Relevant bibliographies by topics / Marine ecology Marine ecology Upwelling (Oceanography) Upwelling (Oceanography)

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Academic literature on the topic 'Marine ecology Marine ecology Upwelling (Oceanography) Upwelling (Oceanography)'

Author: Grafiati
Published: 4 June 2021
Last updated: 7 February 2022

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Journal articles on the topic "Marine ecology Marine ecology Upwelling (Oceanography) Upwelling (Oceanography)"

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Dudas, Sarah E., Brian A. Grantham, Anthony R. Kirincich, Bruce A. Menge, Jane Lubchenco, and John A. Barth. "Current reversals as determinants of intertidal recruitment on the central Oregon coast." ICES Journal of Marine Science 66, no. 2 (December 2, 2008): 396–407. http://dx.doi.org/10.1093/icesjms/fsn179.

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Abstract Dudas, S. E., Grantham, B. A., Kirincich, A. R., Menge, B. A., Lubchenco, J., and Barth, J. A. 2009. Current reversals as determinants of intertidal recruitment on the central Oregon coast. – ICES Journal of Marine Science, 66: 396–407. The influence of current reversals on intertidal invertebrate recruitment was investigated using two seasons of nearshore physical and intertidal biological observations along the central Oregon coast, an intermittent upwelling system. In 1998, upwelling periods were punctuated by infrequent wind reversals and widespread increases in nearshore temperature, whereas 1999 was characterized by frequent, shorter wind reversals. In 1998, barnacle recruitment was best at the site experiencing more frequent reversals of the predominantly equatorward currents, higher poleward velocities, and coincident temperature increases. In 1999, barnacle recruitment peaked at the site with greater poleward current velocities, and maximum mussel recruitment at the site with consistent deep (10 m) onshore currents. Barnacle recruitment generally increased with onshore surface currents and temperature; mussel recruitment showed variable, weaker correlations. The data indicate that substantial decreases or complete reversals of upwelling-driven alongshore currents may be important for barnacle recruitment, but topographically driven differences in the response of currents to wind changes may generate local recruitment differences. This suggests that even relatively straight coastlines may have enhanced recruitment zones attributable to the variable local oceanography. Further, the interannual differences observed in current reversals and recruitment patterns highlight the potential importance of upwelling variation for onshore communities.
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Wiafe, George, Hawa B. Yaqub, Martin A. Mensah, and Christopher L. J. Frid. "Impact of climate change on long-term zooplankton biomass in the upwelling region of the Gulf of Guinea." ICES Journal of Marine Science 65, no. 3 (March 14, 2008): 318–24. http://dx.doi.org/10.1093/icesjms/fsn042.

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Abstract Wiafe, G., Yaqub, H. B., Mensah, M. A., and Frid, C. L. J. 2008. Impact of climate change on long-term zooplankton biomass in the upwelling region of the Gulf of Guinea. – ICES Journal of Marine Science, 65: 318–324. We investigated long-term changes in coastal zooplankton in the upwelling region in the Gulf of Guinea, 1969–1992, in relation to climatic and biotic factors. We considered the role of hydrographic and climatic factors, i.e. sea surface temperature (SST), salinity, sea level pressure, windfield, and Southern Oscillation Index (SOI), in the long-term variation of zooplankton in a multiple regression analysis, along with the abundance of Sardinella. Annual variation in zooplankton biomass was cyclical, with the annual peak occurring during the major upwelling season, July–September. Over the 24-year period, there was a downward trend in zooplankton biomass (equivalent to 6.33 ml per 1000 m3 per year). The decomposed trend in SST during the major upwelling revealed gradual warming of surface waters. This trend was believed to be the main influence on the abundance of the large copepod Calanoides carinatus (sensitive to temperatures above 23°C), which appears in the coastal waters only during the major upwelling season. The warming trend associated with global climate change could affect zooplankton community structure, especially during the major upwelling season. Global warming coupled with “top–down” (predation) control by Sardinella might be responsible for the long-term decline in zooplankton biomass in the upwelling region of the Gulf of Guinea.
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Scheel, D., and C. Johnson. "Sea-surface temperatures predict targeted visual surveys of octopus abundance." Marine and Freshwater Research 72, no. 9 (2021): 1321. http://dx.doi.org/10.1071/mf20318.

