The Paleocene-Eocene Thermal Maximum: A perturbation of carbon cycle, climate, and biosphere with implications for the future

FA McInerney, SL Wing - Annual Review of Earth and Planetary …, 2011 - annualreviews.org
During the Paleocene-Eocene Thermal Maximum (PETM),∼ 56 Mya, thousands of
petagrams of carbon were released into the ocean-atmosphere system with attendant …

Implications of reef ecosystem change for the stability and maintenance of coral reef islands

CT Perry, PS Kench, SG Smithers, B Riegl… - Global Change …, 2011 - Wiley Online Library
Coral reef islands are among the most vulnerable environments on Earth to climate change
because they are low lying and largely constructed from unconsolidated sediments that can …

Mutualisms in a changing world: an evolutionary perspective

E Toby Kiers, TM Palmer, AR Ives, JF Bruno… - Ecology …, 2010 - Wiley Online Library
Ecology Letters (2010) 13: 1459–1474 Abstract There is growing concern that rapid
environmental degradation threatens mutualistic interactions. Because mutualisms can bind …

Foraminifera as bioindicators in coral reef assessment and monitoring: the FORAM index

P Hallock, BH Lidz, EM Cockey-Burkhard… - Environmental …, 2003 - Springer
Coral reef communities are threatened worldwide. Resource managers urgently need
indicators of the biological condition of reef environments that can relate data acquired …

Environmental factors influencing skeletal grain sediment associations: a critical review of Miocene examples from the western Mediterranean

L Pomar, M Brandano, H Westphal - Sedimentology, 2004 - Wiley Online Library
The presence of foramol, rhodalgal and bryomol skeletal grain associations in ancient
shallow‐marine limestones is commonly interpreted as evidence for non‐tropical …

Late Paleocene–early Eocene Tethyan carbonate platform evolution—a response to long-and short-term paleoclimatic change

C Scheibner, RP Speijer - Earth-science reviews, 2008 - Elsevier
The early Paleogene experienced the most pronounced long-term warming trend of the
Cenozoic, superimposed by transient warming events such as the Paleocene–Eocene …

Biological mechanisms supporting adaptation to ocean acidification in coastal ecosystems

IE Hendriks, CM Duarte, YS Olsen, A Steckbauer… - Estuarine, Coastal and …, 2015 - Elsevier
The direct influence of anthropogenic CO 2 might play a limited role in pH regulation in
coastal ecosystems as pH regulation in these areas can be complex. They experience large …

Depth coenoclines and environmental considerations of western Pacific larger foraminifera

J Hohenegger - The Journal of Foraminiferal Research, 2004 - pubs.geoscienceworld.org
Symbiont-bearing benthic foraminifera are restricted to the euphotic zone of tropical and
warm-temperate seas. Species distribution is correlated with depth, and the continuous …

Perspective on the response of marine calcifiers to global warming and ocean acidification—Behavior of corals and foraminifera in a high CO2 world “hot house”

H Kawahata, K Fujita, A Iguchi, M Inoue… - Progress in Earth and …, 2019 - Springer
The CO 2 concentration of air has increased over the last two centuries and recently
surpassed 400 ppm. Carbon cycle models project CO 2 concentrations of 720 to 1000 ppm …

Response of large benthic foraminifera to climate and local changes: Implications for future carbonate production

GR Narayan, CE Reymond, M Stuhr, S Doo… - …, 2022 - Wiley Online Library
Large benthic foraminifera are major carbonate components in tropical carbonate platforms,
important carbonate producers, stratigraphic tools and powerful bioindicators (proxies) of …