The Virtual Copepod Page:
Copepod Introduction

Very Basic Copepod Introduction

(Skip this if you already know what a copepod is.)

Copepods are a type of crustacean, the class of animals that also includes shrimps, lobsters, and crabs. Copepods are one of the most abundant animals on the planet. Most are saltwater plankton, living their entire lives in the open ocean without ever touching the bottom or surface. Copepods also live on the sea bottom, in fresh water, as parasites on fish, in caves...

Euchaeta Biological Introduction

Copepods in the genus Euchaeta are planktonic and predatory. Congeners of Euchaeta (Kingdom Animalia, Phylum Crustacea, Class Copepoda, Order Calanoida, Superfamily Clausocalanoidea, Family Euchaetidae, Genus Euchaeta) live in seas from the Antarctic to the tropics, within the fjords of Norway and Puget Sound, and in deep lochs of Scotland. In their respective open-ocean planktonic communities, these copepods are often biomass dominants because of their high abundance, large size, and high lipid content (up to 70% their body weight). The image to the right was taken by Yen and Strickler and shows a typical Euchaeta. The long antennules are lined with sensitive setal receptors to detect fluid motion and odors. This photo of the live subarctic species, shows its natural coloration with blue oocytes within the oviducts and iridescence imparted by the thin caudal setae. The robust capture appendages, the paired maxillipeds, are shown extended away from anterior section of body.


Euchaeta are gigantic (for copepods), with the adult subtropical females growing to 2.4 millimeters in length and the polar species reaching up to 1 cm. Males are somewhat smaller. Their maxillipeds are used to capture and eat other copepods. These photos depict the structure of the capture appendages, the maxillipeds and maxillae. The left photo is a drawing from Wickstead(1959). The right is a scanning electron micrograph by J. Yen(1985).


Computer Visualization Introduction

We created and animated our model using 3D Studio Max from Discrete Logic. This high-end animation package is widely used by movie special effects artists.

To create our models and animations, we first looked at illustrations in the literature. Rose 1933 gave us a good starting point. To create the prosome, we scanned 2D images from Rose into the computer and traced them using Bezier curves to create the outline of the prosome as seen from the left-hand side. We then made an estimate of curves representing the outline of the prosome as seen from the rear. Using these two sets of curves, we were able to create a Bezier patch surface approximating the prosome. We then checked our results by rendering images from several viewpoints and comparing them against preserved specimens. We also showed the images to Annie Townsend, curator of the SIO Planktonic Invertebrates Collection. She was able to suggest many important improvements.

The other segments of the prosome and urosome were constructed in a similar fashion, as were the appendages. We found that NURBS surfaces generally gave better results with less effort than other techniques for modelling curved surfaces.

Setae provided a special animation challenge, as there are so many of them. After exploring several techniques we used loft surfaces created from circles and Bezier splines. The tip of each seta was attached to a controller, so that each seta could be individually positioned if necessary. We generally avoided this by attaching the tips of each set of setae to a master controller. To give a more natural appearance, the setae on the maxillae are translated and rotated using a random noise function.

To animate our model, we first determined the range of motion of the joints by examining preserved specimens. We then looked at video of live animals. Using key frame animation, we were able to approximate the motion of the living animals. Once the computer model had been animated, it could be examined from any angle and at any speed.

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All images, animations, models, and scripts are copyright 2000 Scripps Institution of Oceanography and may not be published or re-used without permission.