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PLOS ONE | 2011

Man and the Last Great Wilderness: Human Impact on the Deep Sea

Eva Ramírez-Llodra; Paul A. Tyler; Maria Baker; Odd Aksel Bergstad; Malcolm R. Clark; Elva Escobar; Lisa A. Levin; Lenaick Menot; Ashley A. Rowden; Craig R. Smith; Cindy Lee Van Dover

The deep sea, the largest ecosystem on Earth and one of the least studied, harbours high biodiversity and provides a wealth of resources. Although humans have used the oceans for millennia, technological developments now allow exploitation of fisheries resources, hydrocarbons and minerals below 2000 m depth. The remoteness of the deep seafloor has promoted the disposal of residues and litter. Ocean acidification and climate change now bring a new dimension of global effects. Thus the challenges facing the deep sea are large and accelerating, providing a new imperative for the science community, industry and national and international organizations to work together to develop successful exploitation management and conservation of the deep-sea ecosystem. This paper provides scientific expert judgement and a semi-quantitative analysis of past, present and future impacts of human-related activities on global deep-sea habitats within three categories: disposal, exploitation and climate change. The analysis is the result of a Census of Marine Life – SYNDEEP workshop (September 2008). A detailed review of known impacts and their effects is provided. The analysis shows how, in recent decades, the most significant anthropogenic activities that affect the deep sea have evolved from mainly disposal (past) to exploitation (present). We predict that from now and into the future, increases in atmospheric CO2 and facets and consequences of climate change will have the most impact on deep-sea habitats and their fauna. Synergies between different anthropogenic pressures and associated effects are discussed, indicating that most synergies are related to increased atmospheric CO2 and climate change effects. We identify deep-sea ecosystems we believe are at higher risk from human impacts in the near future: benthic communities on sedimentary upper slopes, cold-water corals, canyon benthic communities and seamount pelagic and benthic communities. We finalise this review with a short discussion on protection and management methods.


The Biological Bulletin | 1995

Role of Digestive Gland in the Energetic Metabolism of Penaeus setiferus

Carlos Rosas; Andrea Bolongaro-Crevenna; Adolfo Sánchez; Gabriela Gaxiola; Luis A. Soto; Elva Escobar

We determined the role of the digestive gland in the respiratory metabolism of Penaeus setiferus adult males as a step toward proposing a feeding schedule based on the cycle of activity in the digestive gland. We measured pre- and postprandial values for oxygen consumption rate and hemolymph glucose concentrations in live animals, and oxygen consumption rate and glycogen concentration in excised digestive gland. After the animals were fed, which enhanced general metabolic activity, these indices changed. There was a high correlation between the oxygen consumption rate of the animal and the glucose concentration in the hemolymph, and between the oxygen consumption rate by the digestive gland and the glycogen concentration in the digestive gland, all in relation to time after feeding. Correlations support the hypothesis that the energy demand depends upon the metabolic substrate concentration. In this theory, glucose sustains muscle activity (during ingestion of food) and glycogen is the product of the digestive gland during food assimilation. Our observations of metabolic dynamics during the feeding period allowed us to examine the feeding process. The metabolic activity of the digestive gland was highest 6 h after feeding. This could mean that assimilation, having started 2 h after food intake, peaked 6 h after feeding. Eight hours after feeding, the oxygen consumption rate of the digestive gland decreased and fell to values similar to those recorded for animals subjected to 72 h of fasting.


