Microfitoplancton a lo largo de la ruta transpacífica y al norte de la Península Antártica Occidental , Verano Austral 2023-2024

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dc.contributor.advisorTigreros Benavides, Paulo César
dc.contributor.advisorHerrera, Andrés Franco
dc.contributor.advisorNariño Vargas, María José
dc.creatorCalderón Valderrama, Santiago José
dc.date.accessioned2025-11-24T19:41:05Z
dc.date.created2025-11-24
dc.description.abstractEl fitoplancton desempeña un papel esencial al conectar procesos atmosféricos y oceánicos, siendo un eslabón fundamental en las redes tróficas y en la fijación global de carbono. Este estudio, llevado a cabo durante la X Expedición de Colombia a la Antártica en el verano austral 2023-2024, examinó la composición del fitoplancton a lo largo de la ruta transpacífica y en el norte de la Península Antártica Occidental (PAO). Las muestras se recolectaron con botellas Niskin acopladas a una roseta oceanográfica a la profundidad de máxima Chl-a y se fijaron con Lugol. La identificación y cuantificación de los organismos se realizó mediante microscopía invertida aplicando la metodología de Utermöhl. La biomasa de carbono se estimó con los modelos geométricos de Hillebrand et al. (1999) y Sun y Liu (2003) y de acuerdo con la metodología de Menden-Deuer y Lessard (2000). Los resultados indicaron que la ruta transpacífica presentó mayor densidad y biomasa (620 cel/L y 1,78 μg C/L) que el norte de la PAO (170 cel/L y 0,10 μg C/L), con una dominancia de dinoflagelados de 20 a 50 μm (Prorocentrum spp. y Protoperidinium spp.), mientras que en el norte de la PAO predominaron diatomeas céntricas (Thalassiosira spp.) y dinoflagelados atecados de 20 a 30 μm (Gyrodinium spp.). Ambos sectores se vieron afectados por el evento de El Niño 2023-2024 resultando en una reducción de la densidad y biomasa del microfitoplancton con respecto a otros estudios realizados durante otros eventos El Niño, influenciada principalmente por la abundancia más que por el biovolumen.
dc.description.abstractenglishPhytoplankton plays a vital role in linking atmospheric and oceanic processes, being fundamental to the trophic web and global carbon fixation. This study, conducted during the X Colombian Expedition to Antarctica, at austral summer of 2023–2024, examined phytoplankton composition along the transpacific route and in the northern region of the Western Antarctic Peninsula (WAP). Samples were collected at the depth of maximum Chl-a concentration with Niskin bottles and fixed with Lugol solution. Organisms were identified and quantified through inverted microscopy applying the Utermöhl method. Carbon biomass was estimated following the geometric models of Hillebrand et al. (1999) and Sun and Liu (2003), as well as the methodology of Menden-Deuer and Lessard (2000). Results indicated higher density and biomass along the transpacific route (620 cells/L and 1,78 μg C/L), with dominance of dinoflagellates measuring 20–50 μm (Prorocentrum spp. and Protoperidinium spp.), whereas in the northern WAP, centric diatoms (Thalassiosira spp.) and athecate dinoflagellates measuring 20–30 μm (Gyrodinium spp.) predominated. Both regions were affected by the 2023–2024 El Niño event resulting in a reduction in microphytoplankton density and biomass, which was primarily influenced by the abundance rather than their volume.
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dc.identifier.urihttps://hdl.handle.net/20.500.12010/38447
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dc.relation.referencesAnnett, A.L., D.S. Carson, X. Crosta, A. Clarke and R.S. Ganeshram. 2010. Seasonal progression of diatom assemblages in surface waters of Ryder Bay, Antarctica. Polar Biol., 33(1): 13-29. https://doi.org/10.1007/s00300-009-0681-7
dc.relation.referencesAnnett, A.L., M. Skiba, S.F. Henley, H.J. Venables, M.P. Meredith, P.J. Statham and R.S. Ganeshram. 2015. Comparative roles of upwelling and glacial iron sources in Ryder Bay, coastal western Antarctic peninsula. Mar. Chem. 176, 21–33. https://doi. org/10.1016/j.marchem.2015.06.017.
dc.relation.referencesAntoni, J.S., G.O. Almandoz, M.E. Ferrario, M.P. Hernando, D.E. Varela, P.D. Rozema, A.G.J. Buma, F.E. Paparazzo and I.R. Schloss. 2020. Response of a natural Antarctic phytoplankton assemblage to changes in temperature and salinity. J. Exp. Mar. Biol. Ecol., 532: 151444. https://doi.org/10.1016/j.jembe.2020.151444
dc.relation.referencesBalech, E. 1975. Calve ilustrada de dinoflagelados Antárticos. Instituto Antártico Argentino, Buenos Aires. 99 p.
