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1
Holocene fire regimes, fire‐related plant functional types, and climate in south‐coastal British Columbia forests
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Holocene fire regimes, fire‐related plant functional types, and climate in south‐coastal British Columbia forests

Ecosphere (Washington, D.C), 2023-02, Vol.14 (2), p.n/a [Peer Reviewed Journal]

2023 The Authors. published by Wiley Periodicals LLC on behalf of The Ecological Society of America. ;2023. This work is published under http://creativecommons.org/licenses/by/4.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License. ;ISSN: 2150-8925 ;EISSN: 2150-8925 ;DOI: 10.1002/ecs2.4416

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2
Climate and Species Traits Drive Changes in Holocene Forest Composition Along an Elevation Gradient in Pacific Canada
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Climate and Species Traits Drive Changes in Holocene Forest Composition Along an Elevation Gradient in Pacific Canada

Frontiers in ecology and evolution, 2022-03, Vol.10 [Peer Reviewed Journal]

ISSN: 2296-701X ;EISSN: 2296-701X ;DOI: 10.3389/fevo.2022.838545

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3
Diatom responses to long‐term climate and sea‐level rise at a low‐elevation lake in coastal British Columbia, Canada
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Diatom responses to long‐term climate and sea‐level rise at a low‐elevation lake in coastal British Columbia, Canada

Ecosphere (Washington, D.C), 2019-09, Vol.10 (9), p.n/a [Peer Reviewed Journal]

2019 The Authors. ;2019. This work is published under http://creativecommons.org/licenses/by/3.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License. ;ISSN: 2150-8925 ;EISSN: 2150-8925 ;DOI: 10.1002/ecs2.2868

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4
Current practices in building and reporting age-depth models
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Current practices in building and reporting age-depth models

Quaternary research, 2020-07, Vol.96, p.28-38 [Peer Reviewed Journal]

Copyright © University of Washington. Published by Cambridge University Press, 2020 ;ISSN: 0033-5894 ;EISSN: 1096-0287 ;DOI: 10.1017/qua.2020.47

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5
Pollen-based climate reconstruction techniques for late Quaternary studies
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Pollen-based climate reconstruction techniques for late Quaternary studies

Earth-science reviews, 2020-11, Vol.210, p.1-33 [Peer Reviewed Journal]

Attribution - NonCommercial - NoDerivatives ;ISSN: 0012-8252 ;EISSN: 1872-6828 ;DOI: 10.1016/j.earscirev.2020.103384

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6
Postglacial wetland succession, carbon accumulation, and forest dynamics on the east coast of Vancouver Island, British Columbia, Canada
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Postglacial wetland succession, carbon accumulation, and forest dynamics on the east coast of Vancouver Island, British Columbia, Canada

Quaternary research, 2019-07, Vol.92 (1), p.232-245 [Peer Reviewed Journal]

Copyright © University of Washington. Published by Cambridge University Press, 2019 ;ISSN: 0033-5894 ;EISSN: 1096-0287 ;DOI: 10.1017/qua.2018.146

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7
A multi-proxy peat study of Holocene vegetation history, bog development, and carbon accumulation on northern Vancouver Island, Pacific coast of Canada
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A multi-proxy peat study of Holocene vegetation history, bog development, and carbon accumulation on northern Vancouver Island, Pacific coast of Canada

Holocene (Sevenoaks), 2015-07, Vol.25 (7), p.1165-1178 [Peer Reviewed Journal]

The Author(s) 2015 ;ISSN: 0959-6836 ;EISSN: 1477-0911 ;DOI: 10.1177/0959683615580201

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8
Widespread global peatland establishment and persistence over the last 130,000 y
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Widespread global peatland establishment and persistence over the last 130,000 y

Proceedings of the National Academy of Sciences - PNAS, 2019-03, Vol.116 (11), p.4822-4827 [Peer Reviewed Journal]

Copyright © 2019 the Author(s). Published by PNAS. ;Copyright National Academy of Sciences Mar 12, 2019 ;Copyright © 2019 the Author(s). Published by PNAS. 2019 ;ISSN: 0027-8424 ;ISSN: 1091-6490 ;EISSN: 1091-6490 ;DOI: 10.1073/pnas.1813305116 ;PMID: 30804186

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9
Dendroglaciological investigations of mid- to late-Holocene glacial activity in the Mt. Waddington area, British Columbia Coast Mountains, Canada
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Dendroglaciological investigations of mid- to late-Holocene glacial activity in the Mt. Waddington area, British Columbia Coast Mountains, Canada

