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MARINE SCIENCE AND BIOLOGY

Bloodworm (Glycera dibranchiata Ehlers, 1868) Populations in the Gulf of Maine Are Connected Through Gene Flow

Larissa M. Williams1*, Anna Marie Bowsher1, Maria-Anna Chrysovergi1, William G. Ambrose Jr.2

1 Department of Biology,  Bates College, Lewiston ME 04240, United States
2 Department of Coastal and Marine Systems Science, Coastal Carolina University, United States

CitationCitation COPIED

Williams LM, Bowsher AM, Chrysovergi MA, Ambrose Jr. WG. Bloodworm (Glycera dibranchiata Ehlers, 1868) Populations in the Gulf of Maine Are Connected Through Gene Flow. Mar Sci Biol. 2020 Feb;1(1):101.

© 2020 Williams LM, et al. This is an open-access article distributed under the terms of the Creative Commons Attribution 4.0 international License, which permits unrestricted use, distribution and reproduction in any medium, provided the original author and source are credited.

Abstract

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).


Graphical Abstract

Keywords

Bloodworm, Glycera, gene flow, cytochrome c oxidase I (COI), Gulf of Maine

Introduction

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.

Materials and Methods

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 (\[F_{ST}\]).

Results

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).

Discussion

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.

Acknowledgments

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.

Funding

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).

Data Availability

Haplotype sequences have been deposited into GenBank through accession numbers MN958890-MN958902.

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