Effects of proposed emergency withdrawals from the Hudson River by the City of New York on salt-front migration in the Hydson River estuary; legal testimony given before Judge Susan DuBois

1988 ◽  
Author(s):  
D.C. Hahl

<em>Abstract.</em>—The Hudson River Estuary (defined here as the Hudson River drainage and New York Harbor) is home to a large and diverse ichthyofauna. Estimates of species richness reflect both their geographic boundaries and time periods. The most complete estimate is for the Hudson River drainage north of the southern tip of Manhattan, where, as of 2005, 212 fish species have been recorded. This includes 11 new forms not reported in the most recently published tally (1990). We categorize the fishes of the Hudson River drainage as derived from 12 zoogeographic or anthropogenic sources (including species for which we make no judgment [<em>n </em>= 26]), the largest contributions from which include temperate marine strays (<em>n </em>= 65), introduced species (<em>n </em>= 28), and freshwater species that survived Pleistocene glaciations in Atlantic coastal refugia (<em>n </em>= 21). Additional species appear to have invaded from the Mississippi refugia, some naturally (<em>n </em>= 11) and some later, via canals (<em>n </em>= 11). Only ten diadromous fishes occur in the estuary, but many of these are, or have been, commercially and recreationally important (e.g., Atlantic sturgeon <em>Acipenser oxyrinchus</em>, American shad <em>Alosa sapidissima</em>, and striped bass <em>Morone saxatilis</em>). Extremely high seasonal temperature changes in the main-channel Hudson River foster a seasonally dynamic ichthyofauna with relatively few species occurring year round. However, the small number of resident estuarine fishes (<em>n </em>= 8) often occur in high abundances. Species richness peaks between June and September and reaches a minimum in winter. Long-term data indicate that although species richness has increased with the additions of new species, diversity is decreasing because of the decrease in population size of certain species, especially native cyprinids. The Hudson estuary hosts a population of one federally endangered species, shortnose sturgeon <em>Acipenser brevirostrum</em>, which is flourishing. Only one species, the anadromous rainbow smelt <em>Osmerus mordax </em>appears to have become extirpated in the Hudson Estuary.


Author(s):  
Quincy D. Newell

Jane Manning experienced the gift of tongues shortly after her conversion, an event she took as a confirmation of her decision to join the Mormons. The rest of the Manning family appears to have converted to Mormonism after her and, together with white converts from the area, they all left Connecticut for Nauvoo, Illinois, under the direction of LDS missionary Charles Wesley Wandell. The practice of racial segregation on boats and railways meant that for much, if not all, of their journey from Connecticut to New York City and then up the Hudson River and west on the Erie Canal, the black and white members of the group were separated from one another. At some point during the trip, the black members of the group were refused further passage, so the Mannings walked the rest of the way. Jane’s memory of this portion of the journey emphasized God’s providence. When they arrived in Nauvoo, they found a bustling city that was struggling to accommodate newly arrived converts, many of whom were poor and vulnerable to the diseases that plagued the city.


Estuaries ◽  
1992 ◽  
Vol 15 (2) ◽  
pp. 251
Author(s):  
Paul Geoghegan ◽  
Mark T. Mattson ◽  
James J. Reichle ◽  
Roger G. Keppel

Author(s):  
Melissa K. Cohen ◽  
Anne S. West ◽  
Elizabeth M. Cosper ◽  
Charles F. Wurster

Clones of Ditylum brightwellii and Thalassiosira nordenskioldii were isolated from New York coastal waters, and PCB-resistance in D. brightwellii was induced in the laboratory by exposure to increasing concentrations of PCB. Resistance could not be similarly induced in T. nordenskioldii, but was serendipitously discovered in unexposed cultures that had undergone sexual reproduction.Cells of the resistant strain were substantially larger than those of the sensitive strain in both species. Larger vacuole space seemed to account for this in D. brightwellii, but in T. nordenskioldii larger cells contained more carbon. Experiments with14C-PCB tracer indicated that PCB accumulation was less in resistant strains of both species. Neutral lipid content per cell, as determined using the fluorophore Nile Red, was similar for resistant and sensitive strains of both species. Sub-cellular examination of lipid droplets in D. brightwellii suggested that the PCB-resistant strain may be sequestering this lipophilic toxicant in a location removed from physiological activity. In T. nordenskioldii a decreased ratio of neutral lipidxarbon may reduce intracellular accumulation of PCB. These diatom species have developed PCB resistance in the highly PCB-polluted Hudson River estuary and, since they are the preferred food of dominant copepods, they may offer less PCB per unit ration to zooplankton grazers.


2018 ◽  
Author(s):  
Mark Y. Stoeckle ◽  
Mithun Das Mishu ◽  
Zachary Charlop-Powers

AbstractHere we describe GoFish, a streamlined environmental DNA (eDNA) presence/absence assay. The assay amplifies a 12S segment with broad-range vertebrate primers, followed by nested PCR with M13-tailed, species-specific primers. Sanger sequencing confirms positives detected by gel electrophoresis. We first obtained 12S sequences from 77 fish specimens representing 36 northwestern Atlantic taxa not well documented in GenBank. Using the newly obtained and published 12S records, we designed GoFish assays for 11 bony fish species common in the lower Hudson River estuary and tested seasonal abundance and habitat preference at two sites. Additional assays detected nine cartilaginous fish species and a marine mammal, bottlenose dolphin, in southern New York Bight. GoFish sensitivity was equivalent to Illumina MiSeq metabarcoding. Unlike quantitative PCR (qPCR), GoFish does not require tissues of target and related species for assay development and a basic thermal cycler is sufficient. Unlike Illumina metabarcoding, indexing and batching samples are unnecessary and advanced bioinformatics expertise is not needed. The assay can be carried out from water collection to result in three days. The main limitations so far are species with shared target sequences and inconsistent amplification of rarer eDNAs. We think this approach will be a useful addition to current eDNA methods when analyzing presence/absence of known species, when turnaround time is important, and in educational settings.


2012 ◽  
Vol 42 (3) ◽  
pp. 352-369 ◽  
Author(s):  
Nickitas Georgas

Abstract Seasonal episodes of significant tidal damping (reductions of tidal amplitudes as much as 50%) and tidal modulation were observed in the Hudson River estuary in the course of three consecutive winters from multiple tide gages. Through comparisons with United States Coast Guard ice reports, it was hypothesized that these events correspond with an increase in ice concentration and the development of a seasonal ice field within the upper 170 km of the tidal Hudson north of Peekskill, New York. Using stationary (tidal harmonic) and nonstationary (wavelet) analyses as well as numerical modeling, it is shown that under-ice friction is the primary cause of the observed modulations in tidal circulation (water levels and currents) throughout the 240-km-long estuary. Upstream of the ice field edge at Peekskill, depth-averaged tidal currents are greatly reduced under the ice cover through first-order damping, and vertical current profiles under the ice become parabolic. Tidal ranges increase near the edge of the ice field, and, south of that, on Manhattan’s western shores, currents increase because of tidal wave reflection. These amplified currents create stronger vertical mixing leading to a less stratified estuary and decreasing salt front intrusion. At the other end, near Troy, tidal flows become smaller relative to the river’s streamflow, leading to increased ebb predominance and ebb-directed flows down to the port of Albany. Also, the increased friction leads to a higher sea level setup there. During such episodes, astronomical tide–based and operational forecast model predictions that neglected ice are severely compromised.


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