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In upwelling systems around the world, octopus abundance is forecast by marine productivity linked to upwelling strength, often indicated by sea-surface temperatures. Climate change may disrupt populations of marine animals that are linked to such temperature-dependent events. We analysed the relationship of the abundance of giant Pacific octopuses (Enteroctopus dofleini) to Gulf of Alaska and Washington State water temperatures. Abundance was measured in targeted visual surveys in Prince William Sound, Alaska, over the period 1995–2016 and from REEF.org diver surveys in Washington State from 2003 to 2019. Octopus counts from both survey programs had significant negative correlations with water temperatures over the previous 2.5–4 years. Water temperature accounted for from 0.41 to 0.71 of the variance (R2) in octopus abundance in eastern Gulf of Alaska waters located in ocean currents up-stream of the survey areas, and up to 0.81 of the variance in Washington State waters. These negative correlations provide a possible predictive index for octopus abundance as measured by targeted visual surveys. These methods may be useful tools in management of octopuses and indicate impacts of climate change on North Pacific coastal marine ecosystems.
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Noblezada, Mary Mar P., and Wilfredo L. Campos. "Spatial distribution of chaetognaths off the northern Bicol Shelf, Philippines (Pacific coast)." ICES Journal of Marine Science 65, no. 3 (March 17, 2008): 484–94. http://dx.doi.org/10.1093/icesjms/fsn027.

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Abstract Noblezada, M. M. P., and Campos, W. L. 2008. Spatial distribution of chaetognaths off the northern Bicol Shelf, Philippines (Pacific coast). – ICES Journal of Marine Science, 65: 484–494. The composition, abundance, and distribution of chaetognaths off the northern Bicol Shelf, Philippines (Pacific coast), from 31 stations along transects perpendicular to the coast were analysed. Samples were collected in April, 2001. In all, 26 species belonging to 14 genera were identified. Flaccisagitta enflata was the most abundant and frequently captured species at all stations, and constituted 41.9% of the total specimens. Most of the smallest diversity values were observed from areas affected by upwelling, although the greatest densities were observed at stations located within the upwelling zones. The occurrence of mesopelagic and bathypelagic species (Decipisagitta decipiens, Caecosagitta macrocephala, and Eukrohnia fowleri), in samples collected from upper water layers, could be explained by vertical transport caused by upwelling.
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Jackson, Thomas, Heather A. Bouman, Shubha Sathyendranath, and Emmanuel Devred. "Regional-scale changes in diatom distribution in the Humboldt upwelling system as revealed by remote sensing: implications for fisheries." ICES Journal of Marine Science 68, no. 4 (December 22, 2010): 729–36. http://dx.doi.org/10.1093/icesjms/fsq181.

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Abstract Jackson, T., Bouman, H. A., Sathyendranath, S., and Devred, E. 2011. Regional-scale changes in diatom distribution in the Humboldt upwelling system as revealed by remote sensing: implications for fisheries. – ICES Journal of Marine Science, 68: 729–736. A diatom-detection algorithm was parametrized for the Humboldt upwelling system using local cruise data that were first validated, then used to create monthly composites of diatom distribution from 0 to 40°S and 90 to 70°W for both normal and El Niño conditions. There was a 50% reduction in the areal extent of diatom-dominated waters during the peak of the 1997 El Niño. The extent of the coastward contraction in the diatom-dominated area varied along the South American coastline. These regional shifts in phyto- and zooplankton communities would have increased food stress on local anchovy (Engraulis ringens) populations and could have contributed to diminished larval survival and landings the following year. A region of strong upwelling over the wide Peruvian continental shelf around 15°S was the only area that maintained a strong diatom population throughout the El Niño; the area may require special protection from fishing pressure in years following an El Niño event.
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de Lecea, Ander M., Rachel Cooper, and Albertus J. Smit. "Identifying the drivers of the pelagic ecosystem of an oligotrophic bight (KwaZulu–Natal, South Africa) using stable isotopes (δ13C, δ15N) and C : N ratio analysis." Marine and Freshwater Research 67, no. 11 (2016): 1750. http://dx.doi.org/10.1071/mf15256.