Comparative Biochemistry and Physiology Part A: Physiology | 1992

DAILY VARIATIONS OF OXYGEN-CONSUMPTION AND GLUCOSE HEMOLYMPH LEVEL RELATED TO MORPHOPHYSIOLOGICAL AND ECOLOGICAL ADAPTATIONS OF CRUSTACEA

Carlos Rosas; Adolfo Sánchez; Elva Escobar; Luis A. Soto; Andrea Bolongaro-Crevenna

Abstract 1. 1. Daily variations of oxygen consumption and glucose hemolymph level of seven crustacean species from the continental shelf of the NW Gulf of Mexico were related to the morphophysiological (exoskeleton thickness) and ecological (activity rhythms) adaptations. 2. 2. Metabolic rate and the hemolymph glucose changed with the daily activity patterns observed in the shrimps (Penaeus aztecus: nocturnal; Sicyonia brevirostris: diurnal), the portunid crabs (Callinectes similis, Portunus spinicarpus and P. gibbesii: nocturnal) and the calappids (Calappa sulcata: diurnal; Hepatus ephelyticus: non-selective activity pattern). 3. 3. Rates of oxygen consumption versus glucose concentration were greater in shrimps than in portunids and calappids, and were related to exoskeleton thickness and activity rate. The glucose concentration was considered as the main energy source for the crustacean muscle. 4. 4. Proportion of glucose concentration in relation to oxygen consumption (100%) varies among species, with lowest values for shrimps (55%), against the values recorded in portunid (126%) and calappid crabs (235–423%), indicating the amount of glucose required for chitin synthesis of species with different morphophysiological designs and activity patterns.


Hydrobiologia | 2002

Phytoplankton of cenotes and anchialine caves along a distance gradient from the northeastern coast of Quintana Roo, Yucatan Peninsula

Malinali Sánchez; Javier Alcocer; Elva Escobar; Alfonso Lugo

This work details the taxonomic composition of suspended algae (phytoplankton and tycoplankton) communities in five cenotes (sinkholes) and two anchialine caves in northeastern Quintana Roo, Mexico. The sample set of cenotes are Casa, Nohoch Nah Chich, Maya Blue, Cristal, and Carwash, as well as the two associated caves leading from the cenotes of Maya Blue and Cristal. The site distribution represents a distance gradient with respect to the coastline with which we observe the effects of tidal movement and the mixing of waters (e.g. saline water and freshwater) on the composition of the suspended algae communities. Two sample sets were taken, one at the end of the dry season (March–April 1995) and the second at the end of the rainy season (September–October 1995) with the goal of comparing the contrasting climatic conditions of the region. A total of 79 species were identified, of which, diatoms were the most important with respect to species richness with a total of 75% of species. The floristic composition is very similar between the freshwater cenotes. The distance of a cenote site with respect to the coastline was a determining factor in the species composition. Casa Cenote is the most distinct of the sample set for the presence of marine species due to its proximity to the coastline. The tides are a large determining factor of the floristic composition of Casa Cenote with 24% all species identified in this study found exclusively in this system. The anchialine system species are transported from the cenotes and the adjacent cave systems. The largest percentage or species (95%) are freshwater, and only 5% of the total number of identified species are of marine origin. It is recognized that the most distant cenotes from the coast, Carwash and Cristal, as well as Maya Blue and Nohoch Nah Chich, are the most similar, despite being part of different cave systems. In these inland systems the marine species decreased drastically (2.4% in Nohoch Nah Chich and no marine species in the remaining cenotes). Marine species are found at the halocline of the caves.


