DOI: https://doi.org/10.3354/meps14170
copiedOrigin of marine invertebrate larvae on an Arctic inflow shelf
- Raphaëlle Descôteaux
- Mats Huserbråten
- Lis Lindal Jørgensen
- Paul E. Renaud
- Randi B. Ingvaldsen
- Elizaveta A. Ershova
- Bodil A. Bluhm
ABSTRACT:
Many benthic invertebrate taxa possess planktonic early life stages which drift with water currents and contribute to dispersal of the species, sometimes reaching areas beyond the current ranges of the adults. Until recently, it had been difficult to identify planktonic larvae to species level due to lack of distinguishing features, preventing detection of expatriate species. Here, we used DNA metabarcoding of the COI gene to obtain species-level identification of early life stages of benthic invertebrates in zooplankton samples from the Barents Sea and around Svalbard, where, regionally, large volumes of warm Atlantic Water enter the Arctic from the south. We compared the larval community in the water column to the adult community on the seafloor to identify mismatches. In addition, we implemented particle tracking analysis to identify the possible areas of origin of larvae. Our results show that 30-45% of larval taxa—largely polychaetes and nudibranchs—were not local to the sampling area, though most were found nearby in the Barents Sea. In the particle tracking analysis, some larvae originating along the Norwegian coast were capable of reaching the northwest coast of Svalbard within 3 mo, but larvae found east of Svalbard had a more constrained possible area of origin which did not extend to the Norwegian coast. This study highlights largely regional-scale larval connectivity in the Barents Sea but demonstrates the potential for some long-lived larval taxa to travel to Svalbard and the Barents Sea from further south.
KEYWORDS

Most Barents Sea larvae are of local or regional origin, but some are drifting into the Arctic from further south.
Graphic: Raphaëlle Descôteaux
For many marine benthic invertebrate species, a planktonic larval phase is the main dispersal vector. Inflow shelves like the Barents Sea are likely major entry points of drifting southern larvae into the Arctic. Descôteaux and colleagues compared larval distributions (identified from DNA metabarcoding of zooplankton samples) with adult distributions, complemented with particle tracking analysis, to infer the origins of larvae. They demonstrated that despite its strong advective nature, the Barents Sea was dominated by locally- or regionally-produced larvae. There is evidence, however, that some long-lived larvae can currently drift onto this inflow shelf from further south, raising the possibility of rapid range extensions into the Arctic as the climate continues to warm.
Raphaëlle Descôteaux (Corresponding Author)
- UiT, The Arctic University of Norway, Tromsø 9037, Norway
Mats Huserbråten (Co-author)
- Institute of Marine Research, Bergen 5005, Norway
Lis Lindal Jørgensen (Co-author)
- Institute of Marine Research, Bergen 5005, Norway
Paul E. Renaud (Co-author)
- Akvaplan-niva, Fram Centre for Climate and the Environment, Tromsø 9007, Norway
- The University Centre in Svalbard, Svalbard 9170, Norway
Randi B. Ingvaldsen (Co-author)
- UiT, The Arctic University of Norway, Tromsø 9037, Norway
- Institute of Marine Research, Bergen 5005, Norway
Elizaveta A. Ershova (Co-author)
- Institute of Marine Research, Bergen 5005, Norway
- Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow 117997, Russia
Bodil A. Bluhm (Co-author)
- UiT, The Arctic University of Norway, Tromsø 9037, Norway