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The international literature highlights the importance of understanding the role and fate of terrestrial organic matter (OM) in the marine system, yet little is known about this on the oligotrophic east coast of South Africa. Within the Bight, three important processes make OM biologically available: (1) a topographically induced upwelling cell (north), (2) a Cyclonic Eddy (south), and (3) riverine input. We hypothesise that: (i) these OM sources differ substantially in their isotope ratios, and (ii) zooplankton at the inshore region has an isotope signature linked to localised fluvial fluxes. Particulate OM samples were collected at five locations along the Bight and in three main estuaries during austral summer and winter seasons in 2010 and subjected to isotopic and mixing model analysis. Riverine input played an important role in this ecosystem inshore during the wet season. Only marine OM played a role as a biological driver offshore and at all sites during the dry season. Although there were indications that the upwelling cell did occur, it was not confirmed as active in either season. The current study provides valuable insights into the Bight's biological functioning and principle insights into the fate of terrestrial organic carbon on the east coast of southern Africa.
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Shannon, Lynne J., Marta Coll, Dawit Yemane, Didier Jouffre, Sergio Neira, Arnaud Bertrand, Erich Diaz, and Yunne-Jai Shin. "Comparing data-based indicators across upwelling and comparable systems for communicating ecosystem states and trends." ICES Journal of Marine Science 67, no. 4 (December 24, 2009): 807–32. http://dx.doi.org/10.1093/icesjms/fsp270.

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Abstract Shannon, L. J., Coll, M., Yemane, D., Jouffre, D., Neira, S., Bertrand, A., Diaz, E., and Shin, Y-J. 2010. Comparing data-based indicators across upwelling and comparable systems for communicating ecosystem states and trends. – ICES Journal of Marine Science, 67: 807–832. A suite of ecological indicators was selected for communicating, in a comparable way, how fishing affects the state of several upwelling ecosystems and others in which small pelagic fish play key ecological roles. Detailed background and understanding of system-specific processes and changes is needed for proper interpretation of results. In particular, environmental forcing is important in driving dynamics in upwelling systems; fishing impacts cannot be understood without understanding the corresponding dynamics of the environment. The Saharan Coastal (Morocco) and southern Benguela, both having experienced upsurges in low-trophic-level species, differed from other ecosystems when considering indicator trends. The ecosystem off Portugal emerged as showing reduced signs of fishing impacts in recent years, although the change may also be reflecting climate change favouring recruitment and abundance of demersal stocks. The indicator suite confirmed general understanding that the Mediterranean ecosystems have been notably degraded for several decades. Results and conclusions from this descriptive synthesis are compared with other comparisons of more complex, model-derived indicators. Even in upwelling and comparable systems, the simple data-based indicators are useful in synthesizing information on the status of an ecosystem, in particular on the ecosystem effects of fishing, to provide an ecological diagnosis at the ecosystem level, to be used in decision-making. Indicators of recent ecosystem state and trends over time are needed to assess the effects of fishing, but more indicators measuring biodiversity attributes and environmental change would complement the suite, providing fuller assessment of the status of upwelling and comparable ecosystems.
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Litz, Marisa N. C., Robert L. Emmett, Paul J. Bentley, Andrew M. Claiborne, and Caren Barceló. "Biotic and abiotic factors influencing forage fish and pelagic nekton community in the Columbia River plume (USA) throughout the upwelling season 1999–2009." ICES Journal of Marine Science 71, no. 1 (June 19, 2013): 5–18. http://dx.doi.org/10.1093/icesjms/fst082.

