The influence of environmental conditions on the seasonal variation of Microcystis cell density and microcystins concentration in San Francisco Estuary

Hydrobiologia ◽  
2007 ◽  
Vol 600 (1) ◽  
pp. 187-204 ◽  
Author(s):  
P. W. Lehman ◽  
G. Boyer ◽  
M. Satchwell ◽  
S. Waller
2021 ◽  
Vol 9 ◽  
Author(s):  
Rachel A. Fichman ◽  
Adi Khen ◽  
Malte Willmes ◽  
Jonathon Kuntz ◽  
Alexander R. Scott ◽  
...  

Estuaries are places where fresh water from rivers mixes with salty water from the ocean. Why does this matter? This mixing creates dynamic, ever-changing conditions that fishes must navigate in order to survive. Environmental conditions can change yearly, seasonally, daily, and even hourly. Fishes use many different strategies to adjust to this wild variation. Some are picky and only use certain habitats. Others use many different kinds of habitats and move between them at different times of the year. Adults and juveniles might even live away from each other in different parts of the estuary. In this article, we describe some of the clever strategies that fishes use to survive in estuaries. We also consider how scientists uncover these clever strategies and what each of us can do to help protect the fishes of the San Francisco Estuary and elsewhere.


2019 ◽  
Vol 41 (6) ◽  
pp. 939-954 ◽  
Author(s):  
Stephanie Owens ◽  
Toni R Ignoffo ◽  
Jared Frantzich ◽  
Anne Slaughter ◽  
Wim Kimmerer

ABSTRACT We measured growth rates of the copepod Pseudodiaptomus forbesi in relation to food, environmental conditions and hydrology in the northern San Francisco Estuary, California, USA. We conducted 38 copepod growth-rate experiments during summers 2015–2017 at four sites in a tidal, freshwater channel that had strong gradients in environmental conditions. Copepod growth rates were measured using the artificial cohort method with an image analysis technique, and seston attributes were measured to investigate the effects of food quantity and quality on copepod growth rates. Growth rates ranging from 0.03 to 0.47 day−1 (median 0.30 day−1) and growth rates, chlorophyll, turbidity and total lipids in the channel decreased with distance downstream. Growth rates had a saturating response to chlorophyll and were generally higher than rates previously measured in larger estuarine channels, presumably because of higher chlorophyll and temperature in our study area. Growth rate was positively associated with biovolume of cyanobacteria but not with that of other major phytoplankton groups, which is consistent with a recent finding of high feeding of P. forbesi on cyanobacteria. This adds to the small but growing literature suggesting that crustacean planktons are able to overcome the nutritional deficiencies of cyanobacteria to grow and reproduce.


Water ◽  
2021 ◽  
Vol 13 (15) ◽  
pp. 2139
Author(s):  
Paul H. Hutton ◽  
David M. Meko ◽  
Sujoy B. Roy

This work presents updated reconstructions of watershed runoff to San Francisco Estuary from tree-ring data to AD 903, coupled with models relating runoff to freshwater flow to the estuary and salinity intrusion. We characterize pre-development freshwater flow and salinity conditions in the estuary over the past millennium and compare this characterization with contemporary conditions to better understand the magnitude and seasonality of changes over this time. This work shows that the instrumented flow record spans the range of runoff patterns over the past millennium (averaged over 5, 10, 20 and 100 years), and thus serves as a reasonable basis for planning-level evaluations of historical hydrologic conditions in the estuary. Over annual timescales we show that, although median freshwater flow to the estuary has not changed significantly, it has been more variable over the past century compared to pre-development flow conditions. We further show that the contemporary period is generally associated with greater spring salinity intrusion and lesser summer–fall salinity intrusion relative to the pre-development period. Thus, salinity intrusion in summer and fall months was a common occurrence under pre-development conditions and has been moderated in the contemporary period due to the operations of upstream reservoirs, which were designed to hold winter and spring runoff for release in summer and fall. This work also confirms a dramatic decadal-scale hydrologic shift in the watershed from very wet to very dry conditions during the late 19th and early 20th centuries; while not unprecedented, these shifts have been seen only a few times in the past millennium. This shift resulted in an increase in salinity intrusion in the first three decades of the 20th century, as documented through early records. Population growth and extensive watershed modification during this period exacerbated this underlying hydrologic shift. Putting this shift in the context of other anthropogenic drivers is important in understanding the historical response of the estuary and in setting salinity targets for estuarine restoration. By characterizing the long-term behavior of San Francisco Estuary, this work supports decision-making in the State of California related to flow and salinity management for restoration of the estuarine ecosystem.