dc.relation.referencesCañón, M. and E. Santamaría. 2021. Identification of phytoplankton blooms in the Gerlache Strait, West Antarctic Peninsula. Bol. Investig. Mar. Cost., 50(SuplEsp): 13-30. https://doi.org/10.25268/bimc.invemar.2021.50.SuplEsp.922
dc.relation.referencesCarvalho, F., J.N. Fitzsimmons, N. Couto, N. Waite, M. Gorbunov, J. Kohut, M.J. Oliver, R.M. Sherrell and O. Schofield. 2020. Testing the Canyon Hypothesis: Evaluating light and nutrient controls of phytoplankton growth in penguin foraging hotspots along the West Antarctic Peninsula. Limnol. Oceanogr., 65(3): 455-470. https://doi.org/10.1002/lno.11313
dc.relation.referencesChisholm, S.W. 1992. Phytoplankton size. 213-237. En: Falkowski, P.G., A.D. Woodhead and K. Vivirito (Eds.). Primary productivity and biogeochemical cycles in the sea. Springer, US. https://doi.org/10.1007/978-1-4899-0762-2_12
dc.relation.referencesClarke, K.R. and R.N. Gorley. 2006. Primer v6: User Manual/Tutorial. PRIMER-E Limited. 190.
dc.relation.referencesClarke, K.R. and R.M. Warwick. 2001. Change in marine communities: An approach to statistical analysis and interpretation. PRIMER-E Limited. 174.
dc.relation.referencesCosta, R.R., C.R.B. Mendes, A. Ferreira, V.M. Tavano, T.S. Dotto and E.R. Secchi. 2021. Large diatom bloom off the Antarctic Peninsula during cool conditions associated with the 2015/2016 El Niño. Commun. Earth Environ., 2(1): 252. https://doi.org/10.1038/s43247-021-00322-4
dc.relation.referencesDe La Hoz Barrientos, L.A., M.L. Cañón y D. Rojas. 2020. Estructura y distribución de la comunidad fitoplanctónica a lo largo del Estrecho de Gerlache durante el verano austral 2018-2019. Bol. Cient. CIOH., 39(1): 25-39. https://doi.org/10.26640/22159045.2020.501
dc.relation.referencesDelfina, R. 2004. Las corrientes de Humboldt y «El Niño» sus repercusiones en el ambiente. Rev. Geogr., 135: 95-114. https://doi.org/10.2307/40996681
dc.relation.referencesDelgado, E., S. Sánchez, F. Chang, P. Villanueva y C. Fernández. 2015. Fitoplancton del mar peruano en la primavera austral 2002. Inf. Inst. Mar. Perú, 42(2): 143-149.
dc.relation.referencesFalkowski, P.G., M.E. Katz, A.H. Knoll, A. Quigg, J.A. Raven, O. Schofield and F.J.R. Taylor. 2004. The evolution of modern eukaryotic phytoplankton. Science, 305(5682): 354-360. https://doi.org/10.1126/science.1095964
dc.relation.referencesFalkowski, P.G. and J.A. Raven. 1997. Aquatic photosynthesis. Blackwell science. 375 p. https://doi.org/10.1093/jxb/49.320.621
dc.relation.referencesFerrario, M.E., G. Almandoz, S. Licea, I. Garibotti. 2008. Species of Coscinodiscus (Bacillariophyta) from the Gulf of Mexico, Argentina and Antarctic waters: morphology and distribution. Nova Hedwigia, 133: 187-216. ISNN: 00295035.
