scholarly journals Seasonal dynamics of <I>Pseudocalanus minutus elongatus</I> and <I>Acartia spp.</I> in the southern Baltic Sea (Gdańsk Deep) – numerical simulations

2006 ◽  
Vol 3 (4) ◽  
pp. 1157-1202
Author(s):  
L. Dzierzbicka-Głowacka ◽  
L. Bielecka ◽  
S. Mudrak

Abstract. A population dynamics model for copepods is presented describing a seasonal dynamics of Pseudocalanus minutus elongatus and Acartia spp. in the southern Baltic Sea (Gdansk Deep). The copepod model was coupled with an one-dimensional physical and biological upper layer model for nutrients (total inorganic nitrogen, phosphate), phytoplankton, microzooplankton and an early juvenile of herring as predator. In this model, mesozooplankton (herbivorous copepods) has been introduced as animals having definite patterns of growth in successive stages, reproduction and mortality. The populations are represented by 6 cohorts in different developmental stages, thus assuming, that recruitment of the next generation occurs after a fixed period of adult life. The copepod model links trophic processes and population dynamics, and simulates individual growth within cohorts and the changes in biomass between cohorts. The simulations of annual cycles of copepods contain one complete generation of Pseudocalanus and two generations of Acartia in the whole column water, and indicate the importance of growth of older stages of 6 cohorts each species to total population biomass. The peaks of copepods biomass, main, at the turn of June and July for Pseudocalanus and smaller, in July for Acartia, lag that phytoplankton by ca. two mouths due to growth of cohorts in successive stages and egg production by females. The numerical results show that the investigated species could not be the main factor limiting the spring phytoplankton bloom in the Gdansk Deep, because the initial development was slow for Acartia and faster for Pseudocalanus, but main development formed after the bloom, in both cases. However, the simulated microzooplankton biomass was enough high to conclude, in our opinion, that, in this case, it was major cause limiting phytoplankton bloom. Model presented here is a next step in understanding how the population dynamics of a dominant species in the southern Baltic Sea interact with the environment.

2006 ◽  
Vol 3 (4) ◽  
pp. 635-650 ◽  
Author(s):  
L. Dzierzbicka-Głowacka ◽  
L. Bielecka ◽  
S. Mudrak

Abstract. A population dynamics model for copepods is presented, describing the seasonal dynamics of Pseudocalanus minutus elongatus and Acartia spp. in the southern Baltic Sea (Gdańsk Deep). The copepod model was coupled with a one-dimensional physical and biological upper layer model for nutrients (total inorganic nitrogen, phosphate), phytoplankton, microzooplankton, and an early juvenile of herring as a predator. In this model, mesozooplankton (herbivorous copepods) has been introduced as an animal having definite patterns of growth in successive stages, reproduction and mortality. The populations are represented by 6 cohorts in different developmental stages, thus assuming that recruitment of the next generation occurs after a fixed period of adult life. The copepod model links trophic processes and population dynamics, and simulates individual growth within cohorts and the changes in biomass between cohorts. The simulations of annual cycles of copepods contain one complete generation of Pseudocalanus and two generations of Acartia in the whole column water, and indicate the importance of growth in the older stages of 6 cohorts of each species, to arrive at a total population biomass. The peaks of copepods' biomass are larger at the turn of June and July for Pseudocalanus and smaller in July for Acartia, lagging that of phytoplankton by ca. two mouths, due to the growth of cohorts in successive stages and egg production by females. The numerical results show that the investigated species could not be the main factor limiting the spring phytoplankton bloom in the Gdańsk Deep, because the initial development was slow for Acartia and faster for Pseudocalanus, but the main development formed after the bloom, in both cases. The phytoplankton bloom is very important in the diet of the adults of the copepods, but it is not particularly important for the youngest part of new generation (early nauplii). However, the simulated microzooplankton biomass was enough high to conclude, in our opinion, that, in this case, it was a major cause in limiting phytoplankton bloom. The model presented here is a next step in understanding how the population dynamics of a dominant species in the southern Baltic Sea interact with the environment.


2010 ◽  
Vol 7 (1) ◽  
pp. 55-82 ◽  
Author(s):  
L. Dzierzbicka-Glowacka ◽  
I. M. Żmijewska ◽  
S. Mudrak ◽  
J. Jakacki ◽  
A. Lemieszek

Abstract. This paper describes numerical simulations of the seasonal dynamics of Acartia spp. in the Southern Baltic Sea. The studies were carried out using a structured zooplankton population model adapted to Acartia spp. The population model with state variables for eggs, nauplii, five copepodites stages and adults was coupled with a marine ecosystem model. Four state variables for the carbon cycle represent the functional units of phytoplankton, pelagic detritus, benthic detritus, and bulk zooplankton, which represent all zooplankton other than the structured population. The annual cycle simulated for 2000 under realistic weather and hydrographic conditions was studied with the coupled ecosystem–zooplankton model applied to a water column in the Gdańsk Gulf (Southern Baltic Sea). The vertical profiles of selected state variables were compared to the physical forcing to study differences between bulk and structured zooplankton biomass. The simulated population dynamics of Acartia spp. and zooplankton as one biomass state variable were compared with observations in the Gdańsk Gulf. Simulated generation times are more affected by temperature than food conditions except during the spring phytoplankton bloom. The numerical studies are a following step in understanding how the population dynamics of a dominant species in the Southern Baltic Sea interact with the environment.


