Axopodorhabdus albianus, coccolith
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Axopodorhabdus albianus, coccolith
Scanning electron microscope image of a Cretaceous coccolith from Folkestone Chalk (x 10, 000 on a standard 9 cm wide print)
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Media ID 8591629
© Mary Evans Picture Library 2015 - https://copyrighthub.org/s0/hub1/creation/maryevans/MaryEvansPictureID/10708486
Alga Algae Algal Calcite Calcite Group Carbonate Carbonate Mineral Chalk Chromalveolata Chromista Coccolith Coccolithophore Coccolithophorid Electron Micrograph Eukaryote Eukaryotic Haptophyta Haptophyte Micrograph Microscope Image Mineral Phytoplankton Plankton Invertebrata
EDITORS COMMENTS
1. Title: A Glimpse into the Past: Axopodorhabdus albianus and its Calcite Coccolith in the Folkestone Chalk 2. Description: This stunning scanning electron microscope image showcases the intricate details of a single calcite coccolith, belonging to the Axopodorhabdus albianus species, discovered in the Folkestone Chalk formation. This ancient planktonic organism, a member of the phylum Chromalveolata and the class Haptophyceae, once thrived in the Cretaceous Sea. The coccolith, a carbonate mineral armor made of calcite, encases the microscopic algae and protects it from predators and environmental hazards. 3. Background: Axopodorhabdus albianus is a coccolithophore, a type of eukaryotic algae that produces intricate calcite plates called coccoliths. These organisms are essential primary producers in the marine food chain and play a significant role in carbon cycling in the ocean. The Folkestone Chalk, a renowned geological formation in England, is rich in fossilized coccoliths, providing valuable insights into the biosphere of the late Cretaceous period. 4. Detailed Observation: In this image, the coccolith's hexagonal shape is apparent, with intricate patterns and ridges adorning its surface. The calcite mineral structure is evident, revealing the complex biomineralization process that occurred within the living organism. The presence of this coccolith in the chalk formation indicates that Axopodorhabdus albianus was once abundant in the Cretaceous Sea, contributing to the formation of the chalk through its calcium carbonate production. 5. Significance: This image offers a fascinating glimpse into the past, providing insights into the morphology and biology of an ancient organism that played a crucial role in shaping the marine ecosystem during the Cretaceous period. The study of coccoliths and their fossilized remains contributes to our understanding of past climates, ocean conditions, and the evolution of marine life.
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