Author(s):  
Nicole M. Aha ◽  
Peter B. Moyle ◽  
Nann A. Fangue ◽  
Andrew L. Rypel ◽  
John R. Durand

AbstractLoss of estuarine and coastal habitats worldwide has reduced nursery habitat and function for diverse fishes, including juvenile Chinook salmon (Oncorhynchus tshawytscha). Underutilized off-channel habitats such as flooded rice fields and managed ponds present opportunities for improving rearing conditions and increasing habitat diversity along migratory corridors. While experiments in rice fields have shown enhanced growth rates of juvenile fishes, managed ponds are less studied. To evaluate the potential of these ponds as a nursery habitat, juvenile Chinook salmon (~ 2.8 g, 63 mm FL) were reared in cages in four contrasting locations within Suisun Marsh, a large wetland in the San Francisco Estuary. The locations included a natural tidal slough, a leveed tidal slough, and the inlet and outlet of a tidally muted managed pond established for waterfowl hunting. Fish growth rates differed significantly among locations, with the fastest growth occurring near the outlet in the managed pond. High zooplankton biomass at the managed pond outlet was the best correlate of salmon growth. Water temperatures in the managed pond were also cooler and less variable compared to sloughs, reducing thermal stress. The stress of low dissolved oxygen concentrations within the managed pond was likely mediated by high concentrations of zooplankton and favorable temperatures. Our findings suggest that muted tidal habitats in the San Francisco Estuary and elsewhere could be managed to promote growth and survival of juvenile salmon and other native fishes.


2002 ◽  
Vol 36 (22) ◽  
pp. 4741-4747 ◽  
Author(s):  
Pam Tsai ◽  
Rainer Hoenicke ◽  
Donald Yee ◽  
Holly A. Bamford ◽  
Joel E. Baker

2010 ◽  
Vol 55 (7) ◽  
pp. 1548-1559 ◽  
Author(s):  
KEMAL A. GER ◽  
SWEE J. TEH ◽  
DOLORES V. BAXA ◽  
SARAH LESMEISTER ◽  
CHARLES R. GOLDMAN

2001 ◽  
Vol 55 (1) ◽  
pp. 66-76 ◽  
Author(s):  
Roger Byrne ◽  
B. Lynn Ingram ◽  
Scott Starratt ◽  
Frances Malamud-Roam ◽  
Joshua N. Collins ◽  
...  

AbstractAnalysis of diatoms, pollen, and the carbon-isotopic composition of a sediment core from a brackish marsh in the northern part of the San Francisco Estuary has provided a paleosalinity record that covers the past 3000 yr. Changes in marsh composition and diatom frequencies are assumed to represent variations in freshwater inflow to the estuary. Three periods of relatively high salinity (low freshwater inflow) are indicated, 3000 to 2500 cal yr B.P., 1700 to 730 cal yr B.P., and ca. A.D. 1930 to the present. The most recent period of high salinity is primarily due to upstream storage and water diversion within the Sacramento–San Joaquin watershed, although drought may also have been a factor. The two earlier high-salinity periods are likely the result of reduced precipitation. Low salinity (high freshwater flow) is indicated for the period 750 cal yr B.P. to A.D. 1930.


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