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Abstract Litz, M. N. C., Emmett, R. L., Bentley, P. J., Claiborne, A. M., and Barceló, C. Biotic and abiotic factors influencing forage fish and pelagic nekton community in the Columbia River plume (USA) throughout the upwelling season 1999–2009. – ICES Journal of Marine Science, 71: . Large river plumes modify coastal environments and can impact production across multiple trophic levels. From 1999 to 2009, the assemblages of forage fish, predator fish, and other pelagic nekton were monitored in coastal waters associated with the Columbia River plume. Surveys were conducted at night to target vertically migrating species, and community structure evaluated to better understand ecological interactions. Distinct inshore and offshore communities were identified during spring and summer that were correlated with ocean temperature, salinity, plume volume, and upwelling intensity. Resident euryhaline forage fish species, such as smelts, anchovy, herring, market squid, juvenile salmon, and spiny dogfish, showed a high affinity for inshore habitat and the lower salinity plume during spring. Highly migratory species, such as sardine, piscivorous hake, sharks, and mackerels, were associated with warmer, saltier waters offshore, during strong upwelling periods in summer. Overall, our study of pelagic nekton revealed that temporal dynamics in abundance and community composition were associated with seasonal abiotic phenomenon, but not interannual, large-scale oceanographic processes. Forage fish assemblages differed seasonally and spatially from the assemblages of major piscivorous predators. This finding suggests a potential role of the plume as refuge for forage fish from predation by piscivorous fish in the northern California Current.
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Boch, Charles A., Steven Y. Litvin, Fiorenza Micheli, Giulio De Leo, Emil A. Aalto, Christopher Lovera, C. Brock Woodson, Stephen Monismith, and James P. Barry. "Effects of current and future coastal upwelling conditions on the fertilization success of the red abalone (Haliotis rufescens)." ICES Journal of Marine Science 74, no. 4 (March 30, 2017): 1125–34. http://dx.doi.org/10.1093/icesjms/fsx017.

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Acidification, deoxygenation, and warming are escalating changes in coastal waters throughout the world ocean, with potentially severe consequences for marine life and ocean-based economies. To examine the influence of these oceanographic changes on a key biological process, we measured the effects of current and expected future conditions in the California Current Large Marine Ecosystem on the fertilization success of the red abalone (Haliotis rufescens). Laboratory experiments were used to assess abalone fertilization success during simultaneous exposure to various levels of seawater pH (gradient from 7.95 to 7.2), dissolved oxygen (DO) (∼60 and 180 µm.kg SW) and temperature (9, 13, and 18 °C). Fertilization success declined continuously with decreasing pH but dropped precipitously below a threshold near pH 7.55 in cool (9 °C—upwelling) to average (13 °C) seawater temperatures. Variation in DO had a negligible effect on fertilization. In contrast, warmer waters (18 °C) often associated with El Niño Southern Oscillation conditions in central California acted antagonistically with decreasing pH, largely reducing the strong negative influence below the pH threshold. Experimental approaches that examine the interactive effects of multiple environmental drivers and also strive to characterize the functional response of organisms along gradients in environmental change are becoming increasingly important in advancing our understanding of the real-world consequences of changing ocean conditions.
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Higgason, Kelley D., and Maria Brown. "Local solutions to manage the effects of global climate change on a marine ecosystem: a process guide for marine resource managers." ICES Journal of Marine Science 66, no. 7 (May 14, 2009): 1640–46. http://dx.doi.org/10.1093/icesjms/fsp133.

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Abstract Higgason, K. D., and Brown, M. 2009. Local solutions to manage the effects of global climate change on a marine ecosystem: a process guide for marine resource managers. – ICES Journal of Marine Science, 66: 1640–1646. The marine environment plays an important role in controlling the amount of CO2 that remains within the earth’s atmosphere, but it has not received as much attention as the terrestrial environment regarding climate-change effects, mitigation programmes, and action plans. Potential physical effects of climate change within the marine environment, including ocean acidification, changes in winds that drive upwelling and ocean circulation patterns, increasing global sea surface temperatures, and sea level rise, can result in dramatic changes within marine and coastal ecosystems. Often, marine resource managers feel overwhelmed by the magnitude of this issue and are therefore uncertain how to begin to take action. It may seem that they do not have the time, funding, or staff to take on a challenge as large as climate change, and fail to act as a result. Using NOAA’s Gulf of the Farallones National Marine Sanctuary as a case study, this paper outlines the need to act now and presents an easy-to-use process guide, providing managers options to incorporate effectively the influences of climate change into management strategies, as well as mitigate these influences through community outreach and a reduction in workplace emissions.
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Dissertations / Theses on the topic "Marine ecology Marine ecology Upwelling (Oceanography) Upwelling (Oceanography)"

