Abstract

Arctica islandica is the longest-living non-colonial animal known at present. It inhabits coastal waters in the North Atlantic and its annual shell increments are widely used for paleoclimatic reconstructions. There is no consensus, however, about the intra-annual timing of its feeding activity and growth. This research aims to identify the main environmental drivers of A. islandica valve gape to clarify the ambiguity surrounding its seasonal activity. A lander was deployed from February 2014 to September 2015 on the sea bottom at Ingøya, Norway (71°03′N, 24°05′E) containing living A. islandica specimens (70.17 ± 0.95 mm SE) in individual containers. Each individual was attached to an electrode unit that measured the distance between their valves (valve gape) every minute. Individuals were followed for various lengths of time, and in some cases replaced by smaller individuals (54.34 ± 0.63 mm SE). The lander was also equipped with instruments to simultaneously monitor temperature, salinity, [Chl-a], turbidity, and light. There was a significant difference in the average monthly valve gape (P value < 0.01), with monthly means of 19–84% of the total valve gape magnitude. The experimental population was largely inactive October–January, with an average daily gape <23%. During this period the clams opened at high amplitude once or twice a month for 1–3 days. Seasonal cycles of sea water temperature and [Chl-a] were temporally offset from each other, with temperature lagging [Chl-a] by about 2 months. Multiple regression analyses showed that bivalve gaping activity was most closely correlated with variable [Chl-a], and to a much smaller degree with photoperiod and temperature.

Highlights

  • This study demonstrated a positive relationship between high siphon activity and growth in all treatments (Witbaard et al 1997b). These results suggest that valve opening and closing of A. islandica can be used as a proxy for active feeding and as an indicator of periods of potential growth

  • The lowest individual temperature record of 0.8 °C was recorded on February 3, 2015, and the maximum temperature of 10.3 °C occurred on August 9, 2014 and August 27, 2015

  • The experimental organisms had electro-coils attached to the outside of their shells and were each kept in individual cups, there is no indication that this experimental setup impacted the study results or considerably modified the valve gape behavior

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Summary

Introduction

Electronic supplementary material The online version of this article (doi:10.1007/s00227-017-3144-7) contains supplementary material, which is available to authorized users. The bivalve Arctica islandica, known as the ocean quahog, inhabits coastal waters in the North Atlantic (Jones 1980; Dahlgren et al 2000). The species is the longestliving non-colonial animal yet known, with a longevity of >500 years (Butler et al 2013). A history of their growth is retained in their shells. Shell growth increments (or growth bands) can provide basic biological information on the species including age and growth rate. The pattern of these bands and the composition of the shell material therein can reflect environmental conditions when the shell was deposited

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