Clam dredging effects and subsequent recovery of benthic communities at different depth ranges     

R. Constantino  M.B. Gaspar  J. Tata-Regala  S. Carvalho  J. Cúrdia  T. Drago  R. Taborda  C.C. Monteiro 《Marine environmental research》2009,67(2):89-99

This study aimed to assess the potential effects of clam dredging and the subsequent recovery of the benthic environment. Two experimental areas located at 6 and 18 m depth were established in order to analyse whether impacts and recovery of benthic environment are depth-related. Study areas were located within an area closed to dredging and two different plots were established at both depths. One of the plots was subjected to intense clam dredge-fishing, while the other was undisturbed and therefore used as control. Sampling followed a BACI design, with samples for macrobenthic, meiobenthic and sediment particle size analysis being taken by SCUBA divers from both areas before and after fishing stress. For both depths, impacts on the benthic environment were very low resulting in high recovery rates. Nevertheless, at shallower depths communities demonstrated a faster recovery. It was shown that depending on the faunal component used as a bioindicator, different results can be observed. Generally deposit-feeding organisms with scales or chitinous plates and vermiform shape (mainly crustaceans, polychaetes and ophiuroids), without external protection, were the most affected by dredging, while some polychaetes without external protection and with a carnivorous feeding mode seemed to be enhanced by fishing. The low level of perturbations induced by the dredging activities was comparable to the impact of surface waves on the bottom, as experiments were undertaken in wave-dominated environments. The coexistence of storm events during the study period proved to have similar or even more deleterious effects on the benthic environment. It appears that communities from hydrodynamic fishing grounds that are well adapted to natural physical stress are not highly affected by dredging.  相似文献   

Distribution patterns of macrobenthic species in relation to organic enrichment within aquaculture earthen ponds   总被引：1，自引：0，他引：1  

Carvalho S  Barata M  Pereira F  Gaspar MB  Cancela da Fonseca L  Pousão-Ferreira P 《Marine pollution bulletin》2006,52(12):1573-1584

The relationship between organic enrichment and macrobenthic colonization patterns was investigated during an 8-month period in Diplodus sargus (white seabream) production ponds. A stratified sampling design was applied and each pond was divided into three zones: water entrance (WE); central (C); and automatic feeder zones (AF). Generally, the number of species and Shannon–Wiener diversity increased from the WE to the AF zone. Abundance did not present a clear trend. The recently developed marine biotic index (AMBI) was applied and showed to be sufficiently robust to discriminate, within a relatively small area, differences in macrobenthic communities due to organic enrichment. Nevertheless, caution is advised when applying this index or others based on ecological group’s assignment, as the classification of a certain area may differ when allocating a certain species to an unsuitable group. This is particularly evident when common species are involved.  相似文献   

Short-term environmental impact of clam dredging in coastal waters (south of Portugal): chemical disturbance and subsequent recovery of seabed   总被引：6，自引：0，他引：6  

Falcão M  Gaspar MB  Caetano M  Santos MN  Vale C 《Marine environmental research》2003,56(5):649-664

The physical and chemical changes in sediment and near bottom water caused by clam dredging were examined during July and September 1999, at two locations Vilamoura (VL) and Armona (AR), south coast of Portugal. Sediment cores and near bottom water were collected simultaneously before dredging (control samples) and within short time intervals (min-h) after dredging. After dredging operations, microphytobenthos coming from the path were accumulated in the re-worked sediment (ridge). Chlorophyll a in superficial sediment increased from 1.2 microg x g(-1) before dredging to 1.7 microg x g(-1) after dredging and these higher values remained for a few hours. However, the expected increase of chlorophyll a in near bottom water due to re-suspension was not observed. After sediment disturbance an instantaneous sorption of phosphorus onto iron oxides occurred in the upper sediment layers (from 2 to 3 micromol x g(-1) before dredging to 4-5 micromol x g(-1) after dredging). A microcosm experiment showed that after sediment disturbance HPO(4)(2-) dissolved in pore water decreased from 40 to 10 microM being simultaneously sorbed onto iron oxides formed in the top layer of sediment. The ammonium, nitrates, organic nitrogen, phosphate and silicate dissolved in pore water decreased immediately after dredging activity and simultaneously an increase in near bottom water was sporadically observed. Generally, the re-establishment of seabed was reached within a short time (min-h), at both stations (VL and AR).  相似文献   

The last 5000 years of activity at Sete Cidades volcano (São Miguel Island,Azores): Implications for hazard assessment     

G. Queiroz  J.M. Pacheco  J.L. Gaspar  W.P. Aspinall  J.E. Guest  T. Ferreira 《Journal of Volcanology and Geothermal Research》2008

Sete Cidades is a central volcano with a summit caldera at the western end of São Miguel Island, Azores. Its stratigraphy comprises two main geological groups: the Inferior Group, the units of which date from more than 200 000 years ago through to 36 000 years before present, consisting of thick lava flows and subaerial volcaniclastic deposits that built the base of the central volcano; and the Superior Group which comprises all the activity from the last 36 000 years, including pumice and scoria fallout and PDC deposits with minor lava flows. The volcanostratigraphy is divided into six main formations — Risco, Ajuda, Bretanha, Lombas, Santa Bárbara and Lagoas, each defined by different activity phases in the volcano's evolution.  相似文献   

