{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2026,4,27]],"date-time":"2026-04-27T14:06:13Z","timestamp":1777298773210,"version":"3.51.4"},"reference-count":50,"publisher":"Wiley","issue":"1","license":[{"start":{"date-parts":[[2024,11,30]],"date-time":"2024-11-30T00:00:00Z","timestamp":1732924800000},"content-version":"vor","delay-in-days":0,"URL":"http:\/\/creativecommons.org\/licenses\/by\/4.0\/"}],"content-domain":{"domain":["onlinelibrary.wiley.com"],"crossmark-restriction":true},"short-container-title":["Journal of Phycology"],"published-print":{"date-parts":[[2025,2]]},"abstract":"<jats:title>Abstract<\/jats:title><jats:p>The marine cyanobacterium <jats:italic>Synecococcus<\/jats:italic> sp. (CCMP 1334) was grown in a continuous culture system on a 12:12\u2009h light:dark cycle at all combinations of low and high pCO<jats:sub>2<\/jats:sub> (400 and 1000 ppmv, respectively), nutrient availability (nitrate\u2010limited and nutrient\u2010replete conditions), and temperatures of 21, 24, 28, 32, and 35\u00b0C. The maximum nutrient\u2010replete growth rate was ~1.15\u2009day<jats:sup>\u22121<\/jats:sup> at 32\u201335\u00b0C. Median nutrient\u2010replete growth rates were higher at 1000 ppmv than at 400 ppmv pCO<jats:sub>2<\/jats:sub> at all temperatures. Carbon:nitrogen ratios were independent of pCO<jats:sub>2<\/jats:sub> at a fixed relative growth rate (i.e., growth rate \u00f7 nutrient\u2010replete growth rate) but decreased with increasing temperature. Carbon:chlorophyll <jats:italic>a<\/jats:italic> ratios were decreased monotonically with increasing temperature and were higher under nitrate\u2010limited than nutrient\u2010replete conditions. Ratios of phycoerythrin to chlorophyll <jats:italic>a<\/jats:italic> were independent of growth conditions. Productivity indices were independent of temperature and nutrient limitation but were consistently higher at 1000 ppmv than 400 ppmv pCO<jats:sub>2<\/jats:sub>. Both growth rates and dark respiration rates were positively correlated with temperature, and the associated <jats:italic>Q<\/jats:italic><jats:sub>10<\/jats:sub> values were 2.2 and 2.3, respectively. A model of phytoplankton growth in which cellular carbon is allocated to structure, storage, or the light or dark reactions of photosynthesis accounted for the general patterns of cell composition and growth rate. This strain of <jats:italic>Synechococcus<\/jats:italic> appears well suited to changes in environmental conditions that are expected as the climate warms in response to anthropogenic emissions of CO<jats:sub>2<\/jats:sub>.<\/jats:p>","DOI":"10.1111\/jpy.13531","type":"journal-article","created":{"date-parts":[[2024,11,30]],"date-time":"2024-11-30T16:19:03Z","timestamp":1732983543000},"page":"77-90","update-policy":"https:\/\/doi.org\/10.1002\/crossmark_policy","source":"Crossref","is-referenced-by-count":1,"title":["Interactive effects of <scp>CO<sub>2<\/sub><\/scp>, temperature, and nitrate limitation on the growth and physiology of strain <scp>CCMP<\/scp> 1334 of the marine cyanobacterium <i>Synechococcus<\/i> (Cyanophyceae)"],"prefix":"10.1111","volume":"61","author":[{"given":"Alyssa K.","family":"Sharbaugh","sequence":"first","affiliation":[{"name":"Department of Environmental Sciences Louisiana State University  Baton Rouge Louisiana USA"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"ORCID":"https:\/\/orcid.org\/0000-0002-4893-9311","authenticated-orcid":false,"given":"Edward A.","family":"Laws","sequence":"additional","affiliation":[{"name":"Department of Environmental Sciences Louisiana State University  Baton Rouge Louisiana USA"}],"role":[{"role":"author","vocabulary":"crossref"}]}],"member":"311","published-online":{"date-parts":[[2024,11,30]]},"reference":[{"key":"e_1_2_9_2_1","doi-asserted-by":"publisher","DOI":"10.3389\/fmars.2021.634189"},{"key":"e_1_2_9_3_1","doi-asserted-by":"publisher","DOI":"10.1007\/BF00392580"},{"key":"e_1_2_9_4_1","doi-asserted-by":"publisher","DOI":"10.3390\/su14159508"},{"key":"e_1_2_9_5_1","doi-asserted-by":"publisher","DOI":"10.1080\/17550870903271363"},{"key":"e_1_2_9_6_1","doi-asserted-by":"publisher","DOI":"10.4319\/lo.2008.53.2.0487"},{"key":"e_1_2_9_7_1","doi-asserted-by":"publisher","DOI":"10.1016\/0967-0637(93)90149-W"},{"key":"e_1_2_9_8_1","doi-asserted-by":"publisher","DOI":"10.1029\/2003GB002116"},{"key":"e_1_2_9_9_1","doi-asserted-by":"publisher","DOI":"10.1038\/s41597-022-01196-7"},{"key":"e_1_2_9_10_1","doi-asserted-by":"publisher","DOI":"10.4319\/lo.1965.10.suppl2.r67"},{"key":"e_1_2_9_11_1","volume-title":"Guide for best practices for ocean acidification research and data reporting","author":"Dickson A. 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