2013 ◽  
Vol 10 (7) ◽  
pp. 12347-12384
Author(s):  
L. Dzierzbicka-Glowacka ◽  
A. Lemieszek ◽  
M. Kalarus ◽  
I. M. Żmijewska

Abstract. The ecosystem model 3-D CEMBS connected with the population model, described in this paper, was used to determine the temporal distributions of T. longicornis in the Gdańsk Basin (the southern Baltic Sea) divided into the coastal zone P2 (the Gulf of Gdańsk) and the open sea P1 (Gdańsk Deep). The population model for T. longicornis consists of twelve equations for twelve states of variables, six for the mass Wi and six for the abundance Zi, i.e. two states of variables Wi and Zi, for each of the six model stages of the development; the stages were grouped as follows: eggs – Egg, stages not taking food – NI–NII, subsequent stages of nauplii – NIII–NVI, two copepodid stages – CI–CIII and CIV–CV and the last stage of adult organisms – CVI. Seasonal dynamics of T. longicornis is described by average changes in the total biomass as a sum of biomass of the examined ontogenesis stages, which are the sum of the products of the mass Wi and the abundance Zi of individual organisms at a given stage. The empirical verification of the population model based on in situ data obtained from the analysis of biological material collected in 2010–2011 in the region of Gdańsk Deep (P1) and in the western part of Gdańsk Bay (P2), and in 2006–2007 – only in Gdańsk Bay (P2). The highest values of the modelled T. longicornis biomass occurred in the period of high temperatures, i.e. in summer, in June 2010 and July 2011 in the Bay of Gdańsk – at station P2, and between late June and early July, and for almost the whole summer in Gdańsk Deep – at station P1, and amounted to respectively ca. 5200 mgw.w. m–2 and 6300 mgw.w. m–2 at station P2 and 24 500 mgw.w. m–2 and 27 800 mgw.w. m–2 at station P1. In 2006 and 2007 at station P2 the highest numerical values were recorded between late July and early August, exactly at the same time as environmental data, and amounted to 4300 mgw.w. m–2 and 5800 mgw.w. m–2, respectively. The results determined from the model are 0.25–2 times higher compared to in situ data. The most similar values were obtained for 2007.


2013 ◽  
Vol 47 (5-12) ◽  
pp. 715-738 ◽  
Author(s):  
L. Dzierzbicka-Glowacka ◽  
M. Kalarus ◽  
M. Janecki ◽  
M. Musialik ◽  
S. Mudrak ◽  
...  

Oceanologia ◽  
2009 ◽  
Vol 51 (2) ◽  
pp. 185-201 ◽  
Author(s):  
Lidia Dzierzbicka-Głowacka ◽  
Anna Lemieszek ◽  
Maria Iwona Żmijewska

Author(s):  
Lidia Dzierzbicka-Głowacka ◽  
Anna Lemieszek ◽  
Maja Musialik ◽  
Iwona Żmijewska

AbstractThe paper presents modeling of egg production (Egg — no. of eggs female−1 d−1) by Temora longicornis in the changing environmental conditions of the southern Baltic Sea (Gdańsk Deep). It is hypothesized that the food-saturated rate of egg matter production is equivalent to the specific growth rate of copepods. Based on the findings from the south-western Baltic Sea, Egg of T. longicornis is evaluated as a function of food concentration, temperature and salinity over a wide range of these parameters. Subsequently, the rate of reproduction during the seasons in the Gulf of Gdańsk is determined. According to our calculations, values of Egg reach ca 11 eggs per day in April and decline strongly in June-July, while the second smaller peak in reproduction occurs in September, ca 8 eggs per day. Our results suggest that egg production rates of T. longicornis depend not only on food concentration and temperature, but also on salinity, which is a masking factor in the Baltic Sea.


Oceanologia ◽  
2015 ◽  
Vol 57 (1) ◽  
pp. 78-85 ◽  
Author(s):  
Lidia Dzierzbicka-Głowacka ◽  
Marcin Kalarus ◽  
Maja Musialik-Koszarowska ◽  
Anna Lemieszek ◽  
Maria Iwona Żmijewska

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