dc.relation.referencesFigueroa, F.L. 2002. Bio-optical characteristics of Gerlache and Bransfield Strait waters during an Antarctic summer cruise. Deep Sea Res. Part II Topi. Stud. Oceanogr., 49(4-5): 675-691. https://doi.org/10.1016/S0967-0645(01)00118-7
dc.relation.referencesGarcı́a, M.A., C.G. Castro, A.F. Rı́os, M.D. Doval, G. Rosón, D. Gomis and O. López. 2002. Water masses and distribution of physico-chemical properties in the Western Bransfield Strait and Gerlache Strait during Austral summer 1995/96. Deep Sea Res. Part II Top. Stud. Oceanogr., 49(4-5): 585-602. https://doi.org/10.1016/S0967-0645(01)00113-8
dc.relation.referencesGardiner, W., A.E. Rushing and C.J. Dawes. 1988. Ultrastructural observations of Gyrodinium estuariale (Dinophyceae). J. Phycol., 25: 178-183. https://doi.org/10.1111/j.0022-3646.1989.00178.x
dc.relation.referencesGaribotti, I.A., M. Vernet and M.E. Ferrario. 2005. Annually recurrent phytoplanktonic assemblages during summer in the seasonal ice zone west of the Antarctic Peninsula (Southern Ocean). Deep Sea Res. Part I Oceanogr. Res. Pap., 52(10): 1823-1841. https://doi.org/10.1016/j.dsr.2005.05.003
dc.relation.referencesGaribotti, I., M. Vernet, M. Ferrario, R. Smith, R. Ross and L. Quetin. 2003. Phytoplankton spatial distribution patterns along the western Antarctic Peninsula (Southern Ocean). Mar. Ecol. Prog. Ser., 261: 21-39. https://doi.org/10.3354/meps261021
dc.relation.referencesGleick, P.H., N. Ajami, J. Christian-Smith, H. Cooley, K. Donnelly, J. Fulton, M. Ha, M. Heberger, E. Moore, J. Morrison, S. Orr, P. Schulte, V. Srinivasan. 2014. The world's water. Island Press, Washington D.C. (430 p.).
dc.relation.referencesGómez, F. 2021. Speciation and infrageneric classification in the planktonic Dinoflagellate Tripos (Gonyaulacales, Dinophyceae). Curr. Chin. Sci., 1(3): 346-372. http://dx.doi.org/10.2174/2210298101999210101231020
dc.relation.referencesGómez, F., D. Moreira and P. López-García. 2010. Molecular phylogeny of the dinoflagellates and Blepharocysta (Peridiniales, Dinophyceae). Phycologia, 49(3): 212-220. https://doi.org/10.2216/PH09-29.1
dc.relation.referencesGómez, F., H. Claustre, P. Raimbault and S. Souissi. 2007. Two high-nutrient low-chlorophyl phytoplankton assemblages: the tropical central Pacific and the offshore Perú-Chile Current. Biogeosciences, 4: 1101-1113.
dc.relation.referencesGómez, F., H. Claustre and S. Souissi. 2008. Rarely reported dinoflagellates of the genera Ceratium, Gloeodinium, Histioneis, Oxytoxum and Prorocentrum (Dinophyceae) from the open southeast Pacific Ocean. Rev. Biol. Mar. Oceanogr., 43(1): 25-40. https://doi.org/10.4067/S0718-19572008000100004
dc.relation.referencesGrados, C., A. Chaigneau, V. Echevin and N. Dominguez. 2018. Upper ocean hydrology of the Northern Humboldt Current System at seasonal, interannual and interdecadal scales. Prog. Oceanogr., 165: 123-144. https://doi.org/10.1016/j.pocean.2018.05.005
dc.relation.referencesGutiérrez, D., K. Aronés, F. Chang, L. Quipúzcoa and P. Villanueva. 2005. Impacto de la Impacto de la variación oceanográfica estacional e interanual sobre los ensambles de microfitoplancton, mesozooplancton, ictioplancton y macrozoobentos de dos áreas costeras del norte del Perú entre 1994 y 2002. Bol. Inst. Mar Perú, 22(1-2): 0378 – 7699.
