Experimental parameterisation of principal physics in buoyancy variations of marine teleost eggs

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Abstract

It is generally accepted that the high buoyancy of pelagic marine eggs is due to substantial influx of water across the cell membrane just before ovulation. Here we further develop the theoretical basis by applying laboratory observations of the various components of the fertilized egg in first-principle equations for egg specific gravity (ρegg) followed by statistical validation. We selected Atlantic cod as a model animal due to the affluent amount of literature on this species, but also undertook additional dedicated experimental works. We found that specific gravity of yolk plus embryo is central in influencing ρegg and thereby the buoyancy. However, our established framework documents the effect on ρegg of the initial deposition of the heavy chorion material in the gonad prior to spawning. Thereafter, we describe the temporal changes in ρegg during incubation: Generally, the eggs showed a slight rise in ρegg from fertilization to mid-gastrulation followed by a gradual decrease until full development of main embryonic organs just before hatching. Ontogenetic changes in ρegg were significantly associated with volume and mass changes of yolk plus embryo. The initial ρegg at fertilization appeared significantly influenced by the chorion volume fraction which is determined by the combination of the final chorion volume of the oocyte and of the degree of swelling (hydrolyzation) prior to spawning. The outlined principles and algorithms are universal in nature and should therefore be applicable to fish eggs in general. © 2014 Jung et al.

Figures

  • Figure 1. Ontogenetic changes of three seasons from 2–3 dpf until hatching (continuous egg specific gravity measurements). (A) Batch3, (B) Batch4, and (C) Batch8 represent winter, spring, and fall, respectively. Age of egg development is expressed in days post-fertilization (dpf). Horizontal lines refer to initial specific gravity of the selected layers (Batch3-b, Batch4-b and Batch8-b) at 2–3 dpf. Symbol of underlined # indicates the level of eggs used for slope tests in Table S2. doi:10.1371/journal.pone.0104089.g001
  • Figure 2. Ontogenetic changes in (A) egg dry weight/egg volume, (B) water content, (C) yolk volume/egg volume, and (D) chorion volume/egg volume. Selected buoyancy layers were Batch2-b and Batch3-b in winter, Batch4-b and Batch5-a in spring, and Batch7-a and Batch8-a in fall. As egg distribution overlapped with other layers of eggs, in particular after the latter half incubation, each egg component was divided by mean egg volume in order to avoid egg size effects except for the water content. Points refer to mean and one standard deviation. doi:10.1371/journal.pone.0104089.g002
  • Figure 4. Relationship between egg specific gravity and specific gravity of yolk plus embryo at 2–3 dpf. The specific gravity of yolk plus embryo was estimated by Eq. 4 (Appendix). doi:10.1371/journal.pone.0104089.g004
  • Figure 3. Estimated specific gravity (g cm23) of cod eggs based on equation from multiple regression versus observed specific gravity from the same egg batches (solid line). Open symbols for original cases without missing variable values and filled symbols for extra data points included after the initial analysis. Dashed line represents 1:1 line, and dotted lines represent 95% confidence regression bands. doi:10.1371/journal.pone.0104089.g003
  • Table 1. Calculated influence of three egg components on egg specific gravity (regg) for Atlantic cod based on observed ranges of the components.

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CITATION STYLE

APA

Jung, K. M., Folkvord, A., Kjesbu, O. S., & Sundby, S. (2014). Experimental parameterisation of principal physics in buoyancy variations of marine teleost eggs. PLoS ONE, 9(8). https://doi.org/10.1371/journal.pone.0104089

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