J. Dorley, J. Singley, T. Covino, K. Singha, M. Gooseff, David Van Horn, R. González‐Pinzón
{"title":"源水流呼吸的物理和化学计量学控制","authors":"J. Dorley, J. Singley, T. Covino, K. Singha, M. Gooseff, David Van Horn, R. González‐Pinzón","doi":"10.5194/bg-20-3353-2023","DOIUrl":null,"url":null,"abstract":"Abstract. Many studies in ecohydrology focusing on hydrologic\ntransport argue that longer residence times across a stream ecosystem should\nconsistently result in higher biological uptake of carbon, nutrients, and\noxygen. This consideration does not incorporate the potential for\nbiologically mediated reactions to be limited by stoichiometric imbalances.\nBased on the relevance and co-dependences between hydrologic exchange,\nstoichiometry, and biological uptake and acknowledging the limited amount\nof field studies available to determine their net effects on the retention\nand export of resources, we quantified how microbial respiration is\ncontrolled by the interactions between and the supply of essential nutrients (C, N, and P)\nin a headwater stream in Colorado, USA. For this, we conducted two rounds of\nnutrient experiments, each consisting of four sets of continuous injections\nof Cl− as a conservative tracer, resazurin as a proxy for aerobic\nrespiration, and one of the following nutrient treatments: (a) N, (b) N+C,\n(c) N+P, or (d) C+N+P. Nutrient treatments were considered to be known\nsystem modifications that alter metabolism, and statistical tests helped\nidentify the relationships between reach-scale hydrologic transport and\nrespiration metrics. We found that as discharge changed significantly\nbetween rounds and across stoichiometric treatments, (a) transient storage\nmainly occurred in pools lateral to the main channel and was proportional to\ndischarge, and (b) microbial respiration remained similar between rounds and\nacross stoichiometric treatments. Our results contradict the notion that\nhydrologic transport alone is a dominant control on biogeochemical\nprocessing and suggest that complex interactions between hydrology, resource\nsupply, and biological community function are responsible for driving\nin-stream respiration.\n","PeriodicalId":8899,"journal":{"name":"Biogeosciences","volume":" ","pages":""},"PeriodicalIF":3.9000,"publicationDate":"2023-08-11","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Physical and stoichiometric controls on stream respiration in a headwater stream\",\"authors\":\"J. Dorley, J. Singley, T. Covino, K. Singha, M. Gooseff, David Van Horn, R. González‐Pinzón\",\"doi\":\"10.5194/bg-20-3353-2023\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Abstract. Many studies in ecohydrology focusing on hydrologic\\ntransport argue that longer residence times across a stream ecosystem should\\nconsistently result in higher biological uptake of carbon, nutrients, and\\noxygen. This consideration does not incorporate the potential for\\nbiologically mediated reactions to be limited by stoichiometric imbalances.\\nBased on the relevance and co-dependences between hydrologic exchange,\\nstoichiometry, and biological uptake and acknowledging the limited amount\\nof field studies available to determine their net effects on the retention\\nand export of resources, we quantified how microbial respiration is\\ncontrolled by the interactions between and the supply of essential nutrients (C, N, and P)\\nin a headwater stream in Colorado, USA. For this, we conducted two rounds of\\nnutrient experiments, each consisting of four sets of continuous injections\\nof Cl− as a conservative tracer, resazurin as a proxy for aerobic\\nrespiration, and one of the following nutrient treatments: (a) N, (b) N+C,\\n(c) N+P, or (d) C+N+P. Nutrient treatments were considered to be known\\nsystem modifications that alter metabolism, and statistical tests helped\\nidentify the relationships between reach-scale hydrologic transport and\\nrespiration metrics. We found that as discharge changed significantly\\nbetween rounds and across stoichiometric treatments, (a) transient storage\\nmainly occurred in pools lateral to the main channel and was proportional to\\ndischarge, and (b) microbial respiration remained similar between rounds and\\nacross stoichiometric treatments. Our results contradict the notion that\\nhydrologic transport alone is a dominant control on biogeochemical\\nprocessing and suggest that complex interactions between hydrology, resource\\nsupply, and biological community function are responsible for driving\\nin-stream respiration.\\n\",\"PeriodicalId\":8899,\"journal\":{\"name\":\"Biogeosciences\",\"volume\":\" \",\"pages\":\"\"},\"PeriodicalIF\":3.9000,\"publicationDate\":\"2023-08-11\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Biogeosciences\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://doi.org/10.5194/bg-20-3353-2023\",\"RegionNum\":2,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"ECOLOGY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Biogeosciences","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.5194/bg-20-3353-2023","RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"ECOLOGY","Score":null,"Total":0}
Physical and stoichiometric controls on stream respiration in a headwater stream
Abstract. Many studies in ecohydrology focusing on hydrologic
transport argue that longer residence times across a stream ecosystem should
consistently result in higher biological uptake of carbon, nutrients, and
oxygen. This consideration does not incorporate the potential for
biologically mediated reactions to be limited by stoichiometric imbalances.
Based on the relevance and co-dependences between hydrologic exchange,
stoichiometry, and biological uptake and acknowledging the limited amount
of field studies available to determine their net effects on the retention
and export of resources, we quantified how microbial respiration is
controlled by the interactions between and the supply of essential nutrients (C, N, and P)
in a headwater stream in Colorado, USA. For this, we conducted two rounds of
nutrient experiments, each consisting of four sets of continuous injections
of Cl− as a conservative tracer, resazurin as a proxy for aerobic
respiration, and one of the following nutrient treatments: (a) N, (b) N+C,
(c) N+P, or (d) C+N+P. Nutrient treatments were considered to be known
system modifications that alter metabolism, and statistical tests helped
identify the relationships between reach-scale hydrologic transport and
respiration metrics. We found that as discharge changed significantly
between rounds and across stoichiometric treatments, (a) transient storage
mainly occurred in pools lateral to the main channel and was proportional to
discharge, and (b) microbial respiration remained similar between rounds and
across stoichiometric treatments. Our results contradict the notion that
hydrologic transport alone is a dominant control on biogeochemical
processing and suggest that complex interactions between hydrology, resource
supply, and biological community function are responsible for driving
in-stream respiration.
期刊介绍:
Biogeosciences (BG) is an international scientific journal dedicated to the publication and discussion of research articles, short communications and review papers on all aspects of the interactions between the biological, chemical and physical processes in terrestrial or extraterrestrial life with the geosphere, hydrosphere and atmosphere. The objective of the journal is to cut across the boundaries of established sciences and achieve an interdisciplinary view of these interactions. Experimental, conceptual and modelling approaches are welcome.