FIGURE 11.1 Size classification of plankton based on Sieburth et al. (1978). Note the logarithmic scale on the size axis. Most estuarine zooplankton range.

Slides:



Advertisements
Similar presentations
Great Lakes Offshore Biological Desert and the Nearshore Slime Around the Tub David Rockwell Monitoring Indicators and Reporting Branch US EPA, Great Lakes.
Advertisements

The Changing Climate and Ecology in Narragansett Bay Candace Oviatt 10/12/12.
Abstract We quantified turbulent dissipation in the Raritan river using both conventional methods and a novel technique, the structure function method.
Spring 2015 course: 11:628:410, 3 credits Biophysical Interactions: from Barnacles to Jellyfish Tues-Thurs 2:15-3:35 Life at low Reynolds numbers Drag.
Zooplankton processes Puget Sound Oceanography Jan. 28, 2011.
The influence of movement dynamics on ecosystem structure: Suckers as ecosystem engineers Michael T. Booth, Alex S. Flecker, Nelson G. Hairston, Jr. Dept.
Foodweb support for the threatened Delta smelt: Microzooplankton dynamics in the low salinity zone of San Francisco Bay J.K. York 1, B. Costas 1, G. McManus.
Foodweb support for the threatened Delta smelt: Phytoplankton production within the low salinity zone Ulrika Lidström 1, Anne Slaughter 1, Risa Cohen 2,
An Investigation of the Effect of Turbidity on the Diel Vertical Migration of Zooplankton in the Chincoteague Bay, VA. James Bergenti, Department of Biology,
The Physical Modulation of Seasonal Hypoxia in Chesapeake Bay Malcolm Scully Outline: 1)Background and Motivation 2)Role of Physical Forcing 3)Simplified.
By: ESAI, ROBIN, and CHELSEA
FIGURE 5.1 Examples of submersed vascular plants that occur in estuarine systems: (a) Myriophyllum spicatum (photo: O. Pedersen), (b) Stuckenia pectinata.
IB 362 Lecture 12 Productivity and Food Webs.
Introduction Oithona similis is the most abundant copepod in the Gulf of Alaska, and is a dominant in many ecosystems from the poles to the sub-tropics.
Submerged aquatic vegetation (SAV) abundance and diversity in the tidal Potomac River and estuary By Nancy Rybicki, Jurate Landwehr, Edward Schenk, and.
FIGURE 7.1 (a) Fringe mangrove along Shark River slough dominated by Rhizophora mangle. (b) Interior mangrove forest in Puerto Rico dominated by Avicennia.
Electivity of M. leidyi Natural3x5x A. tonsa P. meadii T. turbinata Table 1.
FIGURE 3.1 Bacterial decomposition of organic matter in marine/estuarine sediments through a sequence of terminal electron acceptors (e.g., O2, NO3¯,
Vertical distribution of ontogenetically migrating copepods in the Western Subarctic Gyre T. Kobari 1, D. K. Steinberg 2, S. Wilson 2, K. Buesseler 3,
Effects of increased dissolved organic matter on zooplankton vertical distribution in a UV-transparent lake: Results from large-scale mesocosms Sandra.
The Effect of Bythotrephes longimanus on Copepod Populations in Lake Mendota Henry Schmit with Jake Walsh and Dr. Jake Vander Zanden UW Hasler Center for.
FIGURE 8.1 Benthic diatom assemblages viewed by scanning electron microscopy (SEM). (a) Epipsammic diatoms (Achnanthes and Navicula) in the cavity of a.
FIGURE 16.1 A simple food chain with three trophic levels illustrated using energy systems language (e.g., Odum, 967; Odum, 1971). Arrows indicate transfer.
FIGURE 2.1 The variation of mean sea level for the past 35,000 years based on data from the Atlantic continental shelf of the United States: the solid.
Narragansett Bay Environmental Monitoring Li-Ling Yang Roger Williams University.
Land-Ocean Interactions: Estuarine Circulation. Estuary: a semi-enclosed coastal body of water which has a free connection with the open sea and within.
FIGURE 6.1 Worldwide distribution of coastal marshes and mangrove swamps. Source: After Chapman (1960). ESTUARINE ECOLOGY, Second Edition. John W. Day.
