‘One physical system’: Tansley's ecosystem as Earth's critical zone

• Published in: The New phytologist 2015-05, Vol.206 (3), p.900-912
• Main Authors: Richter, Daniel deB, Billings, Sharon A
• Format: Article
• Language: English
• Subjects: Biogeochemistry; biogeosciences; Biosphere; carbon; Carbon dioxide; Carbon Dioxide - metabolism; Carbonic acid; Catchment area; Catchments; Diffusion rate; Dimensions; Earth; Earth Sciences - history; Earth Sciences - trends; Earth, Planet; ecohydrology; Ecosystem; ecosystem ecology; ecosystem metabolism; Ecosystem structure; Ecosystems; energy; evolution; History, 20th Century; History, 21st Century; landscapes; Metabolism; Microbial activity; microbial communities; Microorganisms; River basins; Soil; Soil - chemistry; Soil formation; soil respiration; Streams; Structure-function relationships; Tansley reviews; Terrestrial ecosystems; Terrestrial environments; Watersheds; Weathering; weathering profile
• ISSN: 0028-646X; 1469-8137
• DOI: 10.1111/nph.13338

900 I. 900 II. 901 III. 901 IV. 902 V. 905 VI. 908 909 References 909 SUMMARY: Integrative concepts of the biosphere, ecosystem, biogeocenosis and, recently, Earth's critical zone embrace scientific disciplines that link matter, energy and organisms in a systems‐level understanding of our remarkable planet. Here, we assert the congruence of Tansley's (1935) venerable ecosystem concept of ‘one physical system’ with Earth science's critical zone. Ecosystems and critical zones are congruent across spatial–temporal scales from vegetation‐clad weathering profiles and hillslopes, small catchments, landscapes, river basins, continents, to Earth's whole terrestrial surface. What may be less obvious is congruence in the vertical dimension. We use ecosystem metabolism to argue that full accounting of photosynthetically fixed carbon includes respiratory CO₂and carbonic acid that propagate to the base of the critical zone itself. Although a small fraction of respiration, the downward diffusion of CO₂helps determine rates of soil formation and, ultimately, ecosystem evolution and resilience. Because life in the upper portions of terrestrial ecosystems significantly affects biogeochemistry throughout weathering profiles, the lower boundaries of most terrestrial ecosystems have been demarcated at depths too shallow to permit a complete understanding of ecosystem structure and function. Opportunities abound to explore connections between upper and lower components of critical‐zone ecosystems, between soils and streams in watersheds, and between plant‐derived CO₂and deep microbial communities and mineral weathering.