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Siliceous microfossil record of late Holocene oceanography and climate along the west coast of Vancouver Island, British Columbia (Canada)

Published online by Cambridge University Press:  20 January 2017

Murray B. Hay ,
Audrey Dallimore ,
Richard E. Thomson ,
Stephen E. Calvert  and
Reinhard Pienitz
Murray B. Hay*
Affiliation:
Paleolimnology-Paleoecology Laboratory, Département de géographie et Centre d’études nordiques, Université Laval, Québec City (Québec), Canada G1K 7P4
Audrey Dallimore
Affiliation:
Pacific Geoscience Center, Geological Survey of Canada, Sidney, British Columbia, Canada V8L 4B2
Richard E. Thomson
Affiliation:
Department of Fisheries and Oceans, Institute of Ocean Sciences, Sidney, British Columbia, Canada V8L 4B2
Stephen E. Calvert
Affiliation:
Department of Earth and Ocean Sciences, University of British Columbia, 6270 University Boulevard, Vancouver, British Columbia, Canada V6T 1Z4
Reinhard Pienitz
Affiliation:
Paleolimnology-Paleoecology Laboratory, Département de géographie et Centre d’études nordiques, Université Laval, Québec City (Québec), Canada G1K 7P4
*
⁎Corresponding author. Fax: +1 418 656 2978. E-mail address:[email protected] (M.B. Hay).
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Abstract

Diatoms, silicoflagellates, and biogenic silica (BSi) were analyzed from two piston cores recovered from Effingham Inlet, British Columbia. Relatively productive marine conditions from 4850 to 4000 cal yr BP were followed by a transition to the modern ocean–climate regime marked by a decreased siliceous microfossil production since 2800 cal yr BP. This change in the northeast Pacific climate was characterized by an apparent cooling associated with higher rainfall and lower light levels. The reduced abundance of most spring–summer bloom diatom taxa (Skeletonema–Thalassiosira–Chaetoceros) was coupled with a decreased abundance of diatoms normally associated with incursions of offshore water into coastal inlets. This pattern reflected a weaker summer upwelling along Vancouver Island associated with the insolation-related increase in the strength of the Aleutian Low and a weakened North Pacific High. After ca. 2800 cal yr BP, diatom assemblages also indicated more frequent periods of relatively low spring–summer surface water salinity and a disruption of the typical bloom sequence, indicative of increased climatic variability. A period of warmer and drier climate conditions and possibly increased coastal upwelling offshore occurred ca. 1450–1050 cal yr BP. The most recent 500 yr are marked by reduced diatom production and the appearance of three distinct diatom biomarkers in the stratigraphic record (Rhizosolenia setigera ca. AD 1940; Minidiscus chilensis ca. AD 1860; Thalassionema nitzschioides morphotype A, ca. AD 1550). The oceanographic changes recorded in Effingham Inlet are correlative with other marine and terrestrial paleoenvironmental records in the northeast Pacific Ocean.

Keywords

FjordDiatomsPaleoceanographyBritish ColumbiaBiogenic silicaHolocenePacific OceanUpwellingProduction
Type
Research Article
Information
Quaternary Research , Volume 67 , Issue 1 , January 2007 , pp. 33 - 49
Copyright
University of Washington