dc.relation.referencesHenley, S., O. Schofield, K. Hendry, I. Schloss, D. Steinberg, C. Moffat, L. Peck, D. Costa, D.C.E. Bakker, C. Hughes, P. Rozema, H. Ducklow, D. Abele, J. Stefels, M. van Leeuwe, C. Brussaard, A.G.J. Buma, J. Kohut, R. Sahade, A. Friedlaender, H. Venables and M. Meredith. 2019. Variability and change in the West Antarctic peninsula marine system: research priorities and opportunities. Prog. Oceanogr. 173: 208–237. https://doi.org/10.1016/j.pocean.2019.03.003
dc.relation.referencesHernando, M., I.R. Schloss, G. Malanga, G.O. Almandoz, G.A. Ferreyra, M.B. Aguiar and S. Puntarulo. 2015. Effects of salinity changes on coastal Antarctic phytoplankton physiology and assemblage composition. J. Expe. Mar. Biol. Ecol., 466: 110-119. https://doi.org/10.1016/j.jembe.2015.02.012
dc.relation.referencesHillebrand, H., C. Dürselen, D. Kirschtel, U. Pollingher and T. Zohary. 1999. Biovolumen calculation for pelagic and benthic microalgae. J. Phycol., 35(2): 403-424. https://doi.org/10.1046/j.1529-8817.1999.3520403.x
dc.relation.referencesHo, K.C. S.H. Kang, I.H.Y. Lam and I.J. Hodgkiss. 2003. Distribution of Alexandrium tamarense in Drake Passage and the threat of harmful algal blooms in the Antarctic Ocean. Ocean Polar Res., 25(4): 625-631. https://doi.org/10.4217/OPR.2003.25.4.625
dc.relation.referencesIriarte, J. and H. González. 2004. Phytoplankton size structure during and after the 1997/98 El Niño in a coastal upwelling area of the northern Humboldt Current System. Mar. Ecol. Prog. Ser., 269: 83-90. https://doi.org/10.3354/meps269083
dc.relation.referencesJacob, B.G., F.J. Tapia, R.A. Quiñones, R. Montes, M. Sobarzo, W. Schneider, G. Daneri, C.E. Morales, P. Montero and H.E. González. 2018. Major changes in diatom abundance, productivity, and net community metabolism in a windier and dryer coastal climate in the southern Humboldt Current. Prog. Oceanogr., 168: 196-209. https://doi.org/10.1016/j.pocean.2018.10.001
dc.relation.referencesJeong, H.J., Y.D. Yoo, J.S. Kim, K.A. Seong, N.S. Kang and T.H. Kim. 2010. Growth, feeding and ecological roles of the mixotrophic and heterotrophic Dinoflagellates in marine planktonic food webs. Ocean Sci. J. 45(2): 65-91. https://doi.org/10.1007/s12601-010-0007-2
dc.relation.referencesJia, J., Y. Gao, K. Sun, Y. Lu, J. Wang and K. Shi. 2022. Phytoplankton community composition, carbon sequestration, and associated regulatory mechanism in a floodplain lake system. Environ. Pollut., 306(1): 119411. https://doi.org/10.1016/j.envpol.2022.119411
dc.relation.referencesKerr, R., I.B.M. Orselli, J.M. Lencina-Avila, R.T. Eidt, C.R.B. Mendes, L.C. Da Cunha, C. Goyet, M.M. Mata and V.M. Tavano. 2018. Carbonate system properties in the Gerlache Strait, Northern Antarctic Peninsula (February 2015): I. Sea–Air CO2 fluxes. Deep Sea Res. Part II Top. Stud. Oceanogr., 149: 171-181. https://doi.org/10.1016/j.dsr2.2017.02.008
dc.relation.referencesKim, H., H.W. Ducklow, D. Abele, E.M. Ruiz, A.G.J. Buma, M.P. Meredith, P.D. Rozema, O.M. Schofield, H.J. Venables and I.R. Schloss. 2018. Inter-decadal variability of phytoplankton biomass along the coastal West Antarctic Peninsula. Philos. Trans. R. Soc. A Math. Phys. Eng. Sci. 376(2122). 20170174. https://doi.org/ 10.1098/rsta.2017.0174.
dc.relation.referencesKownacka, J., L. Edler, S. Gromisz, M. Lotocka, I. Olenina, M. Ostrowska and K. Piwosz. 2013. Non-indigenous species Chaetoceros cf. lorenzianus Grunow 1863 – a new, predominant component of autumn phytoplankton in the southern Baltic Sea. Estuar. Coast. Shelf Sci., 119: 101-111. https://doi.org/10.1016/j.ecss.2013.01.010
dc.relation.referencesLegendre, P. and L. Legendre. 2012. Numerical ecology. Elsevier. 1006. ISBN: 9780444538680
dc.relation.referencesMarañón, E. 2009. Phytoplankton size structure (445-452). En: Encyclopedia of Ocean Sciences. Elsevier. https://doi.org/10.1016/B978-012374473-9.00661-5
dc.relation.referencesMarañón, E. 2015. Cell size as a key determinant of phytoplankton metabolism and community structure. Annu. Rev. Mar. Sci., 7(1): 241-264. https://doi.org/10.1146/annurev-marine-010814-015955
dc.relation.referencesMascioni, M., G.O. Almandoz, A.O. Cefarelli, A. Cusick, M.E. Ferrario and M. Vernet. 2019. Phytoplankton composition and bloom formation in unexplored nearshore waters of the western Antarctic Peninsula. Polar Biol., 42(10): 1859-1872. https://doi.org/10.1007/s00300-019-02564-7
dc.relation.referencesMascioni, M., G.O. Almandoz, A. Cusick, B.J. Pan and M. Vernet. 2023. Phytoplankton dynamics in nearshore regions of the western Antarctic Peninsula in relation to a variable frontal zone in the Gerlache Strait. Front. Mar. Sci., 10: 1139293. https://doi.org/10.3389/fmars.2023.1139293
dc.relation.referencesMenden-Deuer, S. and E.J. Lessard. 2000. Carbon to volume relationships for dinoflagellates, diatoms, and other protist plankton. Limnol. Oceanogr., 45(3): 569-579. https://doi.org/10.4319/lo.2000.45.3.0569
dc.relation.referencesMendes, C.R.B., V.M. Tavano, T.S. Dotto, R. Kerr, M.S. De Souza, C.A.E. Garcia and E.R. Secchi. 2018. New insights on the dominance of cryptophytes in Antarctic coastal waters: A case study in Gerlache Strait. Deep Sea Res. Part II Top. Stud. Oceanogr., 149: 161-170. https://doi.org/10.1016/j.dsr2.2017.02.010
dc.relation.referencesMontecinos V. and J. Orlando. 2022. Ciencias ecológicas. 1983-2013. Editorial Universitaria de Chile, Santiago de Chile. 332 p.
