ediacaran Doushantuo Formation. The deposits of Doushantuo II recorded consistent δ13Corg values and variable δ13Ccarb values, which suggets that it is strongly redox stratified in Doushantuo ocean, and there is a large DOC reservior in the deep ocean. The redox state of Doushantuo ocean in Yangtze area was not steady. The movement of chemocline was concerned with the transgression and/or regression. During the transgression, raising sea level and upwelling with anoxic deep water would cause the ocean anoxic; during the regression, declining sea level and weathered sulfate input would cause the suface ocean becoming oxic. The oxidations of this DOC reservior would caused negative δ13C excurions in Doushantuo Formation. Comparing with oceanic redox states and fossils productivity, we found that the stratum with high biologic productivity and diversity did not indicated oxic conditions. In the opposite, these stratum recorded anoxic conditions. We suggeste that it would be relatived to burial and preservation of fossils, because anoxic conditions are in favor of burial and preservation of fossils. It is proved that methane seep occurred at the base of Duoshantuo cap carbonate. However, comparing cap carbonate with seep carbonate, we found that oxidation of methan and the post-diagenesis could not derictely result in cap carbonate deoposition. Cap carbonate would be derived from the high level CO2 in atomosphere.

Melanism and disease resistance in insects

There is growing evidence that insects in high-density populations invest relatively more in pathogen resistance than those in low-density populations (i.e. density-dependent prophylaxis). Such increases in resistance are often accompanied by cuticular melanism, which is characteristic of the high-density form of many phase polyphenic insects. Both melanism and pathogen resistance involve the prophenoloxidase enzyme system. In this paper the link between resistance, melanism and phenoloxidase activity is examined in Spodoptera lanae. In S. exempta, cuticular melanism was positively correlated with phenoloxidase activity in the cuticle, haemolymph and midgut. Melanic S. exempta larvae were found to melanize a greater proportion of eggs of the ectoparasitoid Euplectrus laphygmae than non-melanic larvae, and melanic S. littoralis were more resistant to the entomopathogenic fungus Beauveria bassiana (in S. exempta the association between melanism and fungal resistance was non-signficant). These results strengthen the link between melanism and disease resistance and implicate the involvement of phenoloxidase.