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References

Allen, S., Vindeirinho, C., Thomson, R., Foreman, M., and Mackas, D. Physics and biology over a submarine canyon during an upwelling event. Canadian Journal of Fisheries and Aquatic Sciences 58, (2001). 671–684.CrossRefGoogle Scholar
Barlow, M., Nigam, S., and Berbery, E.H. ENSO, Pacific decadal variability, and U.S. summertime precipitation, drought, and stream flow. Journal of Climate 14, (2001). 2105–2128.Google Scholar
Barron, J.A., Heusser, L., Herbert, T., and Lyle, M. High-resolution climatic evolution of coastal northern California during the past 16,000 years. Paleoceanography 18, (2003). 1020 Google Scholar
Bennett, K.D. Documentation for psimpoll 4.10 and pscomb 1.03: C programs for plotting pollen diagrams and analysing pollen data. (2002). Department of Earth Sciences, Uppsala University, Uppsala, Sweden.Google Scholar
Bitz, C.M., and Battisti, D.S. Interannual to decadal variability in climate and the glacier mass balance in Washington, western Canada, and Alaska. Journal of Climate 12, (1999). 3181–3196.2.0.CO;2>CrossRefGoogle Scholar
Clement, A.C., Seager, R., and Cane, M.A. Suppression of El Niño during the mid-Holocene by changes in the Earth's orbit. Paleoceanography 15, (2000). 731–737.Google Scholar
Cremer, H., Roberts, D., McMinn, A., Gore, D., and Melles, M. The Holocene diatom flora of marine bays in the Windmill Islands, East Antarctica. Botanica Marina 46, (2003). 82–106.Google Scholar
Cushing, D.H. A difference in structure between ecosystems in strongly stratified waters and in those that are only weakly stratified. Journal of Plankton Research 11, (1989). 1–13.Google Scholar
Dallimore, A. (2001). Late Holocene geologic, oceanographic and climate history of an anoxic fjord: Effingham Inlet, west coast Vancouver Island. Ph.D. dissertation, Carleton University, Ottawa.Google Scholar
Dallimore, A., Thomson, R.E., and Bertram, M.A. Modern to Late Holocene deposition in an anoxic fjord on the west coast of Canada: implications for regional oceanography, climate and paleoseismic history. Marine Geology 219, (2005). 47–69.CrossRefGoogle Scholar
Gershunov, A., Barnett, T.P., and Cayan, D.R. North Pacific Interdecadal oscillation seen as a factor in ENSO-related North American climate anomalies. EOS 79, (1999). 25–30.CrossRefGoogle Scholar
Haigh, R., Taylor, F.J.R., and Sutherland, T.F. Phytoplankton ecology of Sechelt Inlet, a fjord system on the British Columbia coast. I. General features of the nano- and microplankton. Marine Ecology Progress Series 89, (1992). 117–134.Google Scholar
Håkansson, H., Hajdu, S., Snoeijs, P., and Loginova, L. Cyclotella hakanssoniae Wendker and its relationship to C. caspia Grunow and other similar brackish water Cyclotella species. Diatom Research 8, (1993). 333–347.Google Scholar
Harrison, P.J., Fulton, J.D., Taylor, F.J.R., and Parsons, T.R. Review of the biological oceanography of the Strait of Georgia: pelagic environment. Canadian Journal of Fisheries and Aquatic Sciences 40, (1983). 1064–1094.CrossRefGoogle Scholar
Hay, M.B. (2005). Reconstitution des conditions océanographiques et climatiques de l'holocène supérieur à effingham inlet, colombie britannique. Ph.D. dissertation, université laval, québec. (in English and French). http://www.theses.ulaval.ca/2005/23241/23241.pdf Google Scholar
Hay, M.B., Pienitz, R., and Thomson, R.E. Distribution of diatom surface sediment assemblages within Effingham Inlet, a temperate fjord on the west coast of Vancouver Island (Canada). Marine Micropaleontology 48, (2003). 291–320.Google Scholar
Hebda, R.J. British Columbia vegetation and climate history with focus on 6 ka BP. Géographie physique et Quaternaire 49, (1995). 55–79.Google Scholar
Hitchcock, G.L., and Smayda, T.J. The importance of light in the initiation of the 1972–1973 winter–spring diatom bloom in Narragansett Bay. Limnology and Oceanography 22, (1977). 126–131.Google Scholar