dc.relation.referencesMontecino V., M.A. Paredes, C. Vargas, M. Manley and G. Pizarro. 2003. Composición por tamaños del fitoplancton, abundancia de clorofila y gradientes de productividad primaria en la región de Aysén noviembre 2002. Resultados del Crucero CIMAR 8 Fiordos. Comité Oceanográfico Nacional, Valparaíso. Libro de Resúmenes: 123-137.
dc.relation.referencesMorales, C.E. and V. Anabalón. 2012. Phytoplankton biomass and microbial abundances during the spring upwelling season in the coastal area off Concepción, central-southern Chile: Variability around a time series station. Prog. Oceanogr., 92(95): 81-91. https://doi.org/10.1016/j.pocean.2011.07.004
dc.relation.referencesMoreno, C.E. 2001. Métodos para medir la biodiversidad. M&T-Manuales y Tesis. Sociedad Entomológica Aragonesa (SEA), Zaragoza. 84 p.
dc.relation.referencesNardelli, S.C., P.C. Gray, S.E. Stammerjohn and O. Schofield. 2023. Characterizing coastal phytoplankton seasonal succession patterns on the West Antarctic Peninsula. Limnol. Oceanogr., 68(4): 845-861. https://doi.org/10.1002/lno.12314
dc.relation.referencesNational Oceanic and Atmospheric Administration (NOAA). 2025. Multivariate ENSO Index (MEI) v2. https://psl.noaa.gov/enso/mei/. [31/07/2025].
dc.relation.referencesNational Oceanic and Atmospheric Administration (NOAA). 2025. Oceanic Niño Index (ONI). https://origin.cpc.ncep.noaa.gov/products/analysis_monitoring/ensostuff/ONI_v5.php. [31/07/2025].
dc.relation.referencesNowacek D.P., A.S. Friedlaender, P.N. Halpin, E.L. Hazen, D.W. Johnston, A.J. Read, B. Espinasse, M. Zhou and Y. Zhu. 2011. Super-Aggregations of Krill and Humpback Whales in Wilhelmina Bay, Antarctic Peninsula. PLoS ONE, 6(4): e19173. https://doi.org/10.1371/journal.pone.0019173
dc.relation.referencesOrsi, A.H., T. Whitworth and W.D. Nowlin. 1995. On the meridional extent and fronts of the antarctic circumpolar current. Deep Sea Res. Part I Oceanogr. Res. Pap., 42(5): 641–673. https://doi.org/10.1016/0967-0637(95)00021-W
dc.relation.referencesPesantes, F. 2014. Dinoflagelados del fitoplancton del Golfo de Guayaquil. Acta. Oceanogr. Pac., 19(1): 91-207. http://hdl.handle.net/1834/8292
dc.relation.referencesPetrou, K., S.A. Kranz, S. Trimborn, C.S. Hassler, S.B. Ameijeiras, O. Sackett, P.J. Ralph and A.T. Davidson. 2016. Southern Ocean phytoplankton physiology in a changing climate. J. Plant Physiol., 203: 135-150. https://doi.org/10.1016/j.jplph.2016.05.004
dc.relation.referencesPrézelin, B.B., E.E. Hofmann, C. Mengelt and J.M. Klinck. 2000. The linkage between Upper Circumpolar Deep Water (UCDW) and phytoplankton assemblages on the west Antarctic Peninsula continental shelf. J. Mar. Res., 58(2): 165-202. https://doi.org/10.1357/002224000321511133
dc.relation.referencesRintoul, S., C. Hughes and D. Olbers. 2001. Chapter 4.6 The Antarctic circumpolar current system. Int. Geophys., 77: 271-302. https://doi.org/10.1016/S0074-6142(01)80124-8
dc.relation.referencesReynolds, C.S. 2006. Chapter 8 Phytoplankton ecology and aquatic ecosystem: mechanisms and management. 397-436. En: The ecology of phytoplankton (1.a ed.). Cambridge University Press. 614 p. https://doi.org/10.1017/CBO9780511542145
dc.relation.referencesRiquelme-Bugueño, R., S. Pantoja-Gutiérrez, E. Jorquera, V. Anabalón, B. Srain and W. Schneider. 2020. Fatty acid composition in the endemic Humboldt Current krill, Euphausia mucronata (Crustacea, Euphausiacea) in relation to the phytoplankton community and oceanographic variability off Dichato coast in central Chile. Prog. Oceanogr., 188: 102425. https://doi.org/10.1016/j.pocean.2020.102425
dc.relation.referencesRodríguez, F., M. Chauton, G. Johnsen, K. Andresen, L.M. Olsen and M. Zapata. 2006. Photoacclimation in phytoplankton: implications for biomass estimates, pigment functionality and chemotaxonomy. Mar. Bio. 148: 963-971. https://doi.org/10.1007/s00227-005-0138-7
dc.relation.referencesRStudio Team. 2023. RStudio: Integrated Development Environment for R. Posit Software, PBC, Boston, M.A.
