J
John E. Gordon
Researcher at University of St Andrews
Publications - 80
Citations - 3022
John E. Gordon is an academic researcher from University of St Andrews. The author has contributed to research in topics: Geodiversity & Glacier. The author has an hindex of 29, co-authored 77 publications receiving 2409 citations. Previous affiliations of John E. Gordon include Scottish Natural Heritage.
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Geoheritage, Geotourism and the Cultural Landscape: Enhancing the Visitor Experience and Promoting Geoconservation
TL;DR: In this article, a cultural ecosystem services framework is proposed for geotourism, enabling assessment of multiple benefits and trade-offs for visitors and communities based on the values of the geoheritage assets.
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Geodiversity and the ecosystem approach: the contribution of geoscience in delivering integrated environmental management
TL;DR: In this paper, the authors highlight the importance of geodiversity as an important element of natural capital and the need for more integrated approaches to geodesic, biodiversity and landscape conservation and management to enable a more sustainable future.
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The Northwest Forest Plan: Origins, Components, Implementation Experience, and Suggestions for Change
TL;DR: Recognize that the Northwest Forest Plan has evolved into an integrative conservation strategy, conserve old-growth trees and forests wherever they occur and manage federal forests as dynamic ecosystems.
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Why geodiversity matters in valuing nature's stage
TL;DR: It is found that geosites are important to biodiversity because they often support rare or unique biota adapted to distinctive environmental conditions or create a diversity of microenvironments that enhance species richness.
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Magnitude and geographic variation of the radiocarbon content in Antarctic marine life: Implications for reservoir corrections in radiocarbon dating
TL;DR: In this paper, the authors review measurements of 14 C concentrations in modern Antarctic marine life from South Georgia, the Shetland Islands and Antarctic Peninsula and suggest correction factors required to relate radiocarbon measurements on fossil marine materials from these areas to the conventional radiocaran timescale.