Hsieh, W.W., Ware, D.M., and Thomson, R.E. Wind-induced upwelling along the west coast of North America, 1899–1988. Canadian Journal of Fisheries and Aquatic Sciences 52, (1995). 325–334.Google Scholar
Kutzbach, J.E., Guetter, P.J., Behling, P.J., and Selin, R. Simulated climatic changes: results of the COHMAP climate-model experiments. Wright, H.E., Kutzbach, J.E., Webb, T. III, Ruddiman, W.F., Street-Perrott, F.A., and Bartlein, P.J. Global Climates of the Last Glaciation. (1993). University of Minnesota Press, Minneapolis. 24–93.Google Scholar
Long, C.J., and Whitlock, C. Fire and vegetation history from the coastal rain forest of the western Oregon Coast Range. Quaternary Research 58, (2002). 215–225.CrossRefGoogle Scholar
Long, C.J., Whitlock, C., Bartlein, P.J., and Millspaugh, S.H. A 9000-year fire history from the Oregon Coast Range, based on a high-resolution charcoal study. Canadian Journal of Forest Research 28, (1998). 774–787.Google Scholar
Mackas, D.L., Thomson, R.E., and Galbraith, M. Changes in the zooplankton community of the British Columbia continental margin, 1985–1999, and their covariation with oceanographic conditions. Canadian Journal of Fisheries and Aquatic Sciences 58, (2001). 685–702.Google Scholar
McFarlane, G.A., Ware, D.M., Thomson, R.E., Mackas, D.L., and Robinson, C.L.K. Physical, biological and fisheries oceanography of a large ecosystem (west coast of Vancouver Island) and implications for management. Oceanologia Acta 20, (1997). 191–200.Google Scholar
McQuoid, M.R., and Hobson, L.A. A 91-year record of seasonal and interannual variability of diatoms from laminated sediments in Saanich Inlet, British Columbia. Journal of Plankton Research 19, (1997). 173–194.Google Scholar
McQuoid, M.R., and Hobson, L.A. A Holocene record of diatom and silicoflagellate microfossils in sediments of Saanich Inlet, ODP Leg 169S. Marine Geology 174, (2001). 111–123.CrossRefGoogle Scholar
Mortlock, R.A., and Froelich, P.N. A simple method for the rapid determination of biogenic opal in pelagic marine sediments. Deep-Sea Research I 36, (1989). 1415–1426.Google Scholar
Nederbragt, A.J., and Thurow, J.W. A 6000 yr varve record of Holocene climate in Saanich Inlet, British Columbia, from digital sediment colour analysis of ODP Leg 169S cores. Marine Geology 174, (2001). 95–110.Google Scholar
Patterson, R.T., Guilbault, J.-P., and Thomson, R.E. Oxygen level control on foraminiferal distribution in Effingham Inlet, Vancouver Island, British Columbia. Journal of Foraminiferal Research 30, (2000). 321–335.Google Scholar
Patterson, R.T., Prokoph, A., Kumar, A., Chang, A.S., and Roe, H.M. Late Holocene variability in pelagic fish scales and dinoflagellate cysts along the west coast of Vancouver Island, NE Pacific Ocean. Marine Micropaleontology 55, (2005). 183–204.Google Scholar
Pellatt, M.G., and Mathewes, R.W. Holocene tree line and climate change on the Queen Charlotte Islands, Canada. Quaternary Research 48, (1997). 88–99.Google Scholar
Pickard, G.L. Oceanographic characteristics of inlets of Vancouver Island, British Columbia. Journal Fisheries Research Board of Canada 20, (1963). 1109–1144.Google Scholar
Prasad, A.K.S.K., Nienow, J.A., and Livingston, R.J. The genus Cyclotella (Bacillariophyta) in Choctawhatchee Bay, Florida, with special reference to C. striata and C. choctawhatcheeana sp. nov. Phycologia 29, (1990). 418–436.Google Scholar
Robinson, C.L.K., and Ware, D.M. Simulated and observed response of the southwest Vancouver Island pelagic ecosystem to oceanic conditions in the 1990s. Canadian Journal of Fisheries and Aquatic Sciences 56, (1999). 2433–2443.Google Scholar
Ryder, J.M., and Thomson, B. Neoglaciation in the southern Coast Mountains of British Columbia: chronology prior to the Neoglacial maximum. Canadian Journal of Earth Sciences 23, (1986). 273–287.Google Scholar