FIGURE 15.1 Regression of ecosystem respiration and ecosystem gross primary production across many types of aquatic ecosystems. Gross production and respiration.
Introduction Egg production in copepod species may be the largest component of copepod production and is a parameter routinely monitored in ecosystem studies.
Section 3.2: Biomes *Biomes - a large group of ecosystems that share the same type of climax community. 2 types: 1) Aquatic Biomes 2) Terrestrial Biomes.
ETM: The Estuarine Turbidity Maximum
Acknowledgments Awesome research technicians: Carla Maria Delfino and Kayt Chambers Funding: This research is supported by the U.S. GLOBEC Northeast Pacific.
FIGURE 17.1 A simple nitrogen and water balance for ‘‘Dave the Sea Lion.’’ Both nitrogen and water flows are in units of grams per 40 days. See text for.
Date of download: 6/17/2016 Copyright © 2016 SPIE. All rights reserved. Location of the study area within the Bay of Biscay and oceanographic sampling.
Aquatic Biomes.
FIGURE 12.1 Diagram representing the various types of estuarine benthos. Source: From Day et al. (1989). ESTUARINE ECOLOGY, Second Edition. John W. Day.
Date of download: 6/27/2016 Copyright © 2016 SPIE. All rights reserved. Schematic showing the principle of calculating the TD between the contractile waves.
Vertical Distribution of Larvae off the Coast of Assateague Island, Virginia Carlee Kaisen Department of Biological Sciences, York College of Pennsylvania.
Climate Change Impacts on Estuarine Larval Fish Composition Jamie F. Caridad and Kenneth W. Able Institute of Marine and Coastal Sciences. Rutgers University.
Spring 2017 Biophysical Interactions: from Barnacles to Jellyfish 11:628:410, 3 credits Prerequisites: this class and Calculus II Low Reynolds numbers.
ESTUARINE ECOLOGY, Second Edition. John W. Day JR, Byron C. Crump, W
FIGURE Idealized scheme of carbon flow in a planktonic food web
FIGURE 13.1 The distribution of fish species richness in estuaries by habitat type and latitude. Source: From Houde (1989). ESTUARINE ECOLOGY, Second.
What are Zooplankton, and Why are they Important?
Lotic vs. Lentic Systems
Volume 7, Issue 2, Pages (February 2014)
Chenguang Zheng, Kevin Wood Bieri, Yi-Tse Hsiao, Laura Lee Colgin 
Volume 67, Issue 6, Pages (September 2010)
Smaller T cell zone FRC areas in aged spleens.
하구및 연안생태Coastal management
Feature- and Order-Based Timing Representations in the Frontal Cortex
Archerfish Actively Control the Hydrodynamics of Their Jets
Volume 111, Issue 2, Pages (July 2016)
CA3 Retrieves Coherent Representations from Degraded Input: Direct Evidence for CA3 Pattern Completion and Dentate Gyrus Pattern Separation  Joshua P.
Cortical Mechanisms of Smooth Eye Movements Revealed by Dynamic Covariations of Neural and Behavioral Responses  David Schoppik, Katherine I. Nagel, Stephen.
하구및 연안생태Coastal management
하구및 연안생태Coastal management
하구및 연안생태Coastal management
Stability of Cortical Responses and the Statistics of Natural Scenes
Volume 27, Issue 1, Pages (January 2017)
Secondary Productivity
Volume 27, Issue 11, Pages R478-R483 (June 2017)
The applications of the biohybrid structural color hydrogels in a heart-on-a-chip system. The applications of the biohybrid structural color hydrogels.
Volume 105, Issue 10, Pages (November 2013)
Volume 67, Issue 6, Pages (September 2010)
Volume 27, Issue 1, Pages (January 2017)
Volume 1, Issue 2, Pages (February 2012)
Self-Organization of Minimal Anaphase Spindle Midzone Bundles
Fig. 1 Environmental conditions and concentrations of floating plastic debris in the Arctic Ocean. Environmental conditions and concentrations of floating.
Relationships between species richness and temperature or latitude
Presentation transcript:

