Mangrove rehabilitation in the west coast of Aceh: issues and perspectives

The condition of mangroves pre- and post- tsunami and the socioeconomic role of mangrove forests in the livelihoods of coastal communities along the west coast of Aceh province, Indonesia are examined. The findings indicate that community livelihoods are significantly linked to the mangrove ecosystem. However, most of the mangrove rehabilitation programs are conservation orientated, aimed primarily at land conservation, and are not necessarily linked with livelihood options for local people or integrated resource management. This is a cause for concern as rehabilitation will only succeed when conservation measures are balanced with local community needs to obtain sustainable benefits from the rehabilitated systems. The rehabilitation efforts do involve the communities to a certain extent, but a more holistic and integrated approach needs to be adopted to ensure better management and sustainability of the rehabilitated mangrove forests.

Mangrove rehabilitation and coastal resource management: a case study of Cogtong Bay, Philippines

The Cogtong Bay experience represents a bold attempt to pursue a shared responsibility between the government and local residents for rehabilitating coastal resources. Some of the factors that provided the impetus to co-management arrangements were the recognition of resource management problems, dependence on coastal resources for livelihood and the desire for more sustainable resource use. This paper draws attention to the importance of legitimate user/property rights, vigilant law enforcement efforts, common commitment among stakeholders and continuing support from local leadership in viable co-management arrangements.

Mangrove forests and shrimp culture in Ngoc Hien District, Minh Hai Province, Vietnam

As a result of increased population growth, the attraction of high profits from shrimp culture and ineffective mangrove forest management, a number of serious environmental problems exist in Ngoc Hien District, Minh Hai Province, Vietnam. These environmental problems are highlighted in this article.

Present status of mangrove crab (Scylla serrata (Forskal)) culture in China

The status of mangrove crab (Scylla serrata) culture in China and suggestions on how this may become an important sector in the place are presented.

Modern dinoflagellate cysts found in surface sediments of Santa Cruz Island, Galapagos

Modern dinoflagellate cysts in surface sediments collected on Santa Cruz Island, Galapagos, are described, along with other palynomorphs such as microforaminiferal linings, tintinnid loricae, copepod eggs and acritarchs including Domasiella-like micro-remains and Halodinium spp. The dinoflagellate cyst assemblages mainly consisted of Spiniferites cf. scabratus (gonyaulacoid) followed by Brigantedinium spp. and Selenopemphix quanta (peridinioids). No gymnodinioid cysts were found. No remarkable differences in cyst composition and densities were recognized between stations. The cyst assemblages were characterized by low species diversity and low cyst concentrations in comparison with the Pacific coast of Guatemala and Peru. CDF Contribution Number 1019.

The Coleopteran fauna of exposed riverine sediments on the River Dane, Cheshire: A survey report

This is the Coleopteran Fauna of ERS on the river Dane, Cheshire: a survey report produced by the Environment Agency in 2003. A comprehensive survey of the Exposed Riverine Sediment (ERS) on the River Dane, Cheshire was undertaken between mid-April and mid-June 2003. 6 locations were selected and subsequently examined to determine the importance of the constituent invertebrate fauna. Appropriate sampling techniques (i.e. pitfall trapping, hand searching and excavations) were directed towards the target group (Coleoptera). All adults from the chosen taxa were identified to species level. The relative value of the fauna was assessed using species richness, conservation status, fidelity score and a site quality index.

Visual survey of exposed riverine sediments (Ers) in the Dane, Weaver and Bollin catchments

This is the Visual survey ERS Dane, Weaver & Bollin Catchments produced by the Environment Agency in 2005. Visual surveys of the River Dane downstream of the confluence with the Swettenham Brook, the River Weaver, and the River Bollin catchment in the EA Northwest South area of England were undertaken between 3rd and 9th February 2005 with the aim of identifying the spatial distribution and relative quality of exposed Riverine sediments (ERS). The potential value of these ERS in terms of likely habitat quality for ERS invertebrate communities was determined by recording a suite of appropriate environmental variables. Following an initial cartographical analysis of reaches likely to contain ERS, tens of kilometres of riverbank were inspected and 67 areas of ERS were selected for detailed visual survey. Site characteristics ranged widely both between and within catchments, with habitat quality ranging from poor to very high.

