{"title":"异养细菌在铵利用、新产量和C0/sub 2/循环中的调节作用","authors":"R. Keil, D. Kirchman","doi":"10.1109/OCEANS.1989.592886","DOIUrl":null,"url":null,"abstract":"Ammonium cycling partly determines nitrate utilization by phytoplankton, new production, and indirectly the exchange of CO2 between the atmosphere and the oceans. trophic bacteria play i.n ammonium cycling is unclear. Investigations in the subarctic Pacific and the midcontinental Atlantic shelf indicate the heterotrophic bacteria consume or regenerate ammonium in response to the supply of dissolved free amino acids. Results of whole water incubations with 15NH4+ indicate that bacteria can consume approximately 30% of the ammonium taken up in subarctic Pacific waters. show that amino acid additions (0.3-1.0 p M ) inhibit uptake of ammonium by bacteria. In 0.8 pm size fractions dominated by heterotrophic bacteria, bacteria regenerated ammonium only when amino acid supply met or exceeded bacterial nitrogen demand. In coastal mid-Atlantic waters, amino acid additions (1.0 p M ) have been shown to inhibit uptake of 15N-Nitrate by phytoplankton. This inhibition is hypothesized to be the result of increased availability of ammonium due to either decreased bacterial utilization or increased bacterial utilization of amino acids and ammonium in part regulates nitrate utilization, and thus indirectly ei'fects new productions, flux of organic matter to the deep ocean, and CO2 cycling. The role hetero-","PeriodicalId":331017,"journal":{"name":"Proceedings OCEANS","volume":"1 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1989-09-18","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Role Of Heterotrophic Bacteria In Regulating Ammonium Utilization, New Production And C0/sub 2/ Cycling\",\"authors\":\"R. Keil, D. Kirchman\",\"doi\":\"10.1109/OCEANS.1989.592886\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Ammonium cycling partly determines nitrate utilization by phytoplankton, new production, and indirectly the exchange of CO2 between the atmosphere and the oceans. trophic bacteria play i.n ammonium cycling is unclear. Investigations in the subarctic Pacific and the midcontinental Atlantic shelf indicate the heterotrophic bacteria consume or regenerate ammonium in response to the supply of dissolved free amino acids. Results of whole water incubations with 15NH4+ indicate that bacteria can consume approximately 30% of the ammonium taken up in subarctic Pacific waters. show that amino acid additions (0.3-1.0 p M ) inhibit uptake of ammonium by bacteria. In 0.8 pm size fractions dominated by heterotrophic bacteria, bacteria regenerated ammonium only when amino acid supply met or exceeded bacterial nitrogen demand. In coastal mid-Atlantic waters, amino acid additions (1.0 p M ) have been shown to inhibit uptake of 15N-Nitrate by phytoplankton. This inhibition is hypothesized to be the result of increased availability of ammonium due to either decreased bacterial utilization or increased bacterial utilization of amino acids and ammonium in part regulates nitrate utilization, and thus indirectly ei'fects new productions, flux of organic matter to the deep ocean, and CO2 cycling. The role hetero-\",\"PeriodicalId\":331017,\"journal\":{\"name\":\"Proceedings OCEANS\",\"volume\":\"1 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"1989-09-18\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Proceedings OCEANS\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.1109/OCEANS.1989.592886\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Proceedings OCEANS","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1109/OCEANS.1989.592886","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
摘要
铵循环在一定程度上决定了浮游植物对硝酸盐的利用和新产量,并间接决定了大气和海洋之间CO2的交换。营养细菌在氨循环中的作用尚不清楚。在亚北极太平洋和大西洋中大陆架的调查表明,异养细菌消耗或再生铵,以响应溶解的游离氨基酸的供应。用15NH4+全水孵育的结果表明,细菌可以消耗亚北极太平洋水域约30%的铵。结果表明,氨基酸添加量(0.3 ~ 1.0 p M)可抑制细菌对铵的吸收。在0.8 pm大小的异养细菌中,只有当氨基酸供应满足或超过细菌对氮的需求时,细菌才能再生铵。在大西洋中部沿海水域,氨基酸添加(1.0 p M)已被证明可以抑制浮游植物对15n -硝酸盐的吸收。这种抑制被认为是由于细菌利用氨基酸的减少或细菌利用氨基酸的增加而增加了铵的可用性,而铵在一定程度上调节了硝酸盐的利用,从而间接影响了新产物、有机物向深海的通量和二氧化碳循环。角色hetero-
Role Of Heterotrophic Bacteria In Regulating Ammonium Utilization, New Production And C0/sub 2/ Cycling
Ammonium cycling partly determines nitrate utilization by phytoplankton, new production, and indirectly the exchange of CO2 between the atmosphere and the oceans. trophic bacteria play i.n ammonium cycling is unclear. Investigations in the subarctic Pacific and the midcontinental Atlantic shelf indicate the heterotrophic bacteria consume or regenerate ammonium in response to the supply of dissolved free amino acids. Results of whole water incubations with 15NH4+ indicate that bacteria can consume approximately 30% of the ammonium taken up in subarctic Pacific waters. show that amino acid additions (0.3-1.0 p M ) inhibit uptake of ammonium by bacteria. In 0.8 pm size fractions dominated by heterotrophic bacteria, bacteria regenerated ammonium only when amino acid supply met or exceeded bacterial nitrogen demand. In coastal mid-Atlantic waters, amino acid additions (1.0 p M ) have been shown to inhibit uptake of 15N-Nitrate by phytoplankton. This inhibition is hypothesized to be the result of increased availability of ammonium due to either decreased bacterial utilization or increased bacterial utilization of amino acids and ammonium in part regulates nitrate utilization, and thus indirectly ei'fects new productions, flux of organic matter to the deep ocean, and CO2 cycling. The role hetero-