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Chenillat, Fanny. "Variabilité de structure et de fonctionnement d'un écosystème de bord est : application à l'upwelling de Californie." Phd thesis, Université de Bretagne occidentale - Brest, 2011. http://tel.archives-ouvertes.fr/tel-00747012.

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Le système du Courant de Californie (CCS) est l'un des grands systèmes d'upwelling de bord est de la planète, caractérisés par un régime saisonnier de vents qui provoque des remontées d'eaux profondes (upwelling côtier), riches en nutriments, favorisant une forte activité biologique. À long terme, l'écosystème du CCS révèle des alternances de dominance de communautés marines, encore inexpliquées. L'objet de cette thèse est de comprendre l'effet de la variabilité pluriannuelle des vents sur la structure et le fonctionnement des premiers maillons trophiques de l'écosystème du CCS à partir d'études de processus reposant sur une approche numérique. Une première étude a permis de montrer que l'upwelling côtier et le transport côte-large ont une variabilité à basse fréquence fortement corrélée à celle de la tension de vent parallèle à la côte et au mode North Pacific Gyre Oscillation (NPGO), mis en évidence récemment et connu pour capturer une part de la variabilité à basse fréquence des vents d'upwelling et de la chlorophylle dans le CCS. Une étude fine de ces vents a permis de mettre en évidence une relation forte entre leur variabilité saisonnière et le mode NPGO, avec une modulation temporelle du déclenchement de la saison d'upwelling du CCS. L'impact d'un tel déphasage de l'upwelling sur un écosystème planctonique a pu ensuite être testé. À la côte, l'écosystème répond directement à un scénario d'upwelling précoce par une productivité plus forte. Au large, les incidences sur l'écosystème s'opèrent via les processus de transport côte-large. L'effet sur le zooplancton est plus prononcé que sur le phytoplancton et est susceptible d'affecter les niveaux trophiques supérieurs.
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Samuelsen, Annette O'Brien James J. "Modeling the effect of eddies and advection on the lower trophic ecosystem in the northeast tropical Pacific." Diss., 2005. http://etd.lib.fsu.edu/theses/available/etd-03242005-175448.

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Thesis (Ph. D.)--Florida State University, 2005.
Advisor: Dr. James J. O'Brien, Florida State University, College of Arts and Sciences, Dept. of Oceanography. Title and description from dissertation home page (viewed June 8, 2005). Document formatted into pages; contains xiii, 87 pages. Includes bibliographical references.
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Eerkes-Medrano, Dafne I. "The role of oxygen and other environmental variables on survivorship, abundance, and community structure of invertebrate meroplankton of Oregon nearshore coastal waters." Thesis, 2011. http://hdl.handle.net/1957/26610.

