David Obura
New England Aquarium
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Proceedings of the Royal Society B: Biological Sciences | 2016
Jennifer E. Smith; Rusty Brainard; Amanda L. Carter; Saray Grillo; Clinton Edwards; Jill Harris; Levi S. Lewis; David Obura; Forest Rohwer; Enric Sala; Peter S. Vroom; Stuart A. Sandin
Numerous studies have documented declines in the abundance of reef-building corals over the last several decades and in some but not all cases, phase shifts to dominance by macroalgae have occurred. These assessments, however, often ignore the remainder of the benthos and thus provide limited information on the present-day structure and function of coral reef communities. Here, using an unprecedentedly large dataset collected within the last 10 years across 56 islands spanning five archipelagos in the central Pacific, we examine how benthic reef communities differ in the presence and absence of human populations. Using islands as replicates, we examine whether benthic community structure is associated with human habitation within and among archipelagos and across latitude. While there was no evidence for coral to macroalgal phase shifts across our dataset we did find that the majority of reefs on inhabited islands were dominated by fleshy non-reef-building organisms (turf algae, fleshy macroalgae and non-calcifying invertebrates). By contrast, benthic communities from uninhabited islands were more variable but in general supported more calcifiers and active reef builders (stony corals and crustose coralline algae). Our results suggest that cumulative human impacts across the central Pacific may be causing a reduction in the abundance of reef builders resulting in island scale phase shifts to dominance by fleshy organisms.
Archive | 2008
James E. Maragos; Alan M. Friedlander; Scott Godwin; Craig Musburger; Roy T. Tsuda; Elizabeth Flint; Olga Pantos; Paula Ayotte; Enric Sala; Stuart A. Sandin; Sarah McTee; Daria Siciliano; David Obura
This is the second of two chapters on the coral reefs of the five US Line and Phoenix Islands, consisting of Baker, Howland and Jarvis Islands, Kingman Reef, ; and Palmyra Atoll (Fig. 16.1). The previous chapter (Chapter 15, Maragos et al.) covers the history, geology, oceanography and biology, while this chapter covers the status, threats and significance of the five. All are low reef islets or atolls in the central Pacific Ocean administered by the US Fish and Wildlife Service as National Wildlife Refuges. These 5 Refuges are among 20 within the tropical Pacific and among 10 that protect coral reefs. Together they are geographically a part of the largest series of fully protected marine areas under unified management in the world.
Advances in Marine Biology | 2014
Randi D. Rotjan; Regen Jamieson; Ben Carr; Les Kaufman; Sangeeta Mangubhai; David Obura; Ray Pierce; Betarim Rimon; Bud Ris; Stuart A. Sandin; Peter Shelley; U. Rashid Sumaila; Sue Taei; Heather Tausig; Tukabu Teroroko; Simon R. Thorrold; Brooke Wikgren; Teuea Toatu; Greg Stone
The Republic of Kiribatis Phoenix Islands Protected Area (PIPA), located in the equatorial central Pacific, is the largest and deepest UNESCO World Heritage site on earth. Created in 2008, it was the first Marine Protected Area (MPA) of its kind (at the time of inception, the largest in the world) and includes eight low-lying islands, shallow coral reefs, submerged shallow and deep seamounts and extensive open-ocean and ocean floor habitat. Due to their isolation, the shallow reef habitats have been protected de facto from severe exploitation, though the surrounding waters have been continually fished for large pelagics and whales over many decades. PIPA was created under a partnership between the Government of Kiribati and the international non-governmental organizations-Conservation International and the New England Aquarium. PIPA has a unique conservation strategy as the first marine MPA to use a conservation contract mechanism with a corresponding Conservation Trust established to be both a sustainable financing mechanism and a check-and-balance to the oversight and maintenance of the MPA. As PIPA moves forward with its management objectives, it is well positioned to be a global model for large MPA design and implementation in similar contexts. The islands and shallow reefs have already shown benefits from protection, though the pending full closure of PIPA (and assessments thereof) will be critical for determining success of the MPA as a refuge for open-ocean pelagic and deep-sea marine life. As global ocean resources are continually being extracted to support a growing global population, PIPAs closure is both timely and of global significance.
Reviews in Fish Biology and Fisheries | 2014
Sangeeta Mangubhai; Ayron M. Strauch; David Obura; Gregory Stone; Randi D. Rotjan
Climate change-related disturbances are increasingly recognized as critical threats to biodiversity and species abundance. On coral reefs, climate disturbances have known consequences for reef fishes, but it is often difficult to isolate the effect of coral bleaching from preceding or simultaneous disturbances such as fishing, pollution, and habitat loss. In this study, pre-bleaching surveys of fish family assemblages in the remote Phoenix Islands in 2002 are compared to post-bleaching in 2005, following severe thermal stress. Post-bleaching, total coral cover decreased substantially, as did the combined abundance of all fish families. Yet, changes in abundance for specific fish families were not uniform, and varied greatly from site to site. Of the 13 fish families examined, 3 exhibited significant changes in abundance from 2002 to 2005, regardless of site (Carangidae, Chaetodontidae, and serranid subfamily Epinephelinae). For these families, we explored whether changes in abundance were related to island type (island vs atoll) and/or declining coral cover (percent change). Carangidae on islands experienced larger changes in abundance than those on atolls, though declines in abundance over time were not associated with changes in live coral cover. In contrast, for Chaetodontidae, declines in abundance over time were most dramatic on atolls, and were also associated with changes in live coral cover. The remoteness of the Phoenix Islands excludes many typical local anthropogenic stressors as drivers of short-term changes; observed changes are instead more likely attributed to natural variation in fish populations, or associated with coral loss following the 2002–2003 major thermal stress event.
Archive | 2011
Les Kaufman; Enric Sala; Stuart A. Sandin; David Obura; Forest Rohwer; John Tschirky
Atoll research bulletin | 2011
David Obura; Gregory Stone; Sangetta Mangubhai; Steven Bailey; Holloway Yoshinaga; Robert Barrel
Atoll research bulletin | 2011
David Obura
Archive | 2012
Gregory Stone; David Obura
Archive | 2011
David Obura; Gerald R. Allen; Gregory Stone; Sangetta Mangubhai; Steven Bailey; Austin Yoshinaga; Cat Holloway; Robert Barrel
Archive | 2008
James E. Maragos; Joyce Miller; Jamison M. Gove; Edward E. DeMartini; Alan M. Friedlander; Scott Godwin; Craig Musburger; Molly A. Timmers; Roy T. Tsuda; Peter S. Vroom; Elizabeth Flint; Emily Lundblad; Jonathan R. Weiss; Paula Ayotte; Enric Sala; Stuart A. Sandin; Sarah McTee; Todd Wass; Daria Siciliano; Russel Brainard; David Obura; Scott Ferguson; Bruce C. Mundy