1
Department of Biology, Bates College, Lewiston ME 04240, United States
2
Department of Coastal and Marine Systems Science, Coastal Carolina University, United States
Corresponding author details:
Larissa M. Williams
Bates College Department of Biology
44 Campus Avenue
Lewiston ME 04240,United States
Copyright:
© 2020 Williams LM, et al.
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The polychaete bloodworm, Glycera dibranchiata Ehlers, 1868 is an important source of bait for saltwater fishing and is harvested from mud flats in the Gulf of Maine. Little is known about the life history of G. dibranchiata and management of the fishery is minimal. The goal of our study was to determine the population genetics of several Maine populations in order to inform management. We sequenced the neutral mitochondrial cytochrome c oxidase I (COI) marker in seven populations along the coast of Maine. A total of 486 nucleotides were sequenced in each individual, yielding 13 haplotypes, with 94% of them haploytpe 1. There was very little to no genetic differentiation among populations in the south (\[F_{ST}\] of less than 0.05), and there was only moderate differentiation between one of the most northern sites and the most southern site (\[F_{ST}\] between 0.05 and 0.15). This lack of genetic differentiation indicates the populations are genetically linked via gamete dispersal. Consequently, the bloodworm fishery in the State of Maine can be managed at the scale of the Gulf of Maine(Graphical abstract).
Bloodworm, Glycera, gene flow, cytochrome c oxidase I (COI), Gulf of Maine
Polychaetes are harvested recreationally and commercially for fish bait worldwide [1]. Management of these fisheries is difficult because there is limited data on life histories of the target species and harvesting practices and the harvesters are notoriously difficult 60 to engage [2]. The bloodworm Glycera dibranchiata Ehlers, 1868 is one of the five most valuable (retail price per kg) marine species globally and one of the most popular polychaete species used as saltwater bait on the East Coast of North America [2].
Harvested from mud flats in Maine since the 1930s [3], bloodworms support a sustainable and large industry in the state with an average landed value of $6.3 million over the past 5 years [4]. Yearly fishing effort in Maine, as calculated by dividing the number of harvested pounds by the number of licenses 68 issued, has been relatively consistent [4] (Table 1), but there has been significant 69 variability in the catch from a recent high in 2002 of 682,994 lbs. to an unofficial low in 2018 of 376,294 lbs. Inter-annual variability in catch could be a consequence of market demand [5], but might also be the result of overharvesting in some areas. There is concern that overharvesting could become widespread if the fishery is not properly managed. Furthermore, climate change, which has led to the Gulf of Maine warming faster than 99% of the rest of the ocean [6], may further endanger this species and has contributed to its overall vulnerability rank as “very high” by NOAA (NMFS 2015).
G. dibranchiata is a semelparous, carnivorous, marine polychaete
[7,8]. We know very little about the development of G. dibranchiata,
but it is thought that most adults mature, spawn, and die after 3
years, though some have been shown to reach 5 years of age [7,9].
Spawning in the northeast, where up to 10 million eggs per female
are released, mostly occurs in shallow water during late afternoon
high tides and only lasts a few daysaround mid-May [7,9]. The
duration of the larval stage has never been studied in the field. In the
lab, fertilized eggs develop into a trochophore larva between 14-20
hours post fertilization and survive up to 17 days but not beyond the
trochophore stage [7,10]. The congeneric Glycera capitate Ørsted
develops a benthic form in about 21 days [11]. Glycera spp. larvae
are rarely sampled from the plankton [12] so we assume that their
time in the plankton is short. If they have a short plankton phase and
limited dispersal as adults, then populations should be relatively
genetically isolated.
Our paucity of knowledge on the reproductive biology, harvest practices, and genetics of G. dibranchiata in Maine means we do not have sufficient information to manage the fishery [13,14]. The results of starch gel electrophoresis of four G. dibranchiata enzymes were used to hypothesize that a genetic bottleneck had occurred in one Maine population (Cod Cove) due to overharvesting [15]. Following up, Bristow and Vadas [16] used starch gel electrophoresis of 10 enzymes to assess the genetic variation of G. dibranchiata from eight intertidal sites in the Gulf of Maine and the Atlantic coast of Nova Scotia. They found intra- and inter-estuarine genetic differentiation indicating low gene flow [16],although much of this variation was driven by Cod Cove, the population that had recently collapsed. These studies were important first steps in understanding the population genetics of bloodworms in Maine. Starch gel electrophoresis of proteins, however, is not as sensitive as DNA sequencing and uses enzymes that may be non-neutral and could be influenced by natural selection.
Therefore, we used a more accurate, modern, and neutral
approach to assess populationstructure and gene flow among
populations along t 106 he coast of Maine. We used the cytochrome c
oxidase I gene, a gene that has been used as a neutral genetic marker
[17] to help measure the maternal gene flow among bloodworm
populations in order to assess the genetic linkage of populations in
Maine.
