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  1. Sep 12, 2016 · Sophie Parsons. The International Journal of Life Cycle Assessment (2024) Marine macroalgae are dominant primary producers in coastal zones. A review of the published literature suggests that ...

  2. one that best suits their way of life. From organ-isms that sessile with a benthonic mode of life, or those that swim in the water between the algae Macroalgae: Diversity and Conservation, Fig. 4 Branching types: (a) irregular; (b) dichotomous; (c) alternating; (d) opposite; (e) verticillate; (f) pectinate Macroalgae: Diversity and Conservation 5

  3. en.wikipedia.org › wiki › ProtistProtist - Wikipedia

    Marine protists are highly diverse, have a fundamental impact on biogeochemical cycles (particularly, the carbon cycle) and are at the base of the marine trophic networks as part of the plankton. Phototrophic marine protists located in the photic zone as phytoplankton are vital primary producers in the oceanic systems.

  4. Many of the protist species classified into the supergroup Excavata are asymmetrical, single-celled organisms with a feeding groove “excavated” from one side. This supergroup includes heterotrophic predators, photosynthetic species, and parasites. Its subgroups are the diplomonads, parabasalids, and euglenozoans.

  5. Foraminifera (forams for short) are large protists that design their outer shells, called tests, out of calcium carbonate. They use long thin extensions, called reticulopodia, to catch their prey ...

  6. Hamsher SE, Evans KM, Mann DG, Poulícková A, Saunders GW (2011) Barcoding diatoms: exploring alternatives to COI-5P. Protist 162: 405–422 Saunders GW, Kucera H (2010) An evaluation of rbc L, tufA, UPA, LSU and ITS as DNA barcode markers for the marine green macroalgae. Crypt Algol 31:487–528

  7. Ocean chlorophyll concentration as a proxy for marine primary production. Green indicates where there are a lot of phytoplankton, while blue indicates where there are few phytoplankton. – NASA Earth Observatory 2019. Marine primary production is the chemical synthesis in the ocean of organic compounds from atmospheric or dissolved carbon dioxide.

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