Paleoproductivity and organic matter sources in Late Quaternary Lake Ontario-Reference-Cited by-同舟云学术

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Paleoproductivity and organic matter sources in Late Quaternary Lake Ontario

Published:2015-10 Issue: Volume:435 Page:13-23
ISSN:0031-0182
Container-title:Palaeogeography, Palaeoclimatology, Palaeoecology
language:en
Short-container-title:Palaeogeography, Palaeoclimatology, Palaeoecology

Author:

Hladyniuk Ryan^ORCID,Longstaffe Fred J.^ORCID

Funder

Natural Sciences and Engineering Research Council of Canada

Canada Research Chairs

Canada Foundation for Innovation

Ontario Research Foundation

Publisher

Elsevier BV

Subject

Paleontology,Earth-Surface Processes,Ecology, Evolution, Behavior and Systematics,Oceanography

Reference49 articles.

1. A new water-level history for Lake Ontario basin evidence for a climate-driven early Holocene lowstand;Anderson;J. Paleolimnol.,2012

2. Methods and code for ‘classical’ age-modelling of radiocarbon sequences;Blaauw;Quat. Geochronol.,2010

3. Environmental applications of marine and freshwater ostracoda;Boomer,2002

4. Evidence for bias in C and N concentrations and δ13C composition of terrestrial and aquatic organic materials due to pre-analysis acid preparation methods;Brodie;Chem. Geol.,2011

5. The paleolimnology of Lake Simcoe: oxygen-isotope compositions of ostracodes;Bumstead,2009

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1. A ∼14 000-year record of environmental change from Lake Simcoe, Canada;Quaternary Science Reviews;2022-09

2. A late-glacial lake-effect climate regime and abundant tamarack in the Great Lakes Region, North America;Quaternary Research;2022-05-18

3. Paleoenvironment of the Lower Ordovician Meitan Formation in the Sichuan Basin and Adjacent Areas, China;Minerals;2022-01-08

4. Paleoenvironment and Organic Matter Enrichment of the Middle Ordovician Marine Carbonates in the Ordos Basin of China: Evidence from Element Geochemistry;ACS Earth and Space Chemistry;2021-12-21

5. A 900-year record of effective moisture in the Laurentian Great Lakes region;Quaternary Science Reviews;2021-10

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