Ryves, D.B., Clarke, A.L., Appleby, P.G., Amsinck, S.L., Jeppesen, E., Landkildehus, F., and Anderson, N.J. Reconstructing the salinity and environment of the Limfjord and Vejlerne Nature Reserve, Denmark, using a diatom model for brackish lakes and fjords. Canadian Journal of Fisheries and Aquatic Sciences 61, (2004). 1988–2006.Google Scholar
Sancetta, C. Spatial and temporal trends of diatom flux in British Columbian fjords. Journal of Plankton Research 11, (1989). 503–520.Google Scholar
Sautter, L.R., and Sancetta, C. Seasonal associations of phytoplankton and planktic foraminifera in an upwelling region and their contribution to the seafloor. Marine Micropaleontology 18, (1992). 263–278.Google Scholar
Schell, T.M. (2003). Benthic foraminiferal assemblages in Effingham Inlet, a fjord of western Vancouver Island, British Columbia: implications for late Holocene paleoproductivity of the northeastern Pacific. Ph.D. dissertation, Dalhousie University, Halifax.Google Scholar
Smayda, T.J. The growth of Skeletonema costatum during a winter–spring bloom in Narragansett Bay, Rhode Island. Norwegian Journal of Botany 20, (1973). 219–247.Google Scholar
Southon, J.R., Nelson, D.E., and Vogel, J.S. A record of past ocean–atmosphere radiocarbon differences from the northeast Pacific. Paleoceanography 5, (1990). 197–206.CrossRefGoogle Scholar
Stuiver, M., and Reimer, P.J. Extended 14C database and revised CALIB radiocarbon calibration program. Radiocarbon 35, (1993). 215–230.Google Scholar
Stuiver, M., Reimer, P.J., Bard, E., Beck, J.W., Burr, G.S., Hughen, K.A., Kromer, B., McCormac, F.G., Plicht, J., and Spurk, M. INTCAL98 Radiocarbon age calibration 24,000- 0 cal BP. Radiocarbon 40, (1998). 1041–1083.Google Scholar
Stuiver, M., Reimer, P.J., and Brazunias, T.F. High-precision radiocarbon age calibration for terrestrial and marine samples. Radiocarbon 40, (1998). 1127–1151.CrossRefGoogle Scholar
Takahashi, M., Seibert, D.L., and Thomas, W.H. Occasional blooms of phytoplankton during summer in Saanich Inlet, B.C., Canada. Deep-Sea Research 24, (1977). 775–780.Google Scholar
Thomson, R.E., Hickey, B.M., and LeBlond, P.H. The Vancouver Island Coastal Current: fisheries barrier and conduit. Beamish, R.J., and McFarlane, G.A. Effects of ocean variability on recruitment and an evaluation of parameters used in stock assessment models. Canada Special Publication of Fisheries and Aquatic Sciences vol. 105, (1989). 265–296.Google Scholar
Tunnicliffe, V., O'Connell, J.M., and McQuoid, M.R. A Holocene record of marine fish remains from the northeastern Pacific. Marine Geology 174, (2001). 197–210.Google Scholar
Ware, D.M. A century and a half of change in the climate of the NE Pacific. Fisheries Oceanography 4, (1995). 267–277.Google Scholar
Ware, D.M., and McFarlane, G.A. Fisheries production domains in the northeast Pacific Ocean. Beamish, R.J., and McFarlane, G.A. Effects of ocean variability on recruitment and an evaluation of parameters used in stock assessment models. Canada Special Publication of Fisheries and Aquatic Sciences vol. 105, (1989). 359–379.Google Scholar
Wright, C.A., Dallimore, A., Thomson, R.E., Patterson, R.T., and Ware, D.M. Late Holocene paleofish populations in Effingham Inlet, British Columbia, Canada. Palaeogeography, Palaeoclimatology, Palaeoecology 224, (2005). 367–384.Google Scholar
Zamon, J.E., and Welch, D.W. Rapid shift in zooplankton community composition on the northeast Pacific shelf during the 1998–1999 El Niño–La Niña event. Canadian Journal of Fisheries and Aquatic Sciences 62, (2005). 133–144.Google Scholar
Ziemann, D.A., Conquest, L.D., Olaizola, M., and Bienfang, P.K. Interannual variability in the spring phytoplankton bloom in Auke Bay, Alaska. Marine Biology 109, (1991). 321–334.Google Scholar