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Environmental Monitoring and Assessment · 2025 · Vol. 197 · Issue 9 · Springer
Ocean acidification (OA), caused by the uptake of anthropogenic carbon dioxide, is a concern for ocean resource users in coastal regions where the phenomenon is compounded by variable processes. Sustained OA monitoring systems are critical for characterization of baseline ocean conditions and identification of changes and impacts to coastal ecosystems and communities. Establishing an OA monitoring network is best accomplished...
Yves Guglielmi; Mark McClure; Jeffrey Burghardt; Joseph P. Morris; Thomas Doe; Pengcheng Fu; Hunter Knox; Vince Vermeul; Tim Kneafsey; J. Ajo-Franklin; T. Baumgartner; K. Beckers; D. Blankenship; A. Bonneville; L. Boyd; S. Brown; J.A. Burghardt; C. Chai; A. Chakravarty; T. Chen; Y. Chen; B. Chi; K. Condon; P.J. Cook; D. Crandall; P.F. Dobson; T. Doe; C.A. Doughty; D. Elsworth; J. Feldman; Z. Feng; A. Foris; L.P. Frash; Z. Frone; P. Fu; K. Gao; A. Ghassemi; Y. Guglielmi; B. Haimson; A. Hawkins; J. Heise; C. Hopp; M. Horn; R.N. Horne; J. Horner; M. Hu; H. Huang; L. Huang; K.J. Im; M. Ingraham; E. Jafarov; R.S. Jayne; T.C. Johnson; S.E. Johnson; B. Johnston; S. Karra; K. Kim; D.K. King; T. Kneafsey; H. Knox; J. Knox; D. Kumar; K. Kutun; M. Lee; D. Li; J. Li; K. Li; Z. Li; M. Maceira; P. Mackey; N. Makedonska; C.J. Marone; E. Mattson; M.W. McClure; J. McLennan; T. McLing; C. Medler; R.J. Mellors; E. Metcalfe; J. Miskimins; J. Moore; C.E. Morency; J.P. Morris; T. Myers; S. Nakagawa; G. Neupane; G. Newman; A. Nieto; T. Paronish; R. Pawar; P. Petrov; B. Pietzyk; R. Podgorney; Y. Polsky; J. Pope; S. Porse; J.C. Primo; T. Pyatina; C. Reimers; B.Q. Roberts; M. Robertson; V. Rodríguez-Tribaldos; W. Roggenthen; J. Rutqvist; D. Rynders; M. Schoenball; P. Schwering; V. Sesetty; C.S. Sherman; A. Singh; M.M. Smith; H. Sone; E.L. Sonnenthal; F.A. Soom; D.P. Sprinkle; S. Sprinkle; C.E. Strickland; J. Su; D. Templeton; J.N. Thomle; C. Ulrich; N. Uzunlar; A. Vachaparampil; C.A. Valladao; W. Vandermeer; G. Vandine; D. Vardiman; V.R. Vermeul; J.L. Wagoner; H.F. Wang; J. Weers; N. Welch; J. White; M.D. White; P. Winterfeld; T. Wood; S. Workman; H. Wu; Y.S. Wu; E.C. Yildirim; Y. Zhang; Y.Q. Zhang; Q. Zhou; M.D. Zoback
Global Change Biology · 2023 · Vol. 29 · Issue 12 · Wiley
Scientists and managers rely on indicator taxa such as coral and macroalgal cover to evaluate the effects of human disturbance on coral reefs, often assuming a universally positive relationship between local human disturbance and macroalgae. Despite evidence that macroalgae respond to local stressors in diverse ways, there have been few efforts to evaluate relationships between specific macroalgae taxa and local human‐driven d...
Frontiers in Marine Science · 2021 · Vol. 8 · Frontiers
Coral research is being ushered into the genomic era. To fully capitalize on the potential discoveries from this genomic revolution, the rapidly increasing number of high-quality genomes requires effective pairing with rigorous taxonomic characterizations of specimens and the contextualization of their ecological relevance. However, to date there is no formal framework that genomicists, taxonomists, and coral scientists can co...
