By Gary D. Wisehart, Erin C. Rempala, Michael J. Leboffe, David Ferguson

This publication is a full-color complement that offers pictures of preserved specimens and photographs taken at quite a few aquaria to supply insurance of organisms within the world's oceans. it truly is designed to accompany any marine biology textual content or laboratory guide. 3-hole drilled

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Sample text

The ratio 1 of stable oxygen isotopes changes with water temperature, and this is reflected in the test chemistry. Foraminiferans range in size from 100 µm in the smallest planktonic species to approximately 20 cm in large deep-sea forms. Some forams house algae as endosymbionts that supply them with nutrients, while others feed on diatoms, bacteria, and other small plankton. They capture prey with movable, netlike pseudopodia (pseudo—false, podia—foot) called reticulopodia (reticulo—a network, podia—foot) that extend and branch out of the body wall.

Some species are naked and the vesicles do not contain cellulose plates. On a gross cellular level, the girdle marks the separation of the anterior epitheca (epi—upon, theca—case) and the posterior hypotheca (hypo—below) portions of the cell (these are also referred to as valves). Photosynthetic dinoflagellates are important primary producers and are one of the main causes of harmful algal blooms (HABs), or “red” tides (Figure 3-3). Many HABs are toxic to humans or other organisms upon contact with high levels of dinoflagellates, while others are toxic (and can be fatal) if consumed.

Forams contain two different types of nuclei, similar to ciliates. Radiolaria Radiolaria (Figure 3-5) is a group rich with diverse morphologies, life histories, and a fossil history dating to the Cambrian period. Radiolarians are entirely marine, and most are planktonic, ranging in size from 30 µm–2 mm. A few colonial species are as large as 20 cm. They have durable, glassy tests (most are radially symmetrical) that become part of siliceous biogenic sediment (“radiolarian ooze”) when they die and sink to the seafloor.

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