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The high productivity of Eastern Boundary Upwelling Ecosystems (EBUE), some of the most productive ecosystems in the globe, is attributed to the nutrient rich waters brought up through upwelling. Climate change scenarios for coastal upwelling systems, predict an intensification of coastal upwelling winds. Associated with intensification in upwelling are biogeochemical changes such as ocean hypoxia and ocean acidification. In recent years, the California Current System (CCS) has experienced the occurrence of nearshore hypoxia and the novel rise of anoxia. This has been attributed to changes in the intensity of upwelling wind stress. The effects of some of the more severe hypoxia and anoxia events in the CCS have been mass mortality of fish and benthic invertebrates. However, the impacts on zooplankton in this system are not known. Meroplankton, those organisms which have a planktonic stage for only part of their life cycle, are an important component of zooplankton communities. The larval stage of benthic invertebrates forms an important link between benthic adult communities and planktonic communities. Larvae serve to disperse individuals to new locations and to link populations. They are also food for fish and planktonic invertebrates. This important life stage can spend long periods in the plankton (from days to months) where environmental conditions can affect larval health, subsequent settlement and recruitment success, and juvenile health. This research assesses the role of hypoxia and larval survivorship, and the relationship between individual abundance and community structure of larvae to environmental factors in the field. In laboratory experiments (Chapter 2), a suite of 10 rocky intertidal invertebrate species from four phyla were exposed to low oxygen conditions representative of the nearshore environment of the Oregon coast. Results revealed a wide range in tolerances from species with little tolerance (e.g. the shore crab Hemigrapsus oregonensis) to species with high tolerance (e.g. the California mussel Mytilus californianus). The differential responses across larvae to chronic hypoxia and anoxia potentially could affect their recruitment success and consequently, the structure and species composition of intertidal communities. Field studies (Chapter 3 & 4) explore the relationship between environmental variables and larval abundance and community structure. Chapter 3 focuses on broad taxonomic groups, while Chapter 4 focuses on larval decapods in particular. Fine focus was devoted to decapod larvae, due to laboratory findings of heightened sensitivity to hypoxia of decapod crabs. A finding that is also supported in the literature. The goal of field studies was to identify the environmental parameters that structure meroplankton and larval decapod communities and identify which of these parameters play a significant role in influencing larval abundance. A number of environmental variables contributed to meroplankton assemblage structure and larval decapod assemblage structure. These included distance from shore, depth, date, upwelling intensity, dissolved oxygen, and cumulative wind stress. Some of these factors occurred frequently in larval abundance models. In Chapter 3, individual abundance across broad taxonomic groups was most commonly explained by upwelling intensity while in Chapter 4, individual abundance of different decapod species was explained by cumulative wind stress, which is a proxy for upwelling intensity. The prominent role of upwelling related factors in explaining individual abundance is important considering climate change projections of an increased intensification of upwelling winds in EBUE.
Graduation date: 2012
Access restricted to the OSU Community at author's request from Jan. 6, 2012 - Jan. 6, 2013
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Books on the topic "Marine ecology Marine ecology Upwelling (Oceanography) Upwelling (Oceanography)"

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Workshop on Models for Yield Prediction in the Peruvian Ecosystem (1987 Callao, Perú). peru Peruvian upwelling ecosystem: Dynamics and interactions. Callao, Perú: Instituto del Mar del Perú, 1989.

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Bùi, Hồng Long. Hiện tượng nước trồi trong vùng biển Việt Nam. Hà Nội: Nhà xuất bản Khoa học tự nhiên và công nghệ, 2009.

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M, Hovland, ed. Seabed fluid flow: The impact of geology, biology and the marine environment. Cambridge: Cambridge University Press, 2007.

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P, Summerhayes C., Prell W. L, and Emeis K. C, eds. Upwelling systems: Evolution since the early Miocene. London: Geological Society, 1992.

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Payne, A. I. L. 1946-, Sea Fisheries Research Institute (South Africa), and International Symposium on Population and Community Ecology in the Benguela Upwelling Region and Comparable Frontal Systems (1986 : Cape Town, South Africa), eds. The Benguela and comparable ecosystems. Cape Town, South Africa: Sea Fisheries Research Institute, Dept. of Environment Affairs, 1987.

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The Benguela and comparable ecosystems. Cape Town: Republic of South Africa, Dept. of Environment Affairs, Sea Fisheries Research Institute, 1987.

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Upwelling Systems: Evolution Since the Early Miocene (Geological Society Special Publication). Geological Society Publishing House, 1992.

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Hovland, Martin, and Alan Judd. Seabed Fluid Flow: The Impact on Geology, Biology and the Marine Environment. Cambridge University Press, 2007.

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