International Journal of Salt Lake Research | 1998

Littoral benthos of the saline crater lakes of the basin of Oriental, Mexico

Javier Alcocer; Elva Escobar; Alfonso Lugo; Laura Peralta

Two saline crater lakes in the basin of Oriental, Puebla-Tlaxcala-Veracruz, were investigated for littoral benthic macroinvertebrates. Fifty taxa were identified with the oligochaetes, amphipods, chironomids and leeches the dominant organisms. These four taxa made up to 99 per cent in both number and biomass. Limnodrilus hoffmeisteri, Hyalella azteca, Tanypus (Apelopia) sp. and Stictochironomus sp. were the most abundant organisms. Unlike other saline lakes which have a littoral benthos dominated by chironomids, Alchichica and Atexcac were dominated by oligochaetes (70–73 per cent). The gastropod, Physa sp., was found up to a salinity of 8 g L-1; in other studies, it has been found in lower salinities. L. hoffmeisteri is also a typical inhabitant of freshwater lakes, particularly of deep waters. It was dominant in the shallow, saline waters of the two lakes studied. Salinity did not affect species richness. Alchichica, the most saline of the six crater lakes of Puebla (salinity, 7.4 g L-1), had 30 per cent more species than the freshwater lakes, and double the species number of Atexcac. It seems the main factor controlling species richness and the density and biomass of organisms in Alchichica and Atexcac is the presence of aquatic vegetation. It does this by increasing habitat heterogeneity and providing food and protection against predators.


International Journal of Salt Lake Research | 1996

The macrobenthic fauna of a former perennial and now episodically filled mexican saline lake

Javier Alcocer; Alfonso Lugo; Elva Escobar; Malinali Sánchez

Totolcingo (El Carmen), a large and now episodically filled playa lake in the east-ernmost portion of the Mexican Plateau, filled with water in 1993. Water persisted for just one month (May). Alkaline (pH ≈ 10), saline (K25 up to 30,000μS/cm) waters, dominated by NaHCO3 and Na2CO3, characterized the lake. The fauna was depauperate. The components of the fauna wereEphydra (Hydropyrus)hians Say (ephydrid),Limnodrilus hoffmeisteri Claparede (tubificid), andBerosus sp. (Coleoptera). The species in the lake were widely dispersed and typical inhabitants of saline lakes. Possible reasons for the depauperate fauna include (a) overall physical and chemical conditions, (b) unpredictable hydrology, and (c) the short (one month) inundation period prevented colonization.


Comparative Biochemistry and Physiology Part A: Physiology | 1991

Skeleton weight-free oxygen consumption related to adaptations to environment and habits of six crustacean species

Adolfo Sánchez; Carlos Rosas; Elva Escobar; Luis A Soro

Abstract 1. 1. Oxygen consumption in six crustacean species from the continental shelf of the NW Gulf of Mexico was related to the ash free weight per dry weight (afdw) gram of the tissue excluding the exoskeleton, suggesting a close relationship to their life strategies. 2. 2. Dry weight exoskeleton proportion varied among species, with highest values recorded in callapid brachyuran crab species (46.8–52.5%) against the values recorded in portunid crab (45.8–48%) and the shrimp species (26.7–35.7%). 3. 3. Oxygen consumption was related to afdw in each species according to the expression y = ax b , with b values ranging from 0.68 to 2.92. 4. 4. Rates of oxygen consumption per afdw/dw were larger in shrimps than in portunids and callapids, and was related to the morphophysiology and lifestyle of six species described; the former as the morphological design of the exoskeleton versus the muscle content in the species and the latter as the activity rate in the environment. 5. 5. The oxygen extraction efficiency, calculated from oxygen consumption, was higher in the eurytopic species Penaeus aztecus and Callinecies similis than in species restricted to the marine environment, hence considered as a response to environmental fluctuations.


Hydrobiologia | 2002

Oligochaetes from six tropical crater lakes in Central Mexico: species composition, density and biomass

Laura Peralta; Elva Escobar; Javier Alcocer; Alfonso Lugo

The assemblage of littoral oligochaetes in six crater lakes in Central Mexico, was studied throughout a yearly cycle. To establish species composition, richness, density and biomass, 14 localities were sampled in the lakes. A total of eight species belonging to the families Naididae (five species), Tubificidae (two species), and Enchytraeidae (one species) were found. The dominant species, Limnodrilus hoffmeisteri, contributed with up to 99% in both abundance and biomass. Sediment organic matter is the most important environmental variable explaining the differences in density and biomass. Seasonal (dry and rainy seasons) changes were not significant for density and biomass. Higher density and lower biomass values characterized these lakes in contrast to other tropical and subtropical lakes worldwide. The small size of the dominant species L. hoffmeisteri was recorded in all lakes and explained the low biomass recorded in the area of study. The correlation between L. hoffmeisteri and four other species (Dero (Dero) nivea, D. (D.) digitata, Nais variabilis and Tubifex tubifex) was negative. The naidid species were positively correlated (>0.5) to each other.