Holocene (Sevenoaks), 2013-01, Vol.23 (1), p.93-103 [Peer Reviewed Journal]

The Author(s) 2012 ;SAGE Publications © Jan 2013 ;ISSN: 0959-6836 ;EISSN: 1477-0911 ;DOI: 10.1177/0959683612455537

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10
Late Pleistocene vegetation and sedimentary charcoal at Kilgii Gwaay archaeological site in coastal British Columbia, Canada, with possible proxy evidence for human presence by 13,000 cal bp
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Late Pleistocene vegetation and sedimentary charcoal at Kilgii Gwaay archaeological site in coastal British Columbia, Canada, with possible proxy evidence for human presence by 13,000 cal bp

Vegetation history and archaeobotany, 2020-05, Vol.29 (3), p.297-307 [Peer Reviewed Journal]

Springer-Verlag GmbH Germany, part of Springer Nature 2019 ;Springer-Verlag GmbH Germany, part of Springer Nature 2019. ;ISSN: 0939-6314 ;EISSN: 1617-6278 ;DOI: 10.1007/s00334-019-00743-4

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11
Widespread global peatland establishment and persistence over the last 130,000 y
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Widespread global peatland establishment and persistence over the last 130,000 y

public 565384 ;ISSN: 0027-8424 ;ISSN: 1091-6490 ;EISSN: 1091-6490 ;DOI: 10.1073/pnas.1813305116

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12
Calibrated ages of Port McNeill (PMB) peat core from Canada
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Calibrated ages of Port McNeill (PMB) peat core from Canada

CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess

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13
Age determination of Port McNeill (PMB) peat core from Canada
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Age determination of Port McNeill (PMB) peat core from Canada

CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess

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14
Geochemistry of Port McNeill (PMB) peat core from Canada
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Geochemistry of Port McNeill (PMB) peat core from Canada

CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess

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15
new methodology for reconstructing climate and vegetation from modern pollen assemblages: an example from British Columbia
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new methodology for reconstructing climate and vegetation from modern pollen assemblages: an example from British Columbia

Journal of biogeography, 2009-04, Vol.36 (4), p.626-638 [Peer Reviewed Journal]

Copyright 2009 Blackwell Publishing Ltd. ;2008 The Authors. Journal compilation © 2008 Blackwell Publishing Ltd ;2009 INIST-CNRS ;ISSN: 0305-0270 ;EISSN: 1365-2699 ;DOI: 10.1111/j.1365-2699.2008.02021.x ;CODEN: JBIODN

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16
Climate-driven changes in lake conditions during late MIS 3 and MIS 2: a high-resolution geochemical record from Les Echets, France
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Climate-driven changes in lake conditions during late MIS 3 and MIS 2: a high-resolution geochemical record from Les Echets, France

Boreas, 2009-01, Vol.38 (2), p.230-243 [Peer Reviewed Journal]

2008 The Authors, Journal compilation © 2008 The Boreas Collegium ;Distributed under a Creative Commons Attribution 4.0 International License ;ISSN: 0300-9483 ;ISSN: 1502-3885 ;EISSN: 1502-3885 ;DOI: 10.1111/j.1502-3885.2008.00066.x

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17
Late Glacial and Holocene Palaeoenvironmental Changes in the Rostov-Yaroslavl’ Area, West Central Russia
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Late Glacial and Holocene Palaeoenvironmental Changes in the Rostov-Yaroslavl’ Area, West Central Russia

Journal of paleolimnology, 2006-04, Vol.35 (3), p.543-569 [Peer Reviewed Journal]

Springer 2006 ;ISSN: 0921-2728 ;EISSN: 1573-0417 ;DOI: 10.1007/s10933-005-3240-4

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18
Regional variability in peatland burning at mid-to high-latitudes during the Holocene
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Regional variability in peatland burning at mid-to high-latitudes during the Holocene

info:eu-repo/semantics/openAccess ;DOI: 10.1016/j.quascirev.2023.108020

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19
Pollen-based climate reconstruction techniques for late Quaternary studies
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Pollen-based climate reconstruction techniques for late Quaternary studies

info:eu-repo/semantics/openAccess

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20
Widespread global peatland establishment and persistence over the last 130,000 y
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Article
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Widespread global peatland establishment and persistence over the last 130,000 y

cc_by ;DOI: 10.1073/pnas.1813305116

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