Site locations
We selected seven mud flats across the Gulf of Maine and collected 30 worms per site from January through June of 2017 and in June of 2018. Professional diggers harvested worms from the middle to low intertidal and held them in buckets until worms were frozen upon return to the worm dealer. From south to north, the sites were: (A) Upper Rich Cove--URC (43° 49’ 43.85’’ N 69° 54’ 969’’ W), (B) Brookings Bay--BB (43° 55’ 33.0384’’ N69° 44’ 26.4696’’ W), (C) Cod Cove--CC (44° 0’ 3.906’’ N69° 37’ 56.874’’ W), (D) Round Pond--RP (43° 56’ 52.296’’ N69° 27’ 40.1724’’ W), Raccoon Cove--RC (44° 28’ 1.776’’ N68° 17’ 2.1624’’ W), Long Ledge--LL (44° 31’ 10.6212’’ N 68° 9’ 52.9092’’ W), and Jonesport--JP (44° 31’ 51.762’’ N67° 36’ 10.836’’ W) (Figure 1). Specimens were transported frozen to the laboratory and preserved at -20°C until processing.
Genomic DNA isolation, extraction, and amplification
DNA isolation was performed using the Qiagen DNeasy Blood and Tissue Kit. DNA was then quantified using a NanoDrop Spectrophotometer and a polymerase chain reaction (PCR) was performed on the cytochrome c oxidase I gene using universal primers [18]. PCR reactions were carried using RedTaq (ThermoFisher) and the thermocycling profile consisted of 30 cycles of 2 min at 94°C, 15 s at 94°C, 30 sat 53°C, 1 min at 72°C and of a final extension f 129 or 7 minutes at 72°C. PCR products were electrophoresed on a 1.5% gel and visualized.
Purification of PCR products and sequencing
The successfully amplified products were purified with the Qiagen QIAquick PCR
Purification Kit: The purified PCR products were Sanger sequenced in both directions using an Applied Biosystems 3130xl DNA sequencer at the Mount Desert Island Biological Laboratory.
Data analysis
Consensus sequences for each individual were produced from
the forward and reverse sequences using ClustalX 2.1 [19]. Using
DnaSP v.5 [20], genetic diversity was analyzed within and between
populations by determining haplotype diversity (Hd), nucleotide
diversity (\[P_{i}\]), and pairwise distances between populations (\[F_{ST}\]).
We sequenced 486 nucleotides in each individual, yielding 13 haplotypes (Figure 1). Of the 210 individuals analyzed, 197 (93.8%) had the same haplotype (“haplotype 1”). There were 12 other haplotypes found, but all except haplotype 12 were represented by a single individual in a single population. Haplotype 12 was shared by one individual in Long Ledge and one in Jonesport. Upper Rich Cove, Cod Cove, and Round Pond harbored only haplotype 1 and the most diversity existed in Long Ledge that had 10 haplotypes yet this site only had a small nucleotide diversity of 0.00246.
Figure 1: Cytochrome c oxidase subunit I haplotype frequencies for Glycera dibranchiate (n=30) at sampling locations in the Gulf of Maine. Pie charts indicate the proportion of haplotypes present at each site.
Genetic differentiation between two populations [21] which is
measured by the fixation index, \[F_{ST}\], was calculated. There was very
little to no genetic differentiation between populations in the south
(determined by an FST of less than 0.05; [22], and there was only
moderate differentiation (determined by an \[F_{ST}\]between 155 0.05
and 0.15) between Long Ledge and the most southern site, Upper
Rich Cove (Table 2).
As a vital bait worm used in several fisheries in Maine and exported worldwide [13], and a species that is vulnerable to climate change NOAA [23], it is important to understand how G. dibranchiata populations are genetically connected. In their 1991 paper on G. dibranchiata genetics, Bristow andVadas [16] found moderate levels of genetic variation within populations, moderate levels of differentiation among populations, and thus low levels of genetic exchange among populations. The population that was contributing most to the variation they observed was Cod Cove, a population that had no COI genetic diversity in our study (Figure 1). At our neutral, maternally-derived, marker we show that there is limited population differentiation and low levels of variation within populations indicating gene flow along the section of Maine coast we sampled.
Long Ledge harbored the greatest genetic diversity with 10
haplotypes sequenced compared to 3 at the next most diverse site,
Jones Port (Figure 1). Diggers harvest from many different intertidal
mudflats and return to worm dealers to sort their catch, culling out
‘shorts’, worms that are below market size, in the process. Some
diggers make an effort to return these shorts to a convenient site,
which is rarely the site where they wereharvested. Diggers have been
dumping their ‘shorts’ a 174 t Long Ledge for at least two generations
(Harrington pers. comm.). Therefore, the high genetic diversity at
this site is, easily explained and is the first evidence that returned
worms survive at least long enough to be harvested by our diggers.
The two most likely explanations for the discrepancy between our
study and Bristow et al’s [16] study are: 1) the enzyme markers used
in 1991 were under selection since they are protein coding genes and
are known to be non-neutral; and/or 2) we lose clarity of within and thatmanagement and conservation efforts should be applied at the
scale of the Gulf of Maine.
This work would not have been possible without the help and
insights of Peter Thayer of the Maine Department of Marine Resource
and Dan Harrington. We thank Glen Clark, Dan Harrington, Fred
Johnson, and John Renwick for harvesting worms and giving them
special treatment. Thanks to Dr. Joshua Lord for the help in the design
of Figure 1 and Isabelle Oliver for help in the design of the graphical
abstract.
Research reported in this project was supported by an
Institutional Development Award (IDeA) from the National Institute
of General Medical Sciences of the National Institutes of Health under
grant number P20GM103423 and funds from the Maine Department
ofMarine Resources (Contract 13A 2018 0110*2159).
Haplotype sequences have been deposited into GenBank through
accession numbers MN958890-MN958902.
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