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Bulletin of the Sea Fisheries Institute 1 (155) 2002 - CEEMaR

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14<br />

NATALIA KRASOVSKAJA<br />

Table 5. Duration <strong>of</strong> herring spawning season in <strong>the</strong> Vistula Lagoon by periods <strong>of</strong> different stock abundance<br />

Period<br />

Total herring<br />

catches [t]<br />

Catch per<br />

pound net [t]<br />

Stock<br />

abundance<br />

Duration <strong>of</strong> herring presence in<br />

<strong>the</strong> lagoon [days]<br />

Duration <strong>of</strong> mass<br />

spawning [days]<br />

1951-1954 11884 162 High 81 26<br />

1955-1966 1100 19 Low 62 26<br />

1967-1994 8472 131 High 69 37<br />

1995-2000 2944 31 Low 81 47<br />

On <strong>the</strong> contrary, changes in factors related to <strong>the</strong> spawning stock state did not cause very<br />

noticeable changes in <strong>the</strong> spawning pattern. Alternating periods <strong>of</strong> high and low stock abundance<br />

in <strong>the</strong> Vistula Lagoon are clearly determined (Fig. 2). When <strong>the</strong> data are summarized<br />

taking into account all <strong>the</strong> years until 2000, <strong>the</strong> results (Table 5) indicate ei<strong>the</strong>r weak or insignificant<br />

relationships despite significant changes in stock abundance. The same should be noted<br />

concerning age composition and growth rate changes. The current results confirmed <strong>the</strong> prevalent<br />

effect <strong>of</strong> abiotic factors on <strong>the</strong> herring spawning pattern in <strong>the</strong> Vistula Lagoon.<br />

The first spawning wave<br />

As follows from Table 4, <strong>the</strong> timing and duration <strong>of</strong> spawning are closely connected to <strong>the</strong> date<br />

<strong>the</strong> first spawning wave appeared. When <strong>the</strong> herring arrival is earlier, spawning begins and<br />

ends earlier, but <strong>the</strong> duration <strong>of</strong> <strong>the</strong> reproduction period is longer. The first herring onset in <strong>the</strong><br />

lagoon takes place from February 1 (1989) to April 25 (1970) at a mean water temperature <strong>of</strong><br />

0.5-8.0°C. The difference between <strong>the</strong> dates is up to 80 days. This is associated with <strong>the</strong> time <strong>of</strong><br />

<strong>the</strong> ice breakup and clearing from <strong>the</strong> lagoon. The correlation is remarkably close (Fig. 5). The<br />

role <strong>of</strong> fur<strong>the</strong>r temperature changes should be emphasized. A typical feature <strong>of</strong> <strong>the</strong> hydrological<br />

regime <strong>of</strong> <strong>the</strong> Vistula Lagoon is <strong>the</strong> unstable ice coverage; several ice breakups are observed in<br />

50% <strong>of</strong> <strong>the</strong> cases in winter and spring (Sergeeva 1983). However, <strong>the</strong> arrival <strong>of</strong> <strong>the</strong> herring<br />

schools occurs only with <strong>the</strong> commencement <strong>of</strong> steady water heating. If a standard period for<br />

May 10<br />

Apr 20<br />

March31<br />

March11<br />

Febr 19<br />

Jan 30<br />

Jan 10<br />

1951<br />

1954<br />

1957<br />

1960<br />

1963<br />

1966<br />

1969<br />

1972<br />

1975<br />

1978<br />

1981<br />

1984<br />

1987<br />

1990<br />

1993<br />

1996<br />

1999<br />

cleaning <strong>of</strong> ice<br />

first entering entrance <strong>of</strong> <strong>of</strong> herring into into <strong>the</strong> <strong>the</strong> Lagoon lagoon<br />

Fig. 5. Links between <strong>the</strong> dates <strong>of</strong> <strong>the</strong> herring first entrance into <strong>the</strong> lagoon and cleaning <strong>of</strong> ice<br />

(r 2 – 96.0%, p < 0.001).

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