Foraminíferos como indicadores paleoecológicos do Holoceno no Manguezal de Guaratiba, Baía de Sepetiba, Rio de Janeiro

Os manguezais são ecossistemas estuarinos, representando a transição entre os ambientes continentais e marinhos, e tendo sua formação relacionada com as flutuações do nível do mar no Quaternário. No Manguezal de Guaratiba, diversos estudos sobre as variações do nível do mar, mais precisamente no Holoceno, têm sido realizados, sob os enfoques sedimentológicos, geoquímicos, palinológicos e micropaleontológicos. Entre os estudos micropaleontológicos, destacam-se os que utilizam os foraminíferos bentônicos, micro-organismos amplamente utilizados como indicadores paleoecológicos e paleoambientais do Holoceno. No presente trabalho, foi coletado, através de um amostrador do tipo trado russo, um testemunho (T1) no Manguezal de Guaratiba, no qual foram realizadas análises de parâmetros como granulometria, teores de matéria orgânica (MO), carbonato, carbono orgânico total (COT) e enxofre (S) (abióticos) e da fauna de foraminíferos bentônicos (bióticos). Foram utilizadas também índices ecológicos e análises de agrupamento, através das quais foi possível estabelecer quatro associações faunísticas (I,II,III e IV), assim como os fatores ambientais que mais influenciaram a distribuição da fauna. A correlação com assembleias de foraminíferos de outros testemunhos que possuem datação por Carbono 14 (C14), assim como outros trabalhos que versam sobre a evolução da Baía de Sepetiba, permitiu o estabelecimento de três ciclos de emersão-submersão para a área da planície de maré estudada: 1)Fase transgressiva: nível de concentração de conchas em depósitos lagunares formados por sedimentos finos, sem foraminíferos; provavelmente posterior a uma regressão; 2) Fase transgressiva: formação de uma baía, com presença exclusiva de espécies de foraminíferos calcários (Associação III) com maiores valores de riqueza e queda nos valores de COT; ocorrida há cerca de 3.800 anos A.P 3) Fase transgressiva: período de submersão, presença de espécies de foraminíferos tipicamente estuarinos (Associação IV), com duração entre 3.500 anos A.P. e 2.700 anos A.P.; 4)Fase transgressiva: caracterizada pela alternância entre a formação de baías rasas e lagunas marinhas (maiores índices de riqueza nas associações faunísticas), menores valores de MO e COT e aumento na proporção de sedimentos finos; evento iniciado há cerca de 2.700 anos A.P.; e 5)Fase regressiva: fauna de foraminíferos aglutinantes, resistente às condições de salinidade e acidez características de ambientes confinados como os manguezais, além do incremento nos teores de areia, evidenciando a fase final de confinamento da Baía de Sepetiba pela Restinga da Marambaia; evento iniciado por volta de 2.400 anos A.P., estendendo-se até o presente. Os resultados obtidos mostram a importância da correlação lateral entre testemunhos na interpretação paleoambiental da Baía de Sepetiba, além da identificação de estágios de transgressão e regressão que se aproximam da curva de variação do nível do mar proposta por SUGUIO et al.(1985) para o litoral do Estado do Rio de Janeiro

The history of contamination in sediments from the Mersey Estuary. Development of a chronology for the contamination of the Mersey Estuary by heavy metals and organochlorines

This is the history of contamination in sediments from the Mersey Estuary: Development of a chronology for the contamination of the Mersey Estuary by heavy metals and organochlorines Report produced by the Environment Agency in 1998. This report looks at the history of industrial contamination of the Mersey and Ribble Estuaries back to the early part of the last century, many decades before the start of monitoring programmes providing a remarkably detailed picture of very complex changes. There is a clear record in the sediment of the contamination by each heavy metal (including: Cu, Cr, Hg, Pb, Zn) and organochlorine chemical (including DDT isomers and PCB congeners) studied. The results of the study clearly show the increases in levels of contamination as industry expanded early last century followed by various improvements as this century progressed. Each pollutant has its own idiosyncratic pattern of change with some improvements predating modern environmental concerns whilst other changes seem to relate directly to recent improvements in legislative control. Overall, for the pollutants studied, the results clearly demonstrate the magnitude of improvement that has been achieved in what was a very polluted area. The only major reservation to this story is that despite the wide range of substances covered, many other potentially important pollutants remain to be studied in a similar manner.