dc.relation.referencesR Core Team. 2023. R: language and environment for statistical computing. R Foundation for Statistical Computing, Vienna, Austria
dc.relation.referencesSchofield, O., G. Saba, K. Coleman, F. Carvalho, N. Couto, H. Ducklow, Z. Finkel, A. Irwin, A. Kahl, T. Miles, M. Montes-Hugo, S. Stammerjohn and N. Waite. 2017. Decadal variability in coastal phytoplankton community composition in a changing West Antarctic Peninsula. Deep Sea Res. Part I Oceanogr. Res. Pap., 124: 42-54. https://doi.org/10.1016/j.dsr.2017.04.014
dc.relation.referencesSchofield, O., H.W. Ducklow, D.G. Martinson, M.P. Meredith, M.A. Moline and M.R. Fraser. 2010. How do polar marine ecosystems respond to rapid climate change? Science, 328(5985): 1520-1523. 10.1126/science.1185779
dc.relation.referencesSmayda, T.J. 1997. Harmful algal blooms: Their ecophysiology and general relevance to phytoplankton blooms in the sea. Limnol. Oceanogr., 42: 1137-1153. https://doi.org/10.4319/lo.1997.42.5_part_2.1137
dc.relation.referencesScott, F. and H.J. Marchant. 2005. Antarctic Marine Protist. Australian Biological Resources Study, Canberra. 563 p.
dc.relation.referencesSu, Z., Z. Zhang, Y. Zhu and M. Zhou. 2022. Long-term warm-cold Phase Shifts in the Gerlache Strait, Western Antarctic Peninsula. Front. Mar. Sci. 9: 877043. https://doi.org/10.3389/fmars.2022.877043
dc.relation.referencesSun, J., and D. Liu. 2003. Geometric models for calculating cell biovolume and surface area for phytoplankton. J. Plank. Res., 25(11): 1331-1346. https://doi.org/10.1093/plankt/fbg096
dc.relation.referencesTarazona, J. and W. Arntz. 2001. The Peruvian Coastal Upwelling System (229-244). En: Seeliger, U. and B. Kjerfve (Eds.). Coastal Marine Ecosystems of Latin America. Springer Berlin Heidelberg. https://doi.org/10.1007/978-3-662-04482-7_17
dc.relation.referencesTaylor, L.R. 1961. Aggregation, variance and the mean. Nature, 189(4766): 732-735. https://doi.org/10.1038/189732a0
dc.relation.referencesTomas, C.R. 1997. Identifying marine phytoplankton. Academic Press, St. Petersburg. 859 p. https://doi.org/10.1016/B978-0-12-693018-4.X5000-9
dc.relation.referencesTorres, R.R., A.L. Caicedo and J.D. Iriarte. 2020. Hydrographic conditions during two austral summer situations (2015 and 2017) in the Gerlache and Bismarck straits, northern Antarctic Peninsula. Deep Sea Res. Part I Oceanogr. Res. Pap., 161: 103278. https://doi.org/10.1016/j.dsr.2020.103278
dc.relation.referencesTorstensson, A., C. Jiménez, A.K. Nilsson and A. Wulff. 2019. Elevated temperature and decreased salinity both affect the biochemical composition of the Antarctic sea-ice diatom Nitzschia lecointei, but not increased pCO2. Polar Biol., 42(11): 2149-2164. https://doi.org/10.1007/s00300-019-02589-y
dc.relation.referencesTukey, J.W. 1977. Exploratory data analysis. Addison-Wesley pub. Co. 688 p. ark:/13960/t76t97d30
dc.relation.referencesTurk, D., C.S. Meinen, D. Antoine, M.J. McPhaden and M.R. Lewis. 2011. Implications of changing El Niño patterns for biological dynamics in the equatorial Pacific Ocean. Geophys. Res. Lett., 38(23): L23603. http://dx.doi.org/10.1029/2011GL049674
