The color of the water is the first thing that visitors to Lake Natron notice. The organic material is completely replaced by minerals as the permineralization process continues, resulting in a petrified specimen. These minerals fill the spaces between the organism's cells, preserving the organism's original shape and form. Permineralization gradually replaces organic material with minerals such as silica, calcite, or pyrite. This process is known as permineralization. Minerals from the surrounding rock or sediment begin to seep into the organic material over time, eventually replacing the original material on a cellular level. The organic material is first buried by sediment or volcanic ash, which protects it from decay and exposure to the elements. 'The contributors have identified key knowledge gaps in the fast evolving field of marine global change biology and have provided many important insights,' the co-editors write.īy sharing research on this topic from researchers around the world, the Biological Bulletin is raising awareness of some of the greatest threats to the oceans today and emphasizing the global nature of the problem.There are several steps involved in the process of petrifaction. Several papers take a broader population-based view by studying the effect of ocean acidification on predator-prey interactions in mollusks (Kroeker and colleagues of the University of California-Davis) and oysters (Wright and colleagues of the University of Western Sydney). Abigail Smith of the University of Otago examines how bryozoans, a group of aquatic invertebrate filter-feeders, increase biodiversity by creating niche habitats, and what features make them particularly sensitive to calcium fluctuations.Įvans and Watson-Wynn (California State University-East Bay) take a molecular approach in a meta-analysis showing that ocean acidification is effecting genetic changes in sea urchin larvae. Other researchers address lesser-known organisms that are nevertheless critical to marine ecosystems. Janice Lough and Neal Cantin of the Australian Institute of Marine Science review historical data on coral reefs to look at potential environmental stressors, while Philippe Dubois (Université Libre de Bruxelles) discusses sea urchin skeletons. The CO 2 itself can also directly cause metabolic stress,' write the issue's co-editors, Maria Byrne of the University of Sydney and Gretchen Hofmann of the University of California-Santa Barbara.Ĭontributors to the journal address this timely issue across many taxa and from a variety of perspectives, from genomic to ecosystem-wide. 'Today, modern calcifiers face a new and rapidly escalating crisis caused by warming and acidification of the oceans with a reduction in availability of carbonate minerals, a change driven by the increase in atmospheric CO 2 due to anthropogenic emissions and industrialization. This use of calcium carbonate promoted biodiversity, including the vast array of calcifiers seen today.

The ability to calcify arose independently in many species during the Cambrian era, when calcium levels in seawater increased. This impact of global climate change threatens the survival of calcifying species because of the reduced saturation of the carbonate minerals required for calcification.

The June issue of the Biological Bulletin, published by the Marine Biological Laboratory, addresses the challenges faced by these species as ocean composition changes worldwide.Īs atmospheric carbon dioxide rises, the world's oceans are becoming warmer and more acidic.

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