FIGURE 11.1 Size classification of plankton based on Sieburth et al. (1978). Note the logarithmic scale on the size axis. Most estuarine zooplankton range in size from ~2 μm (heterotrophic flagellates) to a maximum of ~1 m (large scyphomedusae). ESTUARINE ECOLOGY, Second Edition. John W. Day JR, Byron C. Crump, W. Michael Kemp, and Alejandro Yánez-Arancibia. Copyright © 2013 by Wiley-Blackwell. All rights reserved ~

FIGURE 11.2 Schematic representation of the dispersion of developmental stage of E. affinis in the middle part of the Seine estuary (Normandy Bridge) as a function of the mean tidal cycle, based on the results of this study. Width of arrows at the top of the figure represents the magnitude of the water velocity during a length of time represented by their length. The different water masses have been identified at the bottom of the figure as a function of the salinity range according to McLusky (1989): oligohaline zone [0.5–5], mesohaline [5–18] and polyhaline [18–25]. The population abundance increase during the ebb with low constant resuspension and hypothetical migration of adults (oval) and copepodids (square) that dominate the population from the poly- to mesohaline zone in surface and bottom water. In the oligohaline zone around the low slack, when current velocity is low, nauplii dominate the population. At the beginning of the flood when current velocity is maximal, the population is resuspended and adults and copepodids start to migrate (according to the hypothesis of Morgan et al., 1997 and Schmitt et al., unpublished data) to the bottom water while the current is decreasing. Source: Figure 9 from Devreker et al. (2008). ESTUARINE ECOLOGY, Second Edition. John W. Day JR, Byron C. Crump, W. Michael Kemp, and Alejandro Yánez-Arancibia. Copyright © 2013 by Wiley-Blackwell. All rights reserved ~

FIGURE 11.3 Salinity and abundance of E. affinis in the Elbe Estuary during longitudinal sampling (RD = mean river discharge of the 20 days before sampling). The map of the Elbe Estuary shows the distance downstream from the source (numbers = stream kilometers) and the black dot indicates the anchor station, located at stream-km 695. Source: Figure from Figures 1 and 9 of Peitsch et al. (2000). ESTUARINE ECOLOGY, Second Edition. John W. Day JR, Byron C. Crump, W. Michael Kemp, and Alejandro Yánez-Arancibia. Copyright © 2013 by Wiley-Blackwell. All rights reserved ~

FIGURE 11.4 An example of an estuarine planktonic food web from within the turbiditymaximum zone of the Gironde River estuary in July 2002 showing biomass and flux expressed as μgC/m 3 and μgC/m 3 / day, respectively. Estimation of such a food web requires careful measurement of the standing stocks within each pool and grazing rate experiments to quantify the magnitudes of fluxes among consumers. Source: From David et al. (2006). ESTUARINE ECOLOGY, Second Edition. John W. Day JR, Byron C. Crump, W. Michael Kemp, and Alejandro Yánez-Arancibia. Copyright © 2013 by Wiley-Blackwell. All rights reserved ~

FIGURE 11.5 (a) Historical patterns in phenology of A. tonsa and M. leidyi at central estuary stations in Narragansett Bay, USA. Linear regression indicates that A. tonsa phenology has not shown significant alteration (p = 0.195) during the period from 1950 to In contrast, the first appearance of M. leidyi has shifted significantly (p = 0.006) earlier in the year during the same period. (b) Decline in maximum seasonal concentrations of the copepod A. tonsa in the Narragansett Bay estuary during the period 2000–2003 (n = 4) relative to years between 1951 and 1983 (n = 7). All data collected from the same site; historical data (pre- 2000) assembled from a variety of sources. Error bars represent standard error of the mean and, although not shown, negative bars are symmetrical with positive bars. Average values for the two time periods are significantly different (Mann Whitney, p = 0.008). Source: From Costello et al. (2006). ESTUARINE ECOLOGY, Second Edition. John W. Day JR, Byron C. Crump, W. Michael Kemp, and Alejandro Yánez-Arancibia. Copyright © 2013 by Wiley-Blackwell. All rights reserved ~

FIGURE 11.6 Examples of phytoplankton and microzooplankton from Louisiana estuaries imaged with a color FlowCAM. Most particles were imaged at 10 or 20  magnification. ESTUARINE ECOLOGY, Second Edition. John W. Day JR, Byron C. Crump, W. Michael Kemp, and Alejandro Yánez-Arancibia. Copyright © 2013 by Wiley-Blackwell. All rights reserved ~

FIGURE 11.7 (a) An estuarine plankton sample from Louisiana digitized with a Zooscan. (b)Magnified vignettes of different organisms (A, chaetognath; B, crab megalopa; C, decapods; D, doliolid; E, calanoid copepod; F, fish larva). ESTUARINE ECOLOGY, Second Edition. John W. Day JR, Byron C. Crump, W. Michael Kemp, and Alejandro Yánez-Arancibia. Copyright © 2013 by Wiley-Blackwell. All rights reserved ~