dc.relation.referencesUtermöhl, H. 1958. Zur Vervollkommnung der quantitativen Phytoplankton-Methodik: Mit 1 Tabelle und 15 abbildungen im Text und auf 1 Tafel. Mitt. Int. Ver. Theor. Angew. Limnol., 9(1): 1-38. https://doi.org/10.1080/05384680.1958.11904091
dc.relation.referencesVarela, M., E. Fernandez and P. Serret. 2002. Size-fractionated phytoplankton biomass and primary production in the Gerlache and south Bransfield Straits (Antarctic Peninsula) in Austral summer 1995–1996. Deep Sea Res. Part II Top. Stud. Oceanogr., 49(4-5): 749-768. https://doi.org/10.1016/S0967-0645(01)00122-9
dc.relation.referencesVernet, M., D. Martinson, R. Iannuzzi, S. Stammerjohn, W. Kozlowski, K. Sines, R. Smith and I. Garibotti. 2008. Primary production within the sea-ice zone west of the Antarctic Peninsula: I-Sea Ice, mixed layer, and irradiance. Deep Sea Res. Part II Top. Stud. Oceanogr., 55(18-19): 2068-2085. https://doi.org/10.1016/j.dsr2.2008.05.021
dc.relation.referencesWang, B., M. Chen, F. Chen, R. Jia, X. Li, M. Zheng and Y. Qiu. 2020. Meteoric water promotes phytoplankton carbon fixation and iron uptake off the eastern tip of the Antarctic peninsula (eAP). Prog. Oceanogr. 185: 102347. https://doi.org/10.1016/j. pocean.2020.102347
dc.relation.referencesZar, J.H. 2010. Biostatistical analysis (5.a ed) Prentice-Hall. Upper Saddle River, USA. 946 p.
dc.relation.referencesAtkinson, D. 1994. Temperature and organism size – a biological law for ectotherms? 1-58. En: Advances in ecological research, Elsevier, 25 p.
dc.relation.referencesBergmann, C. 1847. Über die Verhältnisse der Wärmeökonomie der Thiere zu ihrer Grösse. Göttingen: Vandenhoeck und Ruprecht. 3: 538-545.
dc.relation.referencesBertrand A., M. Lengaigne, K. Takahashi, A. Avadí, F. Poulain and C. Harrod. 2020. El Niño Southern Oscillation (ENSO) effects on fisheries and aquaculture. FAO Fish Aquac. Tech. Pap. 660:1–84. https://doi.org/10.4060/ca8348en
dc.relation.referencesCanfield, D.E., R.W. Bachmann, M.V. Hoyer, L.S. Johansson, M. Søndergaard and E. Jeppesen. 2019. To measure chlorophyll or phytoplankton biovolume: an aquatic conundrum with implications for the management of lakes. Lake Reserv. Manag., 35(2): 181-192. https://doi.org/10.1080/10402381.2019.1607958
dc.relation.referencesCloern, J.E., T.S. Schraga, E. Nejad and T. Eddy. 2023. Phytoplankton as indicators of global warming? Limnol. Oceanogr. Lett., 9: 199-208. https://doi.org/10.1002/lol2.10354
dc.relation.referencesCook, J., B.R. Stuparyk, M.A. Johnsen and R.D. Vinebrooke. 2020. Concordance of chemically inferred and assayed nutrient limitation of phytoplankton along a depth gradient of alpine lakes in the Canadian Rockies. Aquat. Sci. 82(17): 1-17
dc.relation.referencesDucklow, H.W., D.K. Steinberg and K.O. Buesseler. 2001. Upper ocean carbon export and the biological pump. Oceanogr. 14(4): 50-58.
dc.relation.referencesFelip, M. and J. Catalan. 2000. The relationship between phytoplankton biovolume and chlorophyll in a deep oligotrophic lake: decoupling in their spatial and temporal maxima. J. Plankton Res., 22(1): 91-106. https://doi.org/10.1093/plankt/22.1.91
dc.relation.referencesFranco, K.V.C., J.J. Selvaraj y A.I.G. Alvis. 2012. Efecto del fenómeno de El Niño en la productividad primaria en el Pacífico colombiano. Acta Agronómica, 61(5), 7-8.