Rock Mechanics and Rock Engineering · 2020 · Vol. 53 · Issue 11 · Springer
Katherine J. Condon; Hiroki Sone; Herbert F. Wang; J. Ajo-Franklin; T. Baumgartner; K. Beckers; D. Blankenship; A. Bonneville; L. Boyd; S. Brown; J. A. Burghardt; C. Chai; Y. Chen; B. Chi; K. Condon; P. J. Cook; D. Crandall; P. F. Dobson; T. Doe; C. A. Doughty; D. Elsworth; J. Feldman; Z. Feng; A. Foris; L. P. Frash; Z. Frone; P. Fu; K. Gao; A. Ghassemi; Y. Guglielmi; B. Haimson; A. Hawkins; J. Heise; C. Hopp; M. Horn; R. N. Horne; J. Horner; M. Hu; H. Huang; L. Huang; K. J. Im; M. Ingraham; E. Jafarov; R. S. Jayne; S. E. Johnson; T. C. Johnson; B. Johnston; K. Kim; D. K. King; T. Kneafsey; H. Knox; J. Knox; D. Kumar; M. Lee; K. Li; Z. Li; M. Maceira; P. Mackey; N. Makedonska; E. Mattson; M. W. McClure; J. McLennan; C. Medler; R. J. Mellors; E. Metcalfe; J. Moore; C. E. Morency; J. P. Morris; T. Myers; S. Nakagawa; G. Neupane; G. Newman; A. Nieto; C. M. Oldenburg; T. Paronish; R. Pawar; P. Petrov; B. Pietzyk; R. Podgorney; Y. Polsky; J. Pope; S. Porse; J. C. Primo; C. Reimers; B. Q. Roberts; M. Robertson; W. Roggenthen; J. Rutqvist; D. Rynders; M. Schoenball; P. Schwering; V. Sesetty; C. S. Sherman; A. Singh; M. M. Smith; H. Sone; E. L. Sonnenthal; F. A. Soom; P. Sprinkle; C. E. Strickland; J. Su; D. Templeton; J. N. Thomle; V. R. Tribaldos; C. Ulrich; N. Uzunlar; A. Vachaparampil; C. A. Valladao; W. Vandermeer; G. Vandine; D. Vardiman; V. R. Vermeul; J. L. Wagoner; H. F. Wang; J. Weers; N. Welch; J. White; M. D. White; P. Winterfeld; T. Wood; S. Workman; H. Wu; Y. S. Wu; E. C. Yildirim; Y. Zhang; Y. Q. Zhang; Q. Zhou; M. D. Zoback
Molecular Ecology · 2014 · Vol. 23 · Issue 15 · Wiley
Variation in prey resources influences the diet and behaviour of predators. When prey become limiting, predators may travel farther to find preferred food or adjust to existing local resources. When predators are habitat limited, local resource abundance impacts foraging success. We analysed the diet of Myotis lucifugus (little brown bats) from Nova Scotia (eastern Canada) to the Northwest Territories (north‐western Canada). T...
Molecular Ecology · 2007 · Vol. 16 · Issue 3 · Wiley
The principal vector of malaria in sub‐Saharan Africa, Anopheles gambiae is subdivided into two molecular forms M and S. Additionally, several chromosomal forms, characterized by the presence of various inversion polymorphisms, have been described. The molecular forms M and S each contain several chromosomal forms, including the Savanna, Mopti and Forest forms. The M and S molecular forms are now considered to be the reproduct...
Limnology and Oceanography · 1997 · Vol. 42 · Issue 7 · Wiley
We have developed and successfully collected data with a unique, bottom‐transecting vehicle (ROVER) that permits the first long time‐series measurements of sediment community oxygen consumption (SCOC). This instrument has the following capabilities: (1) it operates as an autonomous, free vehicle on the sea floor to 6,000‐m depth for periods up to 6 months; (2) it transits across the sea floor, minimizing the impact that a long...