Contrasting styles of explosive eruption at Sete Cidades,São Miguel,Azores, in the last 5000 years: Hazard implications from modelling     

P.D. Cole  J.M. Pacheco  R. Gunasekera  G. Queiroz  P. Gonçalves  J.L. Gaspar 《Journal of Volcanology and Geothermal Research》2008

The deposits of three eruptions in the last 5000 years are described in detail in order to constrain eruptive parameters and allow a quantitative assessment of the hazard from a range of explosive eruption types at Sete Cidades volcano, São Miguel, Azores. These deposits include: the Caldeira Seca eruption (P17) which occurred around 600 yr BP, which was the last explosive event from inside the Sete Cidades caldera, the P11 eruption, dated at 2220 ± 70 yr BP, and the undated P8 eruption (< 3000 yr BP). These deposits were chosen to represent the range of likely explosive activity from the caldera.  相似文献   

Growth and extremely high production of the non-indigenous invasive species Corbicula fluminea (Müller, 1774): Possible implications for ecosystem functioning     

Ronaldo Sousa  António J.A. Nogueira  Miguel B. Gaspar  Carlos Antunes  Lúcia Guilhermino 《Estuarine, Coastal and Shelf Science》2008

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Effect of tooth spacing and mesh size on the catch of the Portuguese clam and razor clam dredge   总被引：1，自引：1，他引：0  

Gaspar  M. B.; Castro  M.; Monteiro  C. C. 《ICES Journal of Marine Science》1999,56(1):103-110

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Rebuilding viable spawner patches of the overfished Spisula solida (Mollusca: Bivalvia): a preliminary contribution to fishery sustainability     

Joaquim  Sandra; Gaspar  Miguel B.; Matias  Domitilia; Ben-Hamadou  Radhouan; Arnold  William S. 《ICES Journal of Marine Science》2008,65(1):60-64

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Grappling with Growth: Perceptions of Development and Preservation in Faster- and Slower-Growing Amenity Communities*     

Minkyung Park  Monika Derrien  Emilian Geczi 《社会与自然资源》2019,32(1):73-92

Amenity-rich rural communities attract tourists, retirees, second-home owners, and others whose values are often assumed to conflict with those of longtime residents. While prior research has examined attitudinal differences across types of residents, questions about the effects of community growth on residents’ attitudes remain unanswered. This study examines whether and how seasonal and permanent residents differ within and across towns experiencing different rates of growth, and the implications of differences for attitudes toward community development and preservation. Results showed that permanent residents (both short- and long-term) perceived community development initiatives as more important to maintaining future quality of life than did seasonal homeowners. Further, community growth rates had statistically significant effects: residents of slower-growth towns attributed higher importance to both development and preservation initiatives than did residents of faster-growing towns. Growth rate was thus a stronger predictor of attitudes toward both development and preservation than resident type.  相似文献   

The Catalão I niobium deposit, central Brazil: Resources, geology and pyrochlore chemistry     

Pedro Filipe de Oliveira Cordeiro  José Affonso Brod  Matheus Palmieri  Claudinei Gouveia de Oliveira  Elisa Soares Rocha Barbosa  Roberto Ventura Santos  José Carlos Gaspar  Luis Carlos Assis 《Ore Geology Reviews》2011,41(1):112-121

The Catalão I alkaline–carbonatite–phoscorite complex contains both fresh rock and residual (weathering-related) niobium mineralization. The fresh rock niobium deposit consists of two plug-shaped orebodies named Mine II and East Area, respectively emplaced in carbonatite and phlogopitite. Together, these orebodies contain 29 Mt at 1.22 wt.% Nb₂O₅ (measured and indicated). In closer detail, the orebodies consist of dike swarms of pyrochlore-bearing, olivine-free phoscorite-series rocks (nelsonite) that can be either apatite-rich (P2 unit) or magnetite-rich (P3 unit). Dolomite carbonatite (DC) is intimately related with nelsonite. Natropyrochlore and calciopyrochlore are the most abundant niobium phases in the fresh rock deposit. Pyrochlore supergroup chemistry shows a compositional trend from Ca–Na dominant pyrochlores toward Ba-enriched kenopyrochlore in fresh rock and the dominance of Ba-rich kenopyrochlore in the residual deposit. Carbonates associated with Ba-, Sr-enriched pyrochlore show higher δ¹⁸O_SMOW than expected for carbonates crystallizing from mantle-derived magmas. We interpret both the δ¹⁸O_SMOW and pyrochlore chemistry variations from the original composition as evidence of interaction with low-temperature fluids which, albeit not responsible for the mineralization, modified its magmatic isotopic features. The origin of the Catalão I niobium deposit is related to carbonatite magmatism but the process that generated such niobium-rich rocks is still undetermined and might be related to crystal accumulation and/or emplacement of a phosphate–iron-oxide magma.  相似文献