Hydrobiologia | 1998

Isabela Crater-Lake: a Mexican insular saline lake

Javier Alcocer; Alfonso Lugo; M. Del R. Sanchez; Elva Escobar

The Isabela Crater-Lake is a bright-green, hypersaline lake (68–112.5 mS cm-1) on Isabela Island off the Pacific coast of Nayarit, Mexico. Some salient features were documented in November 1993. It appears meromictic, with three well-defined strata separated by sharp pycnoclines. Surface water was warm (32 °C) reaching a subsurface (0.5–1 m) maximum temperature (33 °C), declining gradually to 26.7 °C at maximum depth (17.5 m). Dissolved oxygen was near saturation at the surface, attained 145 percent saturation at 0.5 m, but was completely absent by 2.5 m. Eh was maximum at the surface (123 mV), declining to a minimum at 3 m (–261 mV), and was about –240 mV from 3.5 m to the bottom. The pH varied from 9.3 in surface waters to slightly acid (6.4) in deep anoxic layers. Atypically, NO3 was more abundant than NH4 in both aerobic and anaerobic strata. PO4 and SiO2 concentrations were extremely high. The planktonic microbial community was formed by four groups: bacteria (photosynthetic sulfur bacteria and heterotrophic bacteria), phytoflagellates (mainly cryptomonads), heterotrophic nanoflagellates ( Spumella spp., Bodo spp.) and ciliates (Hypotricha and Oligotricha). Bacteria occurred throughout the water column, but other biota were restricted to surface waters.


International Journal of Salt Lake Research | 1999

Benthos of a prerennially-astatic, saline, soda lake in Mexico

Javier Alcocer; Elva Escobar; Alfonso Lugo; Luis A. Oseguera

The effects of multiple stressors on the benthic macroinvertebrate community were monitored in Tecuitlapa Norte, a shallow, perennially-astatic, warm, mesosaline, sodaalkaline lake in Mexico. Physico-chemical and biological variables were determined monthly for one year. Tecuitlapa Norte displayed a clear seasonal environmental pattern (dry and rainy seasons). The benthic macroinvertebrate community consisted of five species:Culicoides occidentalis sonorensis Jorgensen,Ephydra hians Say,Stratiomys sp.,Eristalis sp., andLimnophora sp. of which the first two were dominant and the rest scarce.C. occidentalis was the most important species numerically (76 percent of the total), whileE. hians dominated the biomass (73 percent of the total). Primarily salinity and secondarily pH appear to be the most important environmental factors controlling dominance of benthic organisms in Tecuitlapa Norte. Seasonal abundance dynamics of the dominant organisms was associated with phases in their reproductive cycles: environmentally-triggered (i.e., temperature rise, water-level descent) pupation and emergence periods. We concluded that whereas physical and chemical factors (i.e., salinity, pH) exerted the primary control on benthic macroinvertebrate community composition in Tecuitlapa Norte, another assembly of variables (e.g., water-level, temperature) influenced species distribution and abundance.

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Javier Alcocer

National Autonomous University of Mexico

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Alfonso Lugo

National Autonomous University of Mexico

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Luis A. Oseguera

National Autonomous University of Mexico

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Lisa A. Levin

Scripps Institution of Oceanography

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Luis A. Soto

National Autonomous University of Mexico

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Craig R. Smith

University of Hawaii at Manoa

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Kristina M. Gjerde

International Union for Conservation of Nature and Natural Resources

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Adolfo Sánchez

National Autonomous University of Mexico

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Carlos Rosas

National Autonomous University of Mexico

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Daniel O.B. Jones

National Oceanography Centre

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