dc.relation.referencesForsch K.O., L. Hahn-Woernle, R.M. Sherrell, V.J. Roccanova, K. Bu, D. Burdige, M. Vernet and K.A. Barbeau. 2021. Seasonal dispersal of fjord meltwaters as an important source of iron and manganese to coastal Antarctic phytoplankton. Biogeosciences, 18(23): 6349–6375. doi:10.5194/bg-18-6349-2021
dc.relation.referencesGutiérrez, D., M. Akester and L. Naranjo. 2016. Productivity and sustainable management of the Humbolt Current large marine ecosystem under climate change. Environ. Dev., 17(1): 126-144. https://doi.org/10.1016/j.envdev.2015.11.004
dc.relation.referencesHays, G.C., A.J. Richardson and C. Robinson. 2005. Climate change and marine plankton. Trends Ecol. Evol. 20: 337-344.
dc.relation.referencesMcnair, H., C.N. Hammond and S. Menden-Deuer. 2021. Phytoplankton carbon and nitrogen biomass estimates are robust to volume measurement method and growth environment. J. Plankton Res., 43(2): 103-112. https://doi.org/10.1093/plankt/fbab014
dc.relation.referencesMontes-Hugo, M., S.C. Doney, H.W. Ducklow, W. Fraser, D. Martinson, S.E. Stammerjohn and O. Schofield. 2009. Recent changes in phytoplankton communities associated with rapid regional climate change along the Western Antarctic Peninsula. Science, 323: 1470-1473. https://doi.org/10.1126/science.1164533
dc.relation.referencesPan B.J., M.M. Gierarch, S. Stammerjohn, O. Schofield, M.P. Meredith, R.A. Reynolds, M. Vernet, F.A. Haumann, A.J. Orona and C.E. Miller. 2025. Impact of glacial meltwater on phytoplankton biomass along the Western Antarctic Peninsula. Commun. Earth. Environ., 6(456). doi:10.1038/s43247-025-02435-6
dc.relation.referencesSalmoso, N., M. Tolotti. 2021. Phytoplankton and anthropogenic changes in pelagic environments. Hydrobiologia, 848: 251-284. https://doi.org/10.1007/s10750-020-04323-w
dc.relation.referencesSommer, U., H. Stibor, A. Katechakis, F. Sommer and T. Hansen. 2002. Pelagic food web configurations at different levels of nutrient richness and their implications for the ratio fish production:primary production. Hydrobiologia. 484: 11–20.
dc.relation.referencesSommer, U., K.H. Peter, S. Genitsaris and M. Moustaka-gouni. 2017. Do marine phytoplankton follow Bergmann’ s rule sensu lato? Biol. Rev. 92: 1011-1026.
dc.relation.referencesStoer, A.C. and K. Fennel. 2024. Carbon-centric dynamics of earth’s marine phytoplankton. Proc. Natl. Acad. Sci., 121(45): e2405354121. https://doi.org/10.1073/pnas.2405354121
dc.relation.referencesVenables, H.J., A. Clarke and M.P. Meredith. 2013. Wintertime controls on summer stratification and productivity at the western Antarctic Peninsula. Limnol. Oceanogr., 58(3): 1035-1047. https://doi.org/10.4319/lo.2013.58.3.1035
dc.relation.referencesZheng, X., Y. Bai, Y. Zhang, X. He, T. Li and F. Gong. 2025. Diversity mechanisms of long-term changes in phytoplankton biomass and productivity in the Southern Ocean: comparison in the Amundsen and Cosmonaut Seas. Front. Mar. Sci., 12: 1547082. https://doi.org/10.3389/fmars.2025.1547082
dc.subjectRuta transpacífica Antártica
dc.subjectBiomasa
dc.subjectAbundancia
dc.subjectBiovolumen
dc.subject.keywordTrans-pacific route
dc.subject.keywordAntarctic
dc.subject.keywordBiomass
dc.subject.keywordAbundance
dc.subject.keywordBiovolume
dc.subject.lembFitoplancton - Análisis
dc.subject.lembBiomasa marina - Evaluación
dc.subject.lembCambio climático - Impacto en organismos marinos
dc.titleMicrofitoplancton a lo largo de la ruta transpacífica y al norte de la Península Antártica Occidental , Verano Austral 2023-2024
dc.type.coarhttp://purl